Rhenium in Molybdenite: a Database Approach to Identifying Geochemical Controls on the Distribution of a Critical Element

Item Type Article

Authors Barton, Isabel F.; Rathkopf, Christian A.; Barton, Mark D.

Citation Barton, I. F., Rathkopf, C. A., & Barton, M. D. (2019). Rhenium in Molybdenite: a Database Approach to Identifying Geochemical Controls on the Distribution of a Critical Element. Mining, Metallurgy & Exploration, 1-17.

DOI 10.1007/s42461-019-00145-0

Publisher Springer Science and Business Media LLC

Journal MINING METALLURGY & EXPLORATION

Rights © Society for Mining, Metallurgy & Exploration Inc. 2019.

Download date 02/10/2021 13:24:48

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Version Final accepted manuscript

Link to Item http://hdl.handle.net/10150/636269 Manuscript Click here to access/download;Manuscript;Manuscript_ReMolyDatabase_MM Click here to view linked References 1 2 3 4 1 Rhenium in molybdenite: A database approach to identifying geochemical controls 5 6 7 2 on the distribution of a critical element 8 9 3 Isabel F. Barton 1, 2, ,3 , Christian A. Rathkopf 4,5, Mark D. Barton 2, 4 10 11 12 4 13 14 5 1 Corresponding author: [email protected] 15 16 6 2 University of Arizona Lowell Institute for Mineral Resources 17 18 19 7 3 now with University of Arizona Department of Mining and Geological Engineering, 20 21 8 1235 James E. Rogers Way, Tucson, AZ 85721 22 23 4 th 24 9 University of Arizona Department of Geosciences, 1040 E. 4 St., Tucson, AZ 85721 25 26 10 5 now with Hecla Mining, 3300 Traders Way, Suite C, Box 15, Winnemucca, NV 89445 27 28 29 11 30 31 12 Abstract 32 33 34 13 Molybdenite is the world’s principal source of rhenium (Re), a critical element in 35 36 14 multiple high-tech applications. However, the Re contents in molybdenite vary by orders 37 38 15 of magnitude on scales ranging from single grains to whole deposits. In order to better 39 40 41 16 understand the systematics of this variation and what geochemical factors control 42 43 17 molybdenite Re concentration, and hence overall Re resources, we examine global 44 45 46 18 patterns in molybdenite Re contents through a compilation of > 3,000 measurements of 47 48 19 Re in molybdenite from > 700 mainly ore-bearing moderate- to high-temperature 49 50 51 20 hydrothermal systems of different types. Our results are similar to but expand on those of 52 53 21 earlier studies. 54 55 22 Rhenium concentration in molybdenite has a lognormal distribution in 56 57 58 23 molybdenites and varies systematically with type of geologic system, intrusive lithology, 59 60 61 62 63 1 64 65 1 2 3 4 24 and Mo grade. The lowest-Re molybdenite occurs in greisens (geometric mean 1 ppm ± a 5 6 7 25 multiplicative standard deviation of 9), quartz vein-hosted W-Sn deposits (2 ± 5 ppm), 8 9 26 unmineralized granites and granodiorites (12 ± 8 ppm), intrusion-related deposits (14 ± 8 10 11 12 27 ppm), and porphyry W-Sn deposits (16 ± 11 ppm). Rhenium is most enriched in 13 14 28 molybdenites from volcanic sublimates (23,800 ± 5 ppm), with skarn Fe and Au (560 ± 5 15 16 29 ppm and 540 ± 3 ppm respectively) and porphyry Cu and Cu-Au deposits next (470 ± 4 17 18 19 30 and 430 ± 7 ppm respectively). Among porphyries, skarns, and quartz vein-hosted 20 21 31 deposits, Re is most highly concentrated in molybdenites from Cu and Au systems and its 22 23 24 32 concentration decreases systematically through Cu-Mo, Mo, Sn, and W deposits. In 25 26 33 nearly all cases, molybdenites from systems associated with intermediate igneous rocks 27 28 29 34 contain more Re than molybdenites from systems of the same type with more felsic rock 30 31 35 associations. The disparity between Re contents of molybdenite infelsic and intermediate 32 33 34 36 systems is largest for porphyries, quartz vein-hosted, and skarn deposits and is near zero 35 36 37 for subeconomic or barren granite and granodiorite Mo systems; felsic intrusion-related 37 38 38 deposits have slightly higher molybdenite Re than their equivalents associated with 39 40 41 39 intermediate intrusions. In most systems molybdenite Re content does not correlate with 42 43 40 metal grade, but may have an inverse correlation with Au grade in intrusion-related 44 45 46 41 deposits (based on a small number of data points) and does exhibit a strong inverse 47 48 42 correlation with deposit Mo grade. Dilution of Re through larger amounts (higher deposit 49 50 51 43 grades) of molybdenite explains about 40% of this correlation, but the relative 52 53 44 enrichment of Re in molybdenite from low-Mo deposits must also reflect some selective 54 55 45 enrichment of Re:Mo in porphyry Cu systems compared to porphyry Mo systems. We 56 57 58 46 found no evidence for secular increase or other systematic temporal variation in 59 60 61 62 63 2 64 65 1 2 3 4 47 molybdenite Re content. The data regarding the use of molybdenite Re content as a proxy 5 6 7 48 for mantle influence are ambiguous. 8 9 49 Nearly all observed empirical correlations can be traced back to differences in 10 11 12 50 redox state and sulfide concentration, the two geochemical factors identified here and by 13 14 51 previous experimental work as the controlling influences on Re mobility under 15 16 52 hydrothermal conditions. Hydrothermal systems with reducing conditions (W- and Sn- 17 18 19 53 rich) tend to have low molybdenite Re even though compiled whole-rock data indicate 20 21 54 that their source rocks have as much or more Re as those of more oxidized systems (e.g., 22 23 24 55 Cu-rich). Vapor-phase exsolution, crustal assimilation, and mixing with external fluids, 25 26 56 may all enrich molybdenite Re concentrations in individual deposits and deposit types, 27 28 29 57 but their extent and importance in overall hydrothermal concentration of Re is uncertain. 30 31 58 Thus, it appears that the available molybdenite Re resource in an ore deposit largely 32 33 34 59 depends on how the deposit’s redox and sulfidation conditions have varied over time and 35 36 60 space during the timespan of hydrothermal activity. Oxidized, high-sulfide conditions 37 38 61 tend to concentrate Re in molybdenite, whereas reducing conditions tend to leave Re 39 40 41 62 dispersed at low concentrations in the bulk rock. 42 43 63 keywords: rhenium, molybdenite, Re-Os, porphyry deposits, exploration, rhenium 44 45 46 64 behavior in hydrothermal systems 47 48 65 49 50 51 66 1. Introduction 52 53 67 1.1 Background and purpose of this study 54 55 68 Rhenium is an essential element in the manufacture of superalloys, turbine blades, 56 57 58 69 and various catalysts used in refining petroleum. While U.S. reserves of rhenium are 59 60 61 62 63 3 64 65 1 2 3 4 70 substantial, Re is a designated critical element in the U.S. due to limited production, low 5 6 7 71 recycling capability, and heavy reliance on imports (John et al., 2017 [1]).The vast 8 4+ 9 72 majority of Re is produced as a byproduct of molybdenite (MoS2), where Re substitutes 10 11 4+ 12 73 for Mo ; end-member rheniite ReS2 is extremely rare (John and Taylor, 2016 [2]). 13 14 74 However, Re concentrations in natural molybdenite vary over nearly 9 orders of 15 16 75 magnitude from tens of % to a few parts per billion, and over scales from a single grain to 17 18 19 76 a whole deposit (Rathkopf et al., 2017 [3]). Despite several attempts (e.g. John and 20 21 77 Taylor, 2016 [2]; Giles and Schilling, 1972 [4]; Terada et al., 1971 [5]; Newberry, 1979 22 23 24 78 [6]; Berzina et al., 2005 [7]; Voudouris et al., 2013 [8]; Ciobanu et al., 2013 [9]), no 25 26 79 consistent pattern to this variability has been discovered, nor has any geochemical 27 28 29 80 rationale for why Re content in molybdenite varies so much. 30 31 81 To address this question, we compiled a database of Re concentrations measured 32 33 34 82 from molybdenites in mineralized and unmineralized sites, most of them hydrothermal. 35 36 83 Our goal in this compilation is to identify patterns that will enable us to evaluate what 37 38 84 geochemical factors control the Re content of molybdenites and to assess whether 39 40 41 85 molybdenite Re content can reliably be used as a vector to ore deposits or to high grades, 42 43 86 as has been previously suggested (e.g. Berzina et al., 2005 [7]; Voudouris et al., 2013 [8]; 44 45 46 87 Coope, 1973 [10]; Voudouris et al., 2009 [11]). Given this focus on molybdenite Re 47 48 88 contents, we only touch on the Re(-Mo) enrichments present in many sediment-hosted Cu 49 50 51 89 and U systems, which are well known but which have not been definitively traced to Re- 52 53 90 rich molybdenite (John et al., 2017 [1]). 54 55 91 Compilations of molybdenite Re content have been made before (discussion 56 57 58 92 below), but most have included <100 data points. Although these are valuable 59 60 61 62 63 4 64 65 1 2 3 4 93 contributions, the number of data points per deposit type, rock type, or region is 5 6 7 94 comparatively small. Similarly, global estimates of rhenium resources such as by John et 8 9 95 al. (2017 [1]) are based on relatively few major occurrences and in some cases on 10 11 12 96 molybdenite Re contents that are estimated from whole-rock assays rather than measured 13 14 97 directly from molybdenite. Having a larger dataset may serve not only to reveal 15 16 98 previously unobserved patterns in molybdenite Re distribution, but will also help to place 17 18 19 99 the trends already detected on a more rigorous and better-supported statistical basis than 20 21 100 is possible from a study that involves fewer samples. 22 23 24 101 1.2 Previous work 25 26 102 Fleischer (1959 [12]) made the first compilation of 150 Re concentrations in 27 28 29 103 molybdenites from 82 mines around the world. His was one of the first studies to 30 31 104 recognize that Re content of molybdenite varies by orders of magnitude within and 32 33 34 105 between deposits; however, because most of his samples came from molybdenite 35 36 106 concentrates, he was unable to connect Re content to many geological features. Badalov 37 38 107 (1962 [13]) compiled Re concentrations in molybdenites from the USSR and suggested 39 40 41 108 that Re content increased as temperature of molybdenite precipitation decreased. Riley 42 43 109 (1967 [14]) sampled molybdenites at various Australian ore deposits. His work supported 44 45 46 110 Fleischer’s (1959 [12]) correlation of molybdenite Re contents with Cu grade and added 47 48 111 that molybdenite from pipe deposits was Re-depleted compared to molybdenite from vein 49 50 51 112 deposits. Riley found no time- or geography-linked patterns in Re abundance, nor any 52 53 113 evident correlations between deposit geology and Re content. However, Terada et al. 54 55 114 (1971 [5]) were able to link Re content in Japanese ore deposits to deposit type: they 56 57 58 115 found that Re was most abundant in molybdenites from volcanic sublimate systems, 59 60 61 62 63 5 64 65 1 2 3 4 116 where it reached up to 3700 ppm, and decreased consistently through porphyry Cu, 5 6 7 117 skarns, disseminated, and vein-type deposits, with few exceptions. They also found an 8 9 118 approximate correlation between small crystal size and high Re content. A follow-up note 10 11 12 119 by Fleischer (1960 [15]), based on then-recent work in the USSR, highlighted the 13 14 120 extreme variability of molybdenite Re among porphyry copper deposits, and suggested 15 16 121 that molybdenite Re content increased with the progression from higher- to lower- 17 18 19 122 temperature deposition. A later compilation by Ishihara (1988 [16]) corroborated and 20 21 123 expanded these conclusions of Terada et al. (1971 [5]), adding that Re content in 22 23 24 124 molybdenite in igneous provinces mostly reflected the oxidation state of the magma, with 25 26 125 magnetite-stable (i.e. comparatively oxidized) igneous rocks having the most Re in 27 28 29 126 molybdenite. 30 31 127 Giles and Schilling (1972 [4]) provided further documentation of the extreme Re 32 33 34 128 variation even in single crystals, illustrating one molybdenite grain that had zones 35 36 129 varying from < 200 ppm to several weight percent Re. Additional study by Newberry 37 38 130 (1979 [6]) focused on porphyry Cu and Mo deposits, finding that Re content correlated 39 40 41 131 inversely with Mo grade in spite of an overall high average Re content in what Gustafson 42 43 132 and Hunt (1975 [17]) dubbed “B-veinlets.” These veinlets, which typify the middle stage 44 45 46 133 the evolution of a porphyry deposit, are more common and have more Re in the altered 47 48 134 aureole of porphyries than in the central stocks (Newberry, 1979 [6]). Newberry was 49 50 51 135 particularly concerned with the polytypism of molybdenite, whose 3R polytype he found 52 53 136 hosted the most Re. 54 55 137 Since then, most compilations of Re data have been parts of studies of the 56 57 58 138 geochemical behavior of rhenium, particularly in the context of Re-Os geochronology 59 60 61 62 63 6 64 65 1 2 3 4 139 (e.g. McCandless et al., 1993 [18]; Stein et al., 2003 [19]). One exception is a 5 6 7 140 compilation by Berzina et al. (2005 [7]), which corroborated the previously discovered 8 9 141 correlations between high Re content and high Cu, low Mo, low temperature of 10 11 12 142 formation, and oxidized magmas, and suggested additional correlations with mantle-type 13 14 143 Sr isotopes, low δ34S, and high Cl content of fluid inclusions. Sinclair et al. (2009, [20]) 15 16 144 also examined Re concentrations in Canadian porphyry deposits as potential Re 17 18 19 145 resources, and also documented a negative correlation between Re and Mo. The present 20 21 146 article and attached database (Digital Appendix A) compile these and other data into a list 22 23 24 147 of 3,067 measured Re concentrations from 723 molybdenite occurrences around the 25 26 148 world, and criticallyevaluate the factors that influence molybdenite Re content. 27 28 29 149 30 31 150 2. Methods 32 33 34 151 The principal components of this article are Digital Appendices A, B, and C. 35 36 152 Appendix A lists the molybdenite Re data for each deposit, along with deposit type, 37 38 153 associated igneous rocks, metal grades where available, age of mineralization where 39 40 41 154 available, and sampling and analytical details. Appendix B gives the full references for 42 43 155 the data cited in Appendix A. Appendix C contains a brief explanation of the rationale for 44 45 46 156 the choice of classification for deposits where the type was not clear or commonly 47 48 157 known. 49 50 51 158 Data were compiled from the 273 sources listed in Digital Appendix B. Database 52 53 159 sources include Re-Os isotopic studies, molybdenite trace-element studies, and regional 54 55 160 and global compilations of Re data assembled from these and other articles. Whenever 56 57 58 161 possible, the secondary data sets were checked against the primary published source. 59 60 61 62 63 7 64 65 1 2 3 4 162 Some data (fewer than 100 data points) that were published or obtained after most of the 5 6 7 163 calculations were completed have been included in the database but were not factored 8 9 164 into the calculations or figures (e.g. Sillitoe et al., 2017 [21]). Thus calculations made 10 11 12 165 with the database in Appendix A may vary slightly from the results presented here. 13 14 166 All Re values in the database are given as parts per million. Some of the values 15 16 167 were converted from original weight percentages or parts per billion with the addition of 17 18 19 168 leading or trailing zeroes (e.g. 9% Re appears in the database as 90,000 ppm Re, and 21 20 21 169 ppb Re as 0.021 ppm Re), which are not significant digits. Otherwise, no changes have 22 23 24 170 been made to the data, which therefore represent varying levels of precision and 25 26 171 significance. All Re concentrations given are modern values, not corrected for 187Re 27 28 29 172 decay through time. The maximum possible Re loss from molybdenite due to radioactive 30 31 173 decay is < 5% over 3 Ga, which is much less than the analytical error of many of the data 32 33 34 174 collected from older sources. 35 36 175 The compilation includes all types of molybdenite-bearing hydrothermal systems, 37 38 176 primarily ore deposits, with type classifications, genetically associated igneous rocks if 39 40 41 177 any, and other metal grades where available. Many characteristics given in the older 42 43 178 literature, particularly deposit models and intrusive lithologies, had to be reclassified into 44 45 46 179 a scheme consistent with the categories used in more recent publications. If two sources 47 48 180 for a single deposit gave conflicting descriptions or classifications, we attempted to verify 49 50 51 181 the characteristics in question with secondary sources, eventually using either the most 52 53 182 commonly cited version or the one most compatible with other deposit and regional data. 54 55 183 The divisions between some deposit types are fuzzy, for example the distinctions 56 57 58 184 between quartz vein-hosted and greisen systems, or between intrusion-related deposits 59 60 61 62 63 8 64 65 1 2 3 4 185 and the porphyry and granite-related classes. For the database, we classified deposits as 5 6 7 186 greisens only if the original sources unambiguously referred to them as greisen-related, or 8 9 187 described abundant coarse mica and other common characteristics of greisens. All others 10 11 12 188 were placed in the quartz vein-hosted category. In some cases the granite- and 13 14 189 granodiorite-related systems contained the same rock types as porphyries and intrusion- 15 16 190 related deposits, but these were distinguished from porphyries and intrusion-related 17 18 19 191 deposits by lacking economic mineralization, veins, porphyritic textures, hydrothermal 20 21 192 alteration, stockworks, and other features of porphyry-style or intrusion-related 22 23 24 193 mineralization. They are essentially granitic or granodioritic intrusive rocks without 25 26 194 extensive hydrothermal systems. A classification of intrusion-related signifies that a 27 28 29 195 deposit contains potentially economic mineralization, but not of a porphyry style, related 30 31 196 to one or more igneous intrusions. Appendix C documents the reasoning and literature 32 33 34 197 behind the deposit type classifications for deposits with ambiguous characteristics. Skarn 35 36 198 and pegmatite refer to an alteration type and an igneous texture, respectively, but both 37 38 199 terms are also used as deposit types in the literature of economic geology, a convention 39 40 41 200 we have followed here. 42 43 201 Most deposits in the database have more than one type of associated igneous rock, 44 45 46 202 but were classified as felsic or intermediate based on the predominating lithology. 47 48 203 “Felsic” is defined as any type of granite or granitoid, whereas “intermediate” includes 49 50 51 204 andesite, diorite, monzonite, and granodiorite. There were few basalts, gabbros, or 52 53 205 komatiites among the data, but these were classified as mafic. 54 55 206 If the literature contained different average metal grades for a deposit, we chose 56 57 58 207 the most recent. Where assay-based grades were available, we used them instead of 59 60 61 62 63 9 64 65 1 2 3 4 208 production-based grades since the latter can depend more on economics than on geology. 5 6 7 209 Where the age of mineralization was in dispute, we used Re-Os ages if available, as these 8 9 210 are most relevant to the subject of this paper. Due to incompleteness or inconsistency in 10 11 12 211 the literature, it was not possible to include in the database some factors that may 13 14 212 influence molybdenite Re content, such as the tectonic setting of the deposits, the 15 16 213 physicochemical conditions of ore formation, and the polytype of the molybdenite 17 18 19 214 analyzed. 20 21 215 Statistics in this paper are of two types: 1) those based on deposit-wide geometric 22 23 24 216 mean Re concentration, and 2) those based on geometric means of all individual Re data 25 26 217 points. The first type has the advantage of weighting all deposits within a class equally, 27 28 29 218 mitigating the disproportionate impact of large datasets from exceptional deposits. The 30 31 219 second type of statistics is subject to this bias, but offers a more realistic representation of 32 33 34 220 the full range of molybdenite Re concentrations within individual deposits, which can 35 36 221 cover 3-4 orders of magnitude (Giles and Schilling, 1972 [4]; Kosler et al., 2003 [22]). 37 38 222 Throughout the analysis we have used geometric rather than arithmetic means, as the 39 40 41 223 distribution of molybdenite Re content is lognormal rather than normal (Figure 1), as is 42 43 224 common in elemental distributions (Lasky, 1950 [23]; Singer, 2013 [24]). Molybdenite 44 45 46 225 Re contents from porphyry and skarn deposits follow the standard lognormal distribution, 47 48 226 but other deposit types depart slightly from it. For quartz vein-hosted deposits and Mo 49 50 51 227 related to granites and granodiorites, the lognormal distribution of molybdenite Re 52 53 228 concentrations has a large left tail. Thus the geometric mean and median statistics for 54 55 229 quartz vein-hosted deposits and for granite and granodiorite Mo are slightly less 56 57 58 59 60 61 62 63 10 64 65 1 2 3 4 230 representative of the overall characteristics of the distributions than the comparable 5 6 7 231 statistics for porphyry and skarn deposits. 8 9 232 10 11 12 233 3. Results 13 14 234 3.1 Rhenium concentration and deposit type 15 16 235 Of the 731 sample sites in the database, 682 were assigned to one of the 30 17 18 19 236 deposit type categories shown in Figure 2. Thirty-one of the remaining deposits belong to 20 21 237 unknown types, 11 to districts with multiple undifferentiated mineralization styles, and 22 23 24 238 the remaining seven to categories with fewer members than necessary to generate useful 25 26 239 statistics. In three cases, a single site contained multiple mineralization styles matching 27 28 29 240 different data points; these appear as duplicates in the database. Deposits for which the 30 31 241 multiple mineralization styles were not explicitly matched to specific data points were 32 33 34 242 included in the database but were excluded from calculations and figures. 35 36 243 Although there is a large degree of overlap in molybdenite Re concentrations 37 38 244 between types of geological systems, Figure 2 shows several noticeable trends based on 39 40 41 245 geometric mean molybdenite Re content. Volcanic sublimates have the highest 42 43 246 molybdenite Re by all measures (geometric mean > 20000 ppm). For porphyry-type 44 45 46 247 deposits, the molybdenite Re contents are highest in Au- and Cu-dominated classes 47 48 248 (Table 1; generally > 300 ppm) and lowest in Sn and W systems (< 20 ppm). 49 50 51 249 Molybdenum-dominated porphyries contain molybdenite with moderate Re 52 53 250 concentrations (30-60 ppm). Skarn and quartz vein-hosted deposits mostly follow a 54 55 251 similar pattern, with one anomaly in each case. Among skarns, the small class of Cu and 56 57 58 252 Cu-Au skarn deposits was anomalously low in molybdenite Re. Among quartz vein- 59 60 61 62 63 11 64 65 1 2 3 4 253 hosted deposits, the Cu-dominated subset had more Re in molybdenite than the quartz 5 6 7 254 vein-hosted Au deposits. Molybdenite from Fe skarn deposits is enriched in Re (> 500 8 9 255 ppm) compared to molybdenite from Cu and Au porphyry and skarn deposits; however, 10 11 12 256 the small (5 deposits) Fe skarn data set is skewed by molybdenite from Dognecea and 13 14 257 Arendal that is high in Re. Moreover, most of the deposits in the Fe skarn category have 15 16 258 an unclear degree of overlap with the IOCG deposit type. Molybdenite with the lowest 17 18 19 259 Re concentrations occurs in quartz vein-hosted W-Sn (1-2 ppm) and greisen (< 2 ppm) 20 21 260 deposits. Breccia pipe and quartz vein-hosted Mo deposits are approximately comparable 22 23 24 261 in molybdenite Re content at ~ 10 ppm, and porphyry W-Sn deposits (4-16 ppm) and 25 26 262 unmineralized granites and granodiorites (8-12 ppm) have similar values. Molybdenite 27 28 29 263 from IOCG deposits appears to be high in Re (362 ppm) in the statistics based on 30 31 264 individual Re measurements, but the moderate ranking in the statistics based on deposit- 32 33 34 265 wide geometric means (72 ppm) indicates that this is mainly due to a large dataset on 35 36 266 high-Re molybdenite recently published from Merlin, whose inclusion in the IOCG class 37 38 267 is debatable (Babo et al., 2017 [25]; see Appendix C). 39 40 41 268 3.2 Rhenium concentration and igneous composition 42 43 269 Rhenium concentration is generally highest in molybdenite from systems 44 45 46 270 associated with intrusions of intermediate composition, and lowest in systems associated 47 48 271 with intrusions with felsic compositions (Fig. 3). This relationship remains consistent 49 50 51 272 when the data are broken out by deposit classes (Table 2). The only exception is the 52 53 273 intrusion-related category of deposits, in which molybdenite Re concentration is slightly 54 55 274 higher in felsic-associated than in intermediate-associated systems. Granite and 56 57 58 275 granodiorite Mo systems have substantially the same molybdenite Re concentrations, and 59 60 61 62 63 12 64 65 1 2 3 4 276 are the lowest molybdenite Re concentrations of any category except for quartz vein- 5 6 7 277 hosted deposits related to felsic intrusions. It was not possible to examine the relationship 8 9 278 between igneous rock type and molybdenite Re content due to lack of granularity in the 10 11 12 279 data. 13 14 280 3.3 Molybdenite Re concentration and metal grades 15 16 281 For Cu and Au, it is not clear how molybdenite Re concentration correlates with 17 18 19 282 deposit ore metal grade, if it does so at all, for any class of deposit with enough data to 20 21 283 support meaningful statistics (Fig. 4). There is a potential inverse correlation between 22 23 24 284 molybdenite Re and Au grade in intrusion-related deposits, but based on only nine data 25 26 285 points. However, molybdenum grade exhibits a pronounced negative correlation with 27 28 29 286 molybdenite Re concentration in porphyries (Fig. 5). Some of this results from the 30 31 287 dilution of Re through higher-grade molybdenite than is present in a low-Mo system, 32 33 34 288 resulting in lower molybdenite Re concentrations in the higher-Mo deposits (Fig. 5a, 35 36 289 points a and b). However, the data plotted in Figure 5b show that the actual Re 37 38 290 enrichment in molybdenite from low-Mo systems is significantly more than can be 39 40 41 291 attributed to mass balance alone. If molybdenite Re contents reflected simply the 42 43 292 abundance of molybdenite or Mo in the deposits as proposed by Giles and Schilling 44 45 46 293 (1972 [4]), Newberry (1979 [6]), Berzina et al. (2005 [7]), Stein et al., 1997 [26], Stein et 47 48 294 al. (2001 [27]), Selby and Creaser (2001 [28]), and others, then Re contents in 49 50 51 295 molybdenite should show an inverse correlation with Mo grade with a slope of m = -1 in 52 53 296 log-log space (Fig. 5b). In fact, the data are scattered but linear regression of the 54 55 297 logarithms of Re and Mo content yielded a best-fit line with m = -0.4 (R2 = 0.29), 56 57 58 298 indicating that the simple dilution scenario can explain about 40% of the Re enrichment 59 60 61 62 63 13 64 65 1 2 3 4 299 in molybdenite in low-Mo deposits. The remainder indicates preferential enrichment of 5 6 7 300 Re in molybdenite in low-Mo systems compared to higher-Mo ones independent of Mo 8 9 301 grade, discussed further below. 10 11 12 302 3.4 Rhenium concentration and age of system 13 14 303 Golden et al. (2013, [29]) postulated that Re content in molybdenite has increased 15 16 304 over geologic time due to progressive oxidation of the crust. To test this, we plotted all 17 18 19 305 molybdenite Re contents against the age of the hydrothermal system for all data for 20 21 306 which reliable ages were available (Fig. 6). Our compilation shows little meaningful 22 23 24 307 variation with time. The clearest trend is toward better representation of both extremes of 25 26 308 the distribution in younger rocks, suggesting that what Figure 6 evinces is preservation 27 28 29 309 bias in the geological record – younger sites, being better preserved, contain a better 30 31 310 sample of the overall variability of molybdenite Re contents. These data do not show any 32 33 34 311 trends clear enough to support inferences about global geochemical evolution. 35 36 312 37 38 313 4. Potential limitations of the database 39 40 41 314 Several factors may affect the quality of the database presented here. The majority 42 43 315 of its entries come from Re-Os geochronology studies, many of which lack detailed 44 45 46 316 descriptions of the geological context, paragenesis, polytypism, and zoning relationships 47 48 317 of the molybdenite analyzed, and the mineralogy, distribution, textural relationships, and 49 50 51 318 equilibria of the other minerals. Thus, a number of potentially important factors in 52 53 319 molybdenite Re concentration, such as redox state, sulfidation state, and salinity of the 54 55 320 ore-forming environment, cannot be reliably inferred except by the general tendencies of 56 57 58 321 the deposit type. It is quite likely that additional trends in the distribution of Re in 59 60 61 62 63 14 64 65 1 2 3 4 322 molybdenite would emerge with more detailed geological information from individual 5 6 7 323 deposits. Most of the geochronological studies also contain minimal information about 8 9 324 the purity of the molybdenite mineral separate, which can affect the measured Re 10 11 12 325 abundance. 13 14 326 Furthermore, a minority of the Re data in Appendix A came from measurements 15 16 327 made by electron microprobe (EPMA) and laser ablation inductively coupled mass 17 18 19 328 spectrometry (LA-ICP-MS). Recent work has shown that Re is heterogeneously 20 21 329 distributed in molybdenite, with Re concentration varying by an order of magnitude over 22 23 24 330 a scale of 50 microns (John et al., 2017 [1]; Stein et al., 2003 [19]; Kosler et al., 2003 25 26 331 [22]; Stein et al., 2001 [27]; Selby and Creaser, 2004 [30]). The activation volume of an 27 28 3 29 332 EPMA analysis is about 5-10 μm , too small to be representative of the overall Re 30 31 333 content of the bulk of most grains. A comparison of EPMA and LA-ICP-MS analyses of 32 33 34 334 the same samples found that when measured by an LA-ICP-MS spot of 200 μm diameter, 35 36 335 the intra-grain variation is still > 1 order of magnitude (John et al., 2017 [1]). This 37 38 336 indicates that data collected by EPMA, LA-ICP-MS, or any other analytical technique 39 40 41 337 that measures Re concentration in less than the entire molybdenite grain, may differ from 42 43 338 its bulk Re concentration, as found by Stein et al. (2003 [19]); Stein et al. (2001 [27]), 44 45 46 339 Kosler et al. (2003 [22]) and Selby and Creaser (2004 [30]). This is the case even without 47 48 340 considering the large difference in Re concentrations between different molybdenite 49 50 51 341 grains in the same area. Figure 7 shows an example in which Re concentration varies 52 53 342 unsystematically between 22 and 1215 ppm in molybdenite crystals along a single vein 54 55 343 from the Bagdad porphyry Cu-Mo deposit. 56 57 58 59 60 61 62 63 15 64 65 1 2 3 4 344 Fortunately, most Re-Os studies use whole grains of molybdenite, so the 5 6 7 345 anticipated impact on the database is minimal and should affect all deposit and rock types 8 9 346 more or less equally. This is not the case for a related issue, which is that the small 10 11 12 347 numbers of samples of most Re-Os geochronology studies almost certainly underreport 13 14 348 the range of Re content in any given deposit. Molybdenite Re content in the Bagdad 15 16 349 porphyry Cu-Mo deposit ranged from 330 to 642 ppm in the seven analyses on three 17 18 19 350 samples by Barra et al. (2003 [31]). Three hundred and twenty-four analyses of 45 20 21 351 samples from the same deposit by Rathkopf (2015 [32]) found a range from 29 to 1982 22 23 24 352 ppm (Fig. 8), more than twice the range of Re concentrations measured in a follow-up 25 26 353 analysis of 22 randomly selected samples (Rathkopf et al. 2017 [3]). Because most Re-Os 27 28 29 354 papers include fewer than 10 samples from each deposit, much of the range of 30 31 355 molybdenite Re contents in most deposits is probably missing from the literature. 32 33 34 356 The file-drawer effect undoubtedly poses a problem for part of the database. 35 36 357 Ordinary (i.e., not extreme) molybdenite Re concentrations may or may not be 37 38 358 documented, whereas unusually high concentrations are signalized. The sheer abundance 39 40 41 359 of Re-Os geochronological studies provides enough documentation of ordinary 42 43 360 molybdenite Re concentrations to mitigate the file-drawer effect on the larger deposit 44 45 46 361 categories, such as porphyries and unmineralized granites/granodiorites. But in other 47 48 362 deposit types with fewer members, or in deposit types not conventionally dated by the 49 50 51 363 Re-Os method, molybdenite is discussed in print only when it contains extreme Re 52 53 364 concentrations and the datasets are accordingly unrepresentative. 54 55 365 Lastly, there are few data Re analyses available on molybdenum sulfides from 56 57 58 366 low-temperature sediment-hosted systems that contain significant total Re (John et al., 59 60 61 62 63 16 64 65 1 2 3 4 367 2017 [1]). Other potential Re hosts in ore deposits, such as jordisite, rheniite, and other 5 6 7 368 sulfides, are not considered in any of the analyses presented here. 8 9 369 10 11 12 370 5. Discussion 13 14 371 The results of this study corroborate and extend several of the trends observed in 15 16 372 molybdenite Re content in previous work, while contradicting a few others. On the 17 18 19 373 causes of these trends we have many thoughts but few conclusions. 20 21 374 5.1 Correlation of molybdenite Re content with deposit type 22 23 24 375 Terada et al. (1971 [5]) suggested that molybdenite Re content is highest in 25 26 376 volcanic sublimates, next highest in porphyry deposits, and decreases systematically 27 28 29 377 through skarns and quartz vein-hosted deposits. Our database offers limited support for 30 31 378 this. Data are scattered, but the ten deposit types with the highest molybdenite Re content 32 33 34 379 include four of the six classes of porphyries. Molybdenite from deposits classified as 35 36 380 skarns is nearly as enriched, although this trend is based on a much smaller dataset. 37 38 381 Quartz vein-hosted deposits have much lower Re in molybdenite. 39 40 41 382 In molybdenites from IOCG deposits, Re content is highly variable and does not 42 43 383 show any consistent trends with metal endowment or grade. The eventual Re content of 44 45 46 384 IOCG molybdenite is most likely a function of the Re content of the metal source and of 47 48 385 the geochemical processes involved in molybdenite precipitation. Given the diverse 49 50 51 386 possible metal sources and the sulfur-limited nature of IOCG deposits (Barton, 2014 52 53 387 [33]), it seems most likely that controls on IOCG molybdenite Re contents may be case- 54 55 388 specific. 56 57 58 59 60 61 62 63 17 64 65 1 2 3 4 389 Molybdenite Re content is low in the granite/granodiorite Mo systems and in 5 6 7 390 greisens, and only slightly higher in the intrusion-related class. There are several possible 8 9 391 explanations for this. One is igneous rock type, discussed below. Another is 10 11 12 392 superimposed partial melting and migmatization at several of the granites and 13 14 393 granodiorites in the database, such as Kataberget and Allebuoda. Stein (2006, [34]) 15 16 394 documented that the molybdenite recrystallized by such processes contain less Re than 17 18 19 395 the original molybdenite. The fact that several of the deposits were metamorphosed 20 21 396 suggests that recrystallization may have contributed to the typically low Re of 22 23 24 397 molybdenite in the granite-related class of deposits in the database. An additional 25 26 398 possibility is that the hydrothermal systems associated with these systems were too weak, 27 28 29 399 too small, or too poorly focused to extract much Re from the source magma, however 30 31 400 much Re it may have contained. 32 33 34 401 Pegmatite deposits had a generally bimodal distribution of molybdenite Re 35 36 402 contents with Re either < 40 or > 400 ppm (Fig. 2); only four data points fall between 37 38 403 these extremes. The lower concentrations would be surprising if Re behaves incompatibly 39 40 41 404 during differentiation as does Mo (Mackenzie and Canil, 2011 [35]). One possible 42 43 405 explanation for the bimodal distribution is that in some pegmatites molybdenite 44 45 46 406 crystallized after the magma lost most of its Re to either an escaping fluid or to a Re- 47 48 407 sequestering phase, such as a magmatic sulfide, that had already formed. On the other 49 50 51 408 hand, pegmatite being a textural term, the differences could reflect original magmatic Re 52 53 409 contents given differences in sources or assimilant(s) as well as in differentiation 54 55 410 processes. 56 57 58 59 60 61 62 63 18 64 65 1 2 3 4 411 One of the most noticeable features of the dataset is the consistent trend from 5 6 7 412 higher molybdenite Re contents in Cu- and Au-dominated systems to intermediate 8 9 413 concentrations in Mo-dominated systems and to very low concentrations in their W- and 10 11 12 414 Sn-dominated equivalents. This is observed in the porphyry, skarn, and quartz vein- 13 14 415 hosted classes of deposits, and may be the case in intrusion-related deposits (Fig. 2). In 15 16 416 view of the long-established links between porphyry mineralization and the formation of 17 18 19 417 several kinds of skarn (e.g. Newberry, 1979 [6]), these similarities are unsurprising. 20 21 418 Porphyry and skarn deposits are both magmatic-hydrothermal but are distinct from 22 23 24 419 quartz vein-hosted deposits, which can originate from a variety of geological processes. 25 26 420 The fact that the same pattern occurs in all three deposit types, and perhaps in intrusion- 27 28 29 421 related systems as well, suggests that the concentration of Re in molybdenite is controlled 30 31 422 by underlying geochemical factors. The two likeliest are magma composition and redox 32 33 34 423 chemistry, since these are the principal characteristics that distinguish the Cu- and Au- 35 36 424 dominated from the W- and Sn-dominated types of porphyry and skarn system (Einaudi 37 38 425 et al., 1981 [36]; Burnham and Ohmoto, 1980 [37]; Einaudi et al., 2003 [38]). 39 40 41 426 Results from other deposits unrelated to magmatism suggest a broader range of 42 43 427 geochemical factors affect Re concentration in molybdenite, in particular the Re 44 45 46 428 enrichments in sediment-hosted systems (John et al., 2017 [1]). However, these other 47 48 429 deposit types are represented in the database by samples taken from fewer than ten 49 50 51 430 deposits apiece, so little meaningful discussion is possible. 52 53 431 5.2 Correlation of molybdenite Re content with igneous compositions 54 55 432 There is a clear tendency for molybdenite associated with intermediate- 56 57 58 433 composition igneous rocks to have more Re than molybdenite associated with felsic 59 60 61 62 63 19 64 65 1 2 3 4 434 rocks, but this tendency may not correspond to a precise genetic basis due to the nature of 5 6 7 435 the data in the database. Most of the data for intermediate igneous rocks come from Cu- 8 9 436 and Au-dominated porphyries, which are typically fairly oxidized (QFM +3 or higher) 10 11 12 437 magmas (Einaudi et al., 2003 [38]; Seedorff et al., 2005 [39]). By contrast, most of the 13 14 438 molybdenite Re data associated with felsic rocks comes from Mo-, Sn-, and W- 15 16 439 dominated porphyries and unmineralized granite systems, all of which form from less 17 18 19 440 oxidized (QFM +1 to +2) magmas (Seedorff et al., 2005 [39]). There are few data from 20 21 441 felsic systems that are not also reduced and lower-sulfidation, and few data from 22 23 24 442 intermediate-composition systems that are not also oxidized and higher-sulfidation. 25 26 443 Thus, the observed correlation between higher molybdenite Re and intermediate rocks 27 28 29 444 may reduce to a correlation between higher Re and arc magmas, and/or higher Re and 30 31 445 more oxidized magmas. 32 33 34 446 A comparison of the Re content in bulk igneous rocks could clarify whether the 35 36 447 apparent variation in molybdenite Re contents with igneous compositions is real or is a 37 38 448 secondhand reflection of oxidation state. Unfortunately, existing data on bulk Re 39 40 41 449 concentrations in igneous rocks are scanty and mostly drawn from volcanic samples, 42 43 450 which may have less Re than their intrusive equivalents owing to pre-eruptive degassing 44 45 46 451 (Sun et al., 2004 [40]). A January 2016 search of the GeoROC database 47 48 452 (http://georoc.mpch-mainz.gwdg.de/georoc/) yielded a handful of Re and Mo whole-rock 49 50 51 453 data on igneous rocks. Plotting Re concentration with respect to silica content among the 52 53 454 results shows that rhyolite has, if anything, higher bulk rock Re concentrations than 54 55 455 basalt (Fig. 9). There are fewer samples for intermediate compositions, but what data 56 57 58 456 exist indicate that the Re contents of intermediate rocks fall between those of basalt and 59 60 61 62 63 20 64 65 1 2 3 4 457 rhyolite. Extrapolated to equivalent intrusive rocks, this implies that the low Re in felsic- 5 6 7 458 associated hydrothermal deposits is not due to a lack of Re in felsic magmas, nor is the 8 9 459 higher Re in intermediate-associated hydrothermal deposits due to Re enrichment in 10 11 12 460 intermediate or mafic rocks. 13 14 461 The very low molybdenite Re in granite and granodiorite Mo systems could be 15 16 462 due to either an inherent lack of Re in these unmineralized systems, or to the lack of an 17 18 19 463 efficient hydrothermal system to concentrate it into molybdenite. There were no data 20 21 464 available on the oxidation states of the unmineralized intrusions or on their bulk rock Re 22 23 24 465 content, but the data presented in Figure 9 suggests that the granite and granodiorite Mo 25 26 466 systems could have high bulk Re despite their low molybdenite Re content. This indicates 27 28 29 467 that the lack of efficient hydrothermal Re scavenging and concentration is probably the 30 31 468 source of the low molybdenite Re in those systems. 32 33 34 469 5.3. Rhenium concentration and mantle influence 35 36 470 Related to the issue of igneous rock type is the question of mantle influence. In 37 38 471 many recent papers on porphyry deposit geochemistry and exploration, a high 39 40 41 472 molybdenite Re concentration (> 50 to 100 ppm) is interpreted as prima facie evidence of 42 43 473 significant mantle contribution, whereas lower concentrations (< 10 ppm) are supposed to 44 45 46 474 represent purely crustal influence and evolved magma compositions (e.g., Stein et al.., 47 48 475 2001 [27]; Mao et al., 1999 [41]; Mao et al., 2013 [42]; Pasava et al., 2016 [43]; Zhong et 49 50 51 476 al., 2017 [44]; McFall et al., 2019 [45]). Although the numerical thresholds used to 52 53 477 distinguish mantle from crustal influence vary from article to article, nearly every Re-Os 54 55 478 geochronology paper published in recent years has contained some version of this Re- 56 57 58 479 based mantle/crust discrimination (for references see Appendix B). 59 60 61 62 63 21 64 65 1 2 3 4 480 The present compilation does not offer conclusive support for this criterion except 5 6 7 481 for the general correlation of high molybdenite Re with less felsic, more intermediate 8 9 482 igneous compositions discussed above. The data show a wide range of Re contents 10 11 12 483 among even similar rock types and significant ambiguity. Highly evolved, felsic rocks 13 14 484 produce molybdenite with Re contents ranging from < 5 ppm (South Mountain Batholith) 15 16 485 to > 1500 ppm (Xamchab). The dacite-associated Myli porphyry deposit averages 1534 17 18 19 486 ppm Re in molybdenite, compared to an average 12 ppm Re in molybdenite from the 20 21 487 diorite-associated Questa porphyry deposit. Appendix A contains many more such 22 23 24 488 examples, and the analysis below indicates that molybdenite Re content results from the 25 26 489 interplay of many different geochemical factors. Mantle influence may be one of these, 27 28 29 490 but the database shows that molybdenite Re content cannot be straightforwardly related 30 31 491 to mantle influence in hydrothermal systems. 32 33 34 492 5.4. Factors affecting Re concentration in hydrothermal molybdenite 35 36 493 More than 85% of the data in the database represent magmatic-hydrothermal and 37 38 494 related systems: porphyry, skarn, greisen, intrusion-related, volcanic sublimate, and 39 40 41 495 quartz vein-hosted deposits, and subeconomic granite and granodiorite Mo. These are the 42 43 496 focus of the following discussion; for IOCG, sediment-hosted, and breccia pipe deposits, 44 45 46 497 the data are too few and the deposits too varied to draw many firm conclusions about 47 48 498 what the trends observed represent. 49 50 51 499 The inverse correlation between Re and Mo grade in porphyries (Fig. 5) 52 53 500 elucidates the factors that govern Re concentration in molybdenite in magmatic- 54 55 501 hydrothermal deposits. Most previous studies that observed this have attributed this 56 57 58 502 correlation to dilution of Re by Mo as total Mo concentration increases from Cu and Cu- 59 60 61 62 63 22 64 65 1 2 3 4 503 Au to Mo porphyry systems (e.g. Newberry, 1979 [6]; Berzina et al., 2005 [7]; Stein et 5 6 7 504 al., 1997 [26]; Stein et al., 2001 [27]; Selby and Creaser, 2001[28]). However, as 8 9 505 discussed above, the results show that dilution can explain only part of the increase in Re 10 11 12 506 concentration with decreasing Mo grade (Fig. 5a-b). Moreover, if the scarcity of 13 14 507 molybdenite were the sole or the principal reason for the high Re in in porphyry Mo 15 16 508 molybdenite, then low-Mo porphyry W and Sn systems would also be expected to have 17 18 19 509 high molybdenite Re, which is contrary to the observations (Fig. 2). Most of the trend, 20 21 510 therefore, reflects other causes: either the low-Mo, high-Re systems have more Re to start 22 23 24 511 with, or Re partitions into the fluid phase more efficiently in low-Mo than in high-Mo 25 26 512 porphyry systems. 27 28 29 513 A higher absolute Re concentration in source rocks is doubtful for most 30 31 514 magmatic-hydrothermal systems. Among porphyries, there is substantial overlap between 32 33 34 515 igneous compositions involved in systems with completely different metal endowments. 35 36 516 Granodiorites and quartz monzonites contribute to some porphyry Mo deposits, and 37 38 517 granites to some low-Mo porphyry Cu deposits. Molybdenite Re content is only 39 40 41 518 marginally higher in granodiorite Mo than in granite Mo systems, but is much lower in 42 43 519 even the granodiorite molybdenite than in molybdenite from the granodiorites associated 44 45 46 520 with porphyry systems of nearly any type. The GeoROC data (Fig. 9) also indicate that 47 48 521 bulk Re is no lower in felsic rocks than in intermediate or mafic ones – if anything, felsic 49 50 51 522 rocks have more Re – and therefore whole-rock Re contents cannot credibly explain why 52 53 523 molybdenite from hydrothermal systems associated with more felsic rocks should have 54 55 524 less Re than those from intermediate ones. 56 57 58 59 60 61 62 63 23 64 65 1 2 3 4 525 The other option, that Re concentration in molybdenite is governed by the 5 6 7 526 efficiency of Re partitioning into the hydrothermal fluid and not by original Re content of 8 9 527 the source rock, is more plausible. The previous work on molybdenite Re concentrations 10 11 12 528 offers several hypotheses, mainly focusing on porphyries, that could explain the greater 13 14 529 partitioning efficiency. 15 16 530 5.4.1 – Possible role of halogens 17 18 19 531 1) Selby and Creaser (2001 [28]) suggested that higher Cl and F contents in 20 21 532 magmatic-hydrothermal fluids lowered their hydroxyl contents and prevented them from 22 23 24 533 efficiently accumulating Mo, thereby increasing the Re/Mo ratio. In this hypothesis, a 25 26 534 higher halogen content in Cu- and Au-dominated porphyries would lead to a higher 27 28 29 535 Re/Mo ratio and higher molybdenite Re content than would form in less halide-rich Mo 30 31 536 porphyry magmas, even if the source rocks associated with all of the systems had the 32 33 34 537 same amount of Re. However, this hypothesis is not geochemically supportable for 35 36 538 several reasons. Hydroxyl content is fixed for any pH by the water-dissociation reaction, 37 38 539 making [OH-] independent of Cl or F content. Rhenium solubility depends weakly if at 39 40 - 41 540 all on pH or [OH ] (Xiong and Wood, 2002 [46]). Fluorite and topaz are common in 42 43 541 many porphyry Mo systems, along with high-salinity fluid inclusions, indicating that 44 45 46 542 porphyry Mo deposits are not deficient in halogens although they still produce 47 48 543 molybdenite with low Re concentrations (Seedorff et al., 2005 [39]; White et al., 1981 49 50 51 544 [47]; Bodnar et al., 2014 [48]). 52 53 545 2) Berzina et al. (2005 [7]) suggested that since Re speciates as aqueous ReCl4 at 54 55 546 supercritical conditions, and increasing [Cl-] increases solubility (Xiong and Wood, 2002 56 57 58 547 [46]), saltier fluids could extract more Re from a porphyry magma and, later, concentrate 59 60 61 62 63 24 64 65 1 2 3 4 548 it in molybdenite. Although geochemically reasonable, this does not explain the varying 5 6 7 549 Re concentrations in molybdenite from different types of porphyries, since there is no 8 9 550 consistent observed difference in salinity in the hydrothermal fluids produced in Cu- 10 11 12 551 dominated, Mo-dominated, or W-Sn porphyry systems (Bodnar et al., 2014 [48]). Low 13 14 552 salinity may contribute to the relatively low molybdenite Re in other deposit types, such 15 16 553 as greisens and quartz vein-hosted deposits (although such deposits also commonly form 17 18 19 554 from saline fluids), but cannot explain the variation observed in porphyries. 20 21 555 5.4.2 – Differential temperature-dependent solubility of Re and Mo 22 23 24 556 3) Giles and Schilling (1972 [4]) proposed that Re content is higher in late, low- 25 26 557 temperature molybdenite than in early, high-temperature molybdenite in porphyries, 27 28 29 558 greisens, and skarns. Xiong and Wood (2002 [46]) agreed, citing the retrograde solubility 30 31 559 of ReS2 from 400-500 ˚C as one reason Re could selectively dissolve from early 32 33 34 560 molybdenite in a cooling system, re-concentrate in the fluid phase, and reprecipitate at 35 36 561 higher concentrations in later, cooler molybdenite. This hypothesis is difficult to evaluate 37 38 562 fully. Hydrothermal activity commences at temperatures near the magmatic solidus and 39 40 41 563 may extend down to 200 ˚C. Where and for how long molybdenite precipitates over this 42 43 564 interval are uncertain and vary from porphyry to porphyry (Seedorff et al., 2005 [39]). 44 45 46 565 Furthermore, there is no significant difference in the ranges of depositional temperatures 47 48 566 between the Cu-Au-dominated and the W-Sn-dominated classes of porphyries, skarns, or 49 50 51 567 quartz vein-hosted deposits. In addition, it is clear from the high molybdenite Re of many 52 53 568 volcanic sublimates in Appendix A that Re can become enriched in hydrothermal 54 55 569 molybdenite at very high temperatures. Without further evidence, we conclude that 56 57 58 570 temperature may play a role in many systems, but temperature does not vary 59 60 61 62 63 25 64 65 1 2 3 4 571 systematically among deposit types the way molybdenite Re content does, and thus 5 6 7 572 cannot be the main reason for the observed trends. 8 9 573 5.4.3 – Differentiation by partitioning during volatile phase separation 10 11 12 574 4) Candela and Holland (1986 [49]) attributed differences in molybdenite Re 13 14 575 content to depth of emplacement, which they thought would lead to more boiling (and 15 16 576 more extensive distillation of Re into the vapor) in Cu-dominated porphyry systems than 17 18 19 577 in the deeper Mo porphyries. However, depth of emplacement is approximately the same 20 21 578 for Cu-dominated and Mo-dominated porphyries, and both types of systems show signs 22 23 24 579 of repeated boiling (Seedorff et al., 2005 [39]). Moreover, phase separation is complex 25 26 580 and its role in concentrating Re is ambiguous. A fluid exsolving from a decompressing 27 28 29 581 magma may consist of a single phase or may separate into a brine and a vapor, depending 30 31 582 on the pressure, temperature, and composition of the magmatic system relative to the 32 33 34 583 brine-vapor solvus (Fournier, 1999 [50]). An exsolved single-phase fluid may, or may 35 36 584 not, later undergo additional separation through expansion ± cooling or through boiling 37 38 585 (Burnham and Ohmoto, 1980 [37]). All these processes are known to occur extensively 39 40 41 586 in both Cu-dominated and Mo-dominated porphyries, as well as in other types of deposits 42 43 587 (Burnham and Ohmoto, 1980 [37]). Since Re can exist as ReCl4 or as H2ReO4, it is 44 45 46 588 theoretically capable of entering any of the fluid phases produced by phase separation 47 48 589 (Xiong and Wood, 2002 [46]; Bernard et al., 1990 [51]). Thus, key factors in determining 49 50 51 590 actual Re concentration and distribution in molybdenite in any magmatic-hydrothermal 52 53 591 setting are how many fluid phases exist, how Re partitions among them, and whether or 54 55 592 not they remain in contact with the Re source. 56 57 58 59 60 61 62 63 26 64 65 1 2 3 4 593 The database does not offer much insight into how phase separation affects 5 6 7 594 molybdenite Re content. Rhenium-rich vapors were clearly present in volcanic 8 9 595 sublimates, which are represented by a very small sample set (4 occurrences) in the 10 11 12 596 database. The molybdenite grains they contain are universally enriched in Re, which has 13 14 597 been attributed to strong partitioning of rhenic acid into the low-salinity vapor phase 15 16 598 during boiling (Voudouris et al., 2013 [8]); Xiong and Wood, 2002 [46]; Korzhinsky et 17 18 19 599 al., 1994 [52]). However, other deposits commonly associated with phase separation 20 21 600 (such as greisens) show no evidence of Re enrichment in molybdenite (Burt, 1981 [53]). 22 23 24 601 And molybdenite in the Talnakh deposit contains Re in concentrations comparable to 25 26 602 volcanic-sublimate molybdenite, but with no evidence for phase separation other than the 27 28 29 603 exsolution of sulfide and silicate melts (Kovalenker et al., 1974 [54]; Arndt et al., 2003 30 31 604 [55]). The database contains only three epithermal deposits, none of which has high Re. 32 33 34 605 While none of these facts is clear evidence that molybdenite Re content is independent of 35 36 606 boiling, their accumulation does show that boiling and phase separation do not by 37 38 607 themselves capable ensure high-Re molybdenite. 39 40 41 608 5.4.4 – Role of oxidation state 42 43 609 5) Berzina et al. (2005 [7]), Xiong and Wood (2002 [46]), Bernard et al. (1990 44 45 46 610 [51]), and Li (2014 [56]) focused on oxidation state and the availability of sulfide as 47 48 611 controls on Re partitioning efficiency and eventual molybdenite Re content. This is 49 50 51 612 supported by the demonstrated immobility of Re in reduced systems and concentration of 52 53 613 Re in the fluid phase in oxidized systems (e.g. Xiong and Wood, 2002 [46]; Colodner et 54 55 614 al., 1993 [57]; Xiong and Wood, 2001 [58]; Helz and Dolor, 2012 [59]). Unlike Re, Mo 56 57 58 615 is not especially mobile under oxidizing conditions, so an oxidizing fluid phase also has a 59 60 61 62 63 27 64 65 1 2 3 4 616 substantially higher Re/Mo ratio than the bulk rock (as suggested by Fig. 5a). Conversely, 5 6 7 617 low fO2 limits both the mobility of Re and its selective enrichment over Mo. 8 9 618 As noted above, porphyries, skarns, and quartz vein-hosted deposits all show a 10 11 12 619 trend from low molybdenite Re in relatively reduced W and Sn systems to high 13 14 620 molybdenite Re in relatively oxidized Cu and Au systems (Einaudi et al., 2003 [38]). 15 16 621 Oxidation state is the only fundamental geochemical difference among these deposit 17 18 19 622 subtypes, and it varies systematically in the same way that molybdenite Re concentration 20 21 623 varies. Thus we conclude that redox state is probably the fundamental control on Re 22 23 24 624 concentration in molybdenite, although ancillary factors such as molybdenite abundance, 25 26 625 temperature, salinity, and the strength of the hydrothermal system may be involved. 27 28 29 626 5.4.5 – Interplay of redox, sulfur, and magma sources in hydrothermal deposits 30 31 627 Major controls on the sulfide content and oxidation state of a magmatic- 32 33 34 628 hydrothermal system are magma chemistry, crustal assimilation, and the incursion of 35 36 629 external fluids. While oxidation state and sulfide availability vary over time, in general 37 38 630 the I-type magmas that produce Cu-dominated porphyries are strongly oxidized 39 40 41 631 compared to the Mo-, W-, and Sn-dominated porphyries and even ordinary arc magmas 42 43 632 (Einaudi et al., 2003 [38]). Although true S-type magmas are rare, most W- and Sn- 44 45 46 633 dominated systems have absorbed significant amounts of sedimentary rocks, which are 47 48 634 commonly reduced. Since reduced sediments are commonly enriched in Re up to several 49 50 51 635 hundred ppb (Helz and Dolor, 2012 [59]), this assimilation could have the simultaneous 52 53 636 and contradictory effects of increasing Re concentration in the magma while also 54 55 637 reducing much of its sulfur to sulfide, limiting Re solubility in the hydrothermal phase 56 57 58 638 and producing low-Re molybdenite. Conversely, the assimilation of more oxidized 59 60 61 62 63 28 64 65 1 2 3 4 639 metasedimentary or metavolcanic rocks, while probably adding little to the magmatic Re 5 6 7 640 inventory, would not detract from the efficiency of Re partitioning into the hydrothermal 8 9 641 fluid. Similarly, typically reduced conditions of formation coupled with available sulfide 10 11 12 642 explain the low molybdenite Re among the greisen deposits in the database. Most (13 of 13 14 643 the 18) greisens in the database are relatively reduced W-Sn systems. Thus the control by 15 16 644 oxidation state and reduced sulfur content offers an adequate explanation for the patterns 17 18 19 645 observed in the porphyry, skarn, and quartz vein-hosted deposit classes (possibly for the 20 21 646 intrusion-related class as well) and for the low Re in molybdenite from greisens. 22 23 24 647 5.4.6 – Insights from calc-alkaline volcanic systems 25 26 648 Redox state may also help explain the extraordinary Re enrichment in 27 28 29 649 molybdenite from volcanic sublimates. Volcanic sublimate gases are typically rich in SO2 30 31 650 but often contain abundant H2S (Einaudi et al., 2003 [38]; Taran et al., 1995 [60]). The 32 33 34 651 vent gases are also variably, sometimes highly, enriched in overall Re and in Re/Mo ratio 35 36 652 (Taran et al., 1995 [60]; Crowe et al., 1987 [61]; Zelenski et al., 2014 [62]), and would 37 38 653 tend to become more enriched in Re relative to Mo with distance from the vent since the 39 40 41 654 high H2S inhibits long-distance transport of Mo as the gas cools (Bernard et al., 1990 42 43 655 [51]). Under the appropriate circumstances, such as an oxidizing gas carried far from the 44 45 46 656 vent, extremely Re-rich molybdenite and rheniite could precipitate when the gas cools. 47 48 657 The volcanic sublimate dataset probably suffers from a severe case of the file- 49 50 51 658 drawer effect. This is also true of other deposit types, but the skewing effects of the 52 53 659 reports of extreme Re enrichment (e.g. Voudouris et al., 2013 [8]) are counterbalanced by 54 55 660 the scores of Re-Os geochemistry papers reporting more representative molybdenite Re 56 57 58 661 contents from these deposit types. Because Re-Os dating is not generally employed to 59 60 61 62 63 29 64 65 1 2 3 4 662 date volcanic sublimates, the only data points in the database on volcanic sublimate 5 6 7 663 molybdenite are the ones highlighting its extraordinary Re content, and molybdenite with 8 9 664 low or moderate Re content, if it exists, is not represented. 10 11 12 665 The low Re in molybdenite from granite and granodiorite Mo is somewhat 13 14 666 enigmatic. As noted above, Re in these subeconomic or barren systems is significantly 15 16 667 depleted compared to all but the lowest-Re porphyries and intrusion-related deposits (Fig. 17 18 19 668 2), even though they are associated with igneous rocks of generally similar composition 20 21 669 and Re content. Unfortunately, few of the Re-Os studies on the unmineralized systems 22 23 24 670 included information on the redox-sensitive mineralogy, so their redox state is uncertain. 25 26 671 5.5 Implications of rhenium in molybdenite for whole rock contents 27 28 29 672 Although this paper focuses on Re in molybdenite, for that is where virtually all 30 31 673 of the data exist, it is worth considering the overall implications of our results for bulk 32 33 34 674 Mo contents. Comparisons between recovered molybdenite and bulk chemical analyses 35 36 675 suggest, unsurprisingly, that most of the Mo in ore deposits is in molybdenite (e.g. 37 38 676 Fleischer, 1959 [12]). It is difficult to evaluate this for Re as very few whole-rock Re data 39 40 41 677 exist at all, let alone in rocks from ore deposits. However, the vast majority of Re in ore- 42 43 678 bearing rocks must also be in molybdenite, since otherwise the whole-rock Re 44 45 46 679 concentrations would be highly anomalous compared to rocks of similar types. This is 47 48 680 borne out by the lack of detected Re in molybdenite-poor copper concentrates, which 49 50 51 681 contain the sulfides into which Re would otherwise partition (e.g. Germani et al., 1981 52 53 682 [63]). 54 55 683 56 57 58 684 6. Conclusions 59 60 61 62 63 30 64 65 1 2 3 4 685 The principal geochemical control on molybdenite Re content is oxidation state, 5 6 7 686 with sulfide availability having some effect. The variation in molybdenite Re content, 8 9 687 though messy, is systematic with respect to deposit type, igneous composition, and 10 11 12 688 overall Mo content. The highest overall Re contents are found in molybdenites from 13 14 689 volcanic sublimates, but this may be due to a skewed dataset representing only the 15 16 690 highest-Re samples. Molybdenites from greisens and unmineralized granites and 17 18 19 691 granodiorites had the least Re. In porphyries, skarns, quartz vein-hosted, and possibly 20 21 692 intrusion-related deposits, molybdenite Re content is high in Cu- and Au-dominated 22 23 24 693 members of the class and decreases systematically through Mo and W-Sn types. Among 25 26 694 deposits associated with igneous rocks, intermediate compositions correlate with higher 27 28 29 695 molybdenite Re than felsic compositions, except for intrusion-related deposits; by 30 31 696 contrast, whole-rock data from diverse igneous rock types shows that felsic rocks 32 33 34 697 typically have more Re than their intermediate counterparts. Rhenium content of 35 36 698 molybdenite shows a possible negative correlation with Au grade in intrusion-related 37 38 699 deposits based on a very small number of data points, but no correlation with Au or Cu 39 40 41 700 grades in other deposit types. There is, however, a pronounced negative relationship 42 43 701 between porphyry deposit Mo grade and molybdenite Re content. The depletion of Re in 44 45 46 702 molybdenites from high-Mo systems cannot be attributed to mass-balance considerations 47 48 703 alone; Re is selectively enriched in molybdenites in low-Mo porphyries compared to in 49 50 51 704 high-Mo ones. Molybdenite Re content was found to be unrelated to the geological age of 52 53 705 the system. The effect of mantle influence in molybdenite Re concentration was 54 55 706 ambiguous. 56 57 58 59 60 61 62 63 31 64 65 1 2 3 4 707 Variations in redox state and sulfide availability between different deposit types 5 6 7 708 and subtypes offer plausible explanations for nearly all of the observed trends in 8 9 709 molybdenite Re content from systems associated with magmatic-hydrothermal activity. 10 11 12 710 Porphyry, skarn, and quartz vein-hosted systems with high molybdenite Re are oxidized 13 14 711 (Cu- and Au-dominated), whereas the low-Re molybdenites correspond to relatively 15 16 712 reduced environments or those with abundant sulfide (W- and Sn-dominated). 17 18 19 713 Molybdenum-dominated porphyry, skarn, and quartz vein-hosted systems are 20 21 714 intermediate in oxidation state. There are not enough data to be certain, but intrusion- 22 23 24 715 related deposits may exhibit a similar trend. Greisens form under varying conditions, but 25 26 716 almost always in the presence of preexisting magmatic sulfide, which limits Re solubility. 27 28 29 717 There is no evidence of any systematic control by salinity, temperature, pH, or the Re 30 31 718 content of the source rock, although these may exert an effect in specific cases. The effect 32 33 34 719 of boiling is ambiguous, since some deposits formed by boiling have extremely high Re 35 36 720 contents in molybdenites whereas others do not, and some deposits with high-Re 37 38 721 molybdenites show no evidence of boiling. The strength and focusing of the 39 40 41 722 hydrothermal system is also likely to be a factor in the efficiency of Re scavenging from 42 43 723 the magma, and weakness or poor focusing of the fluid system may explain why 44 45 46 724 unmineralized granites and granodiorites have much lower molybdenite Re than their 47 48 725 compositional counterparts in well-mineralized systems. Control of molybdenite Re 49 50 51 726 content by redox state and reduced sulfur concentration is consistent with geochemical 52 53 727 data in the literature indicating that Re is mobile in oxidized, sulfide-poor environments, 54 55 728 and immobile in reduced, sulfide-rich environments. 56 57 58 729 59 60 61 62 63 32 64 65 1 2 3 4 730 Acknowledgments 5 6 7 731 This study was sponsored by Freeport-McMoRan Copper & Gold. In particular, 8 9 732 we thank Richard Leveille who suggested the project originally along with Robert 10 11 12 733 Jenkins and Ralph Stegen, all of Freeport for their support, as well as for providing the 13 14 734 Bagdad samples included in the database. We are also indebted to Eric Seedorff and 15 16 735 Frank Mazdab for their advice on the study. David Selby, Panagiotis Voudouris, Jeff 17 18 19 736 Mauk, and four anonymous reviewers provided helpful comments and suggestions. 20 21 737 22 23 24 738 Conflict of interest statement 25 26 739 On behalf of all authors, the corresponding author states that there is no conflict 27 28 29 740 of interest. 30 31 741 References 32 33 34 742 1. John, D.A., Seal, R.R., II, and Polyak, D.E., 2017, Rhenium, chap. P of Schulz, 35 36 743 K.J., DeYoung, J.H., Jr., Seal, R.R., II, and Bradley, D.C., eds., Critical mineral 37 38 744 resources of the United States—Economic and environmental geology and 39 40 41 745 prospects for future supply: U.S. Geological Survey Professional Paper 1802, p. 42 43 746 P1–P49. 44 45 46 747 2. John, D., and Taylor, R., 2016: By-products of porphyry copper and molybdenum 47 48 748 deposits. Reviews in Economic Geology 18: 137-164. 49 50 51 749 3. Rathkopf, C., Mazdab, F., Barton, I., and Barton, M.D., 2017: Grain-scale and 52 53 750 deposit-scale heterogeneity of Re distribution in molybdenite at the Bagdad 54 55 751 porphyry Cu-Mo deposit, Arizona. Journal of Geochemical Exploration 178: 45- 56 57 58 752 54. 59 60 61 62 63 33 64 65 1 2 3 4 753 4. Giles, D., and Schilling, J., 1972: Variation in rhenium content of molybdenite. 5 6 th 7 754 Proceedings of the 24 International Geological Congress 10: 145-152. 8 9 755 5. Terada, K., Osaki, S., Ishihara, S., and Kiba, T., 1971: Distribution of rhenium in 10 11 12 756 molybdenites from Japan. Geochemical Journal 4: 123-141. 13 14 757 6. Newberry, R., 1979: Polytypism in molybdenite (II): relationships between 15 16 758 polytypism, ore deposition/alteration stages and rhenium contents. American 17 18 19 759 Mineralogist 64: 768-775. 20 21 760 7. Berzina, A., Sotnikov, V., Economou-Eliopoulos, M., and Eliopoulos, D., 2005: 22 23 24 761 Distribution of rhenium in molybdenite from porphyry Cu-Mo and Mo-Cu 25 26 762 deposits of Russia (Siberia) and Mongolia. Ore Geology Reviews 26: 91-113. 27 28 29 763 8. Voudouris, P., Melfos, V., Spry, P.G., Bindi, L., Moritz, R., Ortelli, M., and 30 31 764 Kartal, T., 2013: Extremely Re-rich molybdenite from porphyry Cu-Mo-Au 32 33 34 765 prospects in northeastern Greece: mode of occurrence, causes of enrichment, and 35 36 766 implications for gold exploration. Minerals 3: 165-191. 37 38 767 9. Ciobanu, C., Cook, N., Kelson, C., Guerin, R., Kalleske, N., and Danyushevsky, 39 40 41 768 L., 2013: Trace element heterogeneity in molybdenite fingerprints stages of 42 43 769 mineralization. Chemical Geology 347: 175-189. 44 45 46 770 10. Coope, J.A., 1973: Geochemical prospecting for porphyry copper-type 47 48 771 mineralization – a review: Journal of Geochemical Exploration 2: 81-102. 49 50 51 772 11. Voudouris, P., Melfos, V., Spry, P., Bindi, L., Kartal, T., and Arikas, K., 2009: 52 53 773 Rhenium-rich molybdenite and rheniite in the Pagoni Rachi Mo-Cu-Te-Ag-Au 54 55 774 prospect, northern Greece: Implications for the Re geochemistry of porphyry-style 56 57 58 775 Cu-Mo and Mo mineralization. Canadian Mineralogist 47: 1013-1036. 59 60 61 62 63 34 64 65 1 2 3 4 776 12. Fleischer, M., 1959: The geochemistry of rhenium, with special reference to its 5 6 7 777 occurrence in molybdenite. Economic Geology 54: 1406-1413. 8 9 778 13. Badalov, S.T., Basitova, S.M., and Godunova, L.I., 1962: Distribution of rhenium 10 11 12 779 in central Asia molybdenite. Geokhimiya 9: 813-817. 13 14 780 14. Riley, G.H., 1967: Rhenium concentration in Australian molybdenites by stable 15 16 781 isotope dilution. Geochimica et Cosmochimica Acta 31: 1489-1497. 17 18 19 782 15. Fleischer, M., 1960: The geochemistry of rhenium – addendum. Economic 20 21 783 Geology 55: 607-609. 22 23 24 784 16. Ishihara, S., 1988: Rhenium contents of molybdenites in granitoid-series rocks in 25 26 785 Japan. Economic Geology 83: 1047-1051. 27 28 29 786 17. Gustafson, L., and Hunt, J., 1975: The porphyry copper deposit at El Salvador, 30 31 787 Chile. Economic Geology 70: 857-912. 32 33 34 788 18. McCandless, T.E., Ruiz, J., and Campbell, A.R., 1993: Rhenium behavior in 35 36 789 molybdenite in hypogene and near-surface environments: implications for Re-Os 37 38 790 geochronometry. Geochimica et Cosmochimica Acta 57: 889-905. 39 40 41 791 19. Stein, H., Schersten, A., Hannah, J., and Markey, R., 2003: Subgrain-scale 42 43 792 decoupling of Re and 187Os and assessment of laser ablation ICP-MS spot dating 44 45 46 793 in molybdenite. Geochimica et Cosmochimica Acta 67: 3673-3686. 47 48 794 20. Sinclair, W., Jonasson, I.R., Kirkham, R.V., and Soregaroli, A.E., 2009: Rhenium 49 50 51 795 and other platinum-group metals in porphyry deposits. Geological Survey of 52 53 796 Canada Open File 6181. 54 55 797 21. Sillitoe, R., Perello, J., Creaser, R., Wilton, J., Wilson, A., and Dawborn, T., 56 57 58 798 2017: Age of the Zambian Copperbelt. Mineralium Deposita 52: 1245-1268. 59 60 61 62 63 35 64 65 1 2 3 4 799 22. Kosler, J., Simonetti, A., Sylvester, P., Cox, R., Tubrett, M., and Wilton, D., 5 6 7 800 2003: Laser-ablation ICP-MS measurements of Re/Os in molybdenite and 8 9 801 implications for Re-Os geochronology. Canadian Mineralogist 41: 307-320. 10 11 12 802 23. Lasky, S., 1950: How tonnage and grade relations help predict ore reserves. 13 14 803 Engineering and Mining Journal 151.4: 81-85. 15 16 804 24. Singer, D., 2013: The lognormal distribution of metal resources in mineral 17 18 19 805 deposits. Ore Geology Reviews 55: 80-86. 20 21 806 25. Babo, J., Spandler, C., Oliver, N., Brown, M., Rubenach, M., and Creaser R., 22 23 24 807 2017: The high-grade Mo-Re Merlin deposit, Cloncurry district, Australia: 25 26 808 Paragenesis and geochronology of hydrothermal alteration and ore formation. 27 28 29 809 Economic Geology 112: 397-422. 30 31 810 26. Stein, H., Maarkey, R., Morgan, J., Du, A., and Sun, Y., 1997: Highly precise and 32 33 34 811 accurate Re-Os ages for molybdenite from the East Qinling Molybdenum Belt, 35 36 812 Shaanxi Province, China. Economic Geology 92: 827-835. 37 38 813 27. Stein, H., Markey, R.J., Morgan, J.W., Hannah, J.L., and Scherstén, A., 2001: The 39 40 41 814 remarkable Re-Os chronometer in molybdenite: how and why it works. Terra 42 43 815 Nova 13:6: 479-486. 44 45 46 816 28. Selby, D., and Creaser, R., 2001: Re-Os geochronology and systematics in 47 48 817 molybdenite from the Endako porphyry molybdenum deposit, British Columbia, 49 50 51 818 Canada. Economic Geology 96: 197-204. 52 53 819 29. Golden, J., McMillan, M., Downs, R., Hystad, G., Goldstein, I., Stein, H., 54 55 820 Zimmerman, A., Sverjensky, D., Armstrong, J., and Hazen, R., 2013: Rhenium 56 57 58 59 60 61 62 63 36 64 65 1 2 3 4 821 variations in molybdenite (MoS2): Evidence for progressive subsurface oxidation. 5 6 7 822 Earth and Planetary Science Letters 366: 1-5. 8 9 823 30. Selby and Creaser, 2004: Macroscale NTIMS and microscale LA-MC-ICP-MS 10 11 12 824 Re-Os isotopic analysis of molybdenite: Testing spatial restrictions for reliable 13 14 825 Re-Os age determinations, and implications for the decoupling of Re and Os 15 16 826 within molybdenite. Geochimica et Cosmochimica Acta 68: 3897-3908. 17 18 19 827 31. Barra, F., Ruiz, J., Mathur, R., and Titley, S., 2003: A Re-Os study of sulfide 20 21 828 minerals from the Bagdad porphyry Cu-Mo deposit, northern Arizona, USA. 22 23 24 829 Mineralium Deposita 38: 585-596. 25 26 830 32. Rathkopf, C.A., 2015: Distribution of rhenium concentrations in molybdenite 27 28 29 831 among hydrothermal ore deposits. Unpublished M.S. thesis, University of 30 31 832 Arizona, 27p and digital appendices. 32 33 34 833 33. Barton, M.D., 2014: Iron oxide(-Cu-Au-REE-P-Ag-U-Co) Systems. Treatise on 35 36 834 Geochemistry, 2nd ed., 515-541. 37 38 835 34. Stein, H., 2006: Low-rhenium molybdenite by metamorphism in northern 39 40 41 836 Sweden: Recognition, genesis, and global implications. Lithos 87: 300-327. 42 43 837 35. Mackenzie, J., and Canil, D., 2011: Fluid/melt partitioning of Re, Mo, W, Tl, and 44 45 46 838 Pb in the system haplobasalt-H2O-Cl and the volcanic degassing of trace metals. 47 48 839 Journal of Volcanology and Geothermal Research 204: 57-65. 49 50 51 840 36. Einaudi, M., Meinert, L., and Newberry, R., 1981: Skarn deposits. In: Skinner, B., 52 53 841 ed., Economic Geology 75th Anniversary Volume, p. 317-391. 54 55 842 37. Burnham, C., and Ohmoto, H., 1980: Late-stage processes of felsic magmatism. 56 57 58 843 Mining Geology Special Issue 8: 1-11. 59 60 61 62 63 37 64 65 1 2 3 4 844 38. Einaudi, M., Hedenquist, J., and Inan, E., 2003: Sulfidation state of fluids in 5 6 7 845 active and extinct hydrothermal systems: transitions from porphyry to epithermal 8 9 846 environments. Society of Economic Geologists and Geochemical Society Special 10 11 12 847 Publication 10: 285-314. 13 14 848 39. Seedorff, E., Dilles, J., Proffett, J., Einaudi, M., Zurcher, L., Stavast, W., Johnson, 15 16 849 D., and Barton, M.D., 2005: Porphyry deposits: characteristics and origin of 17 18 19 850 hypogene features. Economic Geology 100th Anniversary Volume 29: 251-298. 20 21 851 40. Sun, W., Bennett., V., and Kamenetsky, V., 2004: The mechanism of Re 22 23 24 852 enrichment in arc magmas: evidence from Lau Basin basaltic glasses and 25 26 853 primitive melt inclusions. Earth and Planetary Science Letters 222: 101-114. 27 28 29 854 41. Mao, J., Zhang, Z., Zhang, Z., and Du, A., 1999: Re-Os isotopic dating of 30 31 855 molybdenites in the Xioaliugou W (Mo) deposit in the northern Qilian mountains 32 33 34 856 and its geological significance. Geochimica et Cosmochimica Acta 63: 1815- 35 36 857 1818. 37 38 858 42. Mao, Z., Cheng, Y., Liu, J., Yuan, S., Wu, S., Xiang, X., and Luo, X., 2013: 39 40 41 859 Geology and molybdenite Re-Os age of the Dahutang granite-related veinlets- 42 43 860 disseminated tungsten ore field in the Jiangxin Province, China. Ore Geology 44 45 46 861 Reviews 53: 422-413. 47 48 862 43. Pasava, J., Svojtka, M., Veselovsky, F., Durisova, J., Ackerman, L., Pour, O., 49 50 51 863 Drabek, M., Halodova, P., and Haluzova, E., 2016: Laser ablation ICPMS study 52 53 864 of trace element chemistry in molybdenite coupled with scanning electron 54 55 865 microscopy (SEM) – An important tool for identification of different types of 56 57 58 866 mineralization. Ore Geology Reviews 72: 874-895. 59 60 61 62 63 38 64 65 1 2 3 4 867 44. Zhong, J., Chen, Y., and Pirajno, F., 2017: Geology, geochemistry, and tectonic 5 6 7 868 settings of the molybdenum deposits in South China: A review. Ore Geology 8 9 869 Reviews 81: 829-855. 10 11 12 870 45. McFall, K., Roberts, S., McDonald, I., Boyce, A., Naden, J., and Teagle, D., 13 14 871 2019: Rhenium enrichment in the Muratdere Cu-Mo (Au-Re) porphyry deposit, 15 16 34 18 17 872 Turkey: Evidence from stable isotope analyses ( S,  O, D,) and laser ablation 18 19 873 inductively coupled plasma mass spectrometry analysis of sulfides. Economic 20 21 22 874 Geology, https://doi.org/10.5382/econgeo.4638. 23 24 875 46. Xiong, Y., and Wood, S., 2002: Experimental determination of the hydrothermal 25 26 876 solubility of ReS2 and the Re-ReO2 buffer assemblage and transport of rhenium 27 28 29 877 under supercritical conditions. Geochemical Transactions 3: 1-10. 30 31 878 47. White, W., Bookstrom, A., Kamilli, R., Ganster, M., Smith, R., Ranta, D., and 32 33 34 879 Steininger, R., 1981: Character and origin of Climax-type molybdenum deposits. 35 36 880 In: Skinner, B., ed., Economic Geology 75th Anniversary Volume: 270-316. 37 38 39 881 48. Bodnar, R., Lecumberri-Sanchez, P., Moncada, D., and Steele-MacInnis, M., 40 41 882 2014: Fluid inclusions in hydrothermal ore deposits. Treatise on Geochemistry 2nd 42 43 883 ed., 119-142. 44 45 46 884 49. Candela, P.A., and Holland, H.D., 1986: A mass transfer model for copper and 47 48 885 molybdenum in magmatic hydrothermal systems: the origin of porphyry-type ore 49 50 51 886 deposits. Economic Geology 81: 1-19. 52 53 887 50. Fournier, R., 1999: Hydrothermal processes related to movement of fluid from 54 55 56 888 plastic into brittle rock in the magmatic-epithermal environment. Economic 57 58 889 Geology 94: 1193-1211. 59 60 61 62 63 39 64 65 1 2 3 4 890 51. Bernard, A., Symonds, R.B., and Rose, W.I., 1990: Volatile transport and 5 6 7 891 deposition of Mo, W and Re in high temperature magmatic fluids. Applied 8 9 892 Geochemistry 5: 317-326. 10 11 12 893 52. Korzhinsky, M.A., Tkachenko, S.I., Shmulovich, K.I., Taran, Y., and Steinberg, 13 14 894 G.S., 1994: Discovery of a pure rhenium mineral at Kudriavy volcano. Nature 15 16 895 369: 51-52. 17 18 19 896 53. Burt, D., 1981: Acidity-salinity diagrams – application to greisen and porphyry 20 21 897 deposits. Economic Geology 76: 832-843. 22 23 24 898 54. Kovalenker, V., Laputina, I., and Vyal’sov, L., 1974: Rhenium-rich molybdenite 25 26 899 from the Talnakh copper-nickel deposit (Noril’sk region). Doklady Akademii 27 28 29 900 Nauk SSSR 217: 187-189. 30 31 901 55. Arndt, N., Czamanske, G., Walker, R., Chauvel, C., and Fedorenko, V., 2003: 32 33 34 902 Geochemistry and origin of the intrusive hosts of the Noril’sk-Talnakh Cu-Ni- 35 36 903 PGE sulfide deposits. Economic Geology 98: 495-515. 37 38 904 56. Li, Y., 2014: Comparative geochemistry of rhenium in oxidized arc magmas and 39 40 41 905 MORB and rhenium partitioning during magmatic differentiation. Chemical 42 43 906 Geology 386: 101-114. 44 45 46 907 57. Colodner, D., Sachs, J., Ravizza, G., Turekian, K., Edmond, J., and Boyle, E., 47 48 908 1993: The geochemical cycle of rhenium: a reconnaissance. Earth and Planetary 49 50 51 909 Science Letters 117: 205-221. 52 53 910 58. Xiong, Y., and Wood, S., 2001: Hydrothermal transport and deposition of 54 55 911 rhenium under subcritical conditions (up to 200 ˚C) in light of experimental 56 57 58 912 studies. Economic Geology 96: 1429-1444. 59 60 61 62 63 40 64 65 1 2 3 4 913 59. Helz, G.R., and Dolor, M.K., 2012: What regulates rhenium deposition in euxinic 5 6 7 914 basins? Chemical Geology 304-305:131-141. 8 9 915 60. Taran, Y., Hedenquist, J., Korzhinsky, M., Tkachenko, S., and Shmulovich, K., 10 11 12 916 1995: Geochemistry of magmatic gases from Kudryavy volcano, Iturup, Kuril 13 14 917 Islands. Geochimica et Cosmochimica Acta 59: 1749-1761. 15 16 918 61. Crowe, B., Finnegan, D., Zoller, W., and Boynton, W., 1987: Trace element 17 18 19 919 geochemistry of volcanic gases and particles from 1983-1984 eruptive episodes of 20 21 920 Kilauea volcano. Journal of Geophysical Research 92: 13708-13714. 22 23 24 921 62. Zelenski, M., Malik, N., and Taran, Y., 2014: Emissions of trace elements during 25 26 922 the 2012-2013 effusive eruption of Tolbachik volcano, Kamchatka: enrichment 27 28 29 923 factors, partition coefficients and aerosol contribution. Journal of Volcanology 30 31 924 and Geothermal Research 285: 136-149. 32 33 34 925 63. Germani, M., Small, M., Zoller, W., and Moyers, J., 1981: Fractionation of 35 36 926 elements during copper smelting. Journal of the American Chemical Society 15.3: 37 38 927 299-305. 39 40 41 928 42 43 929 Figure Captions 44 45 46 930 1. Histogram of Re concentrations in molybdenite, showing lognormal distribution. 47 48 931 2. Geometric means, arithmetic means, and first and third quartiles of Re content in 49 50 51 932 molybdenites from different types of hydrothermal systems. 52 53 933 3. Comparison of molybdenite Re content in hydrothermal systems associated with 54 55 934 igneous rocks, showing that molybdenite Re content is typically higher in systems 56 57 58 59 60 61 62 63 41 64 65 1 2 3 4 935 associated with intermediate rocks than in those associated with felsic rocks. 5 6 7 936 Symbols and colors as in Fig. 2. 8 9 937 4. Relationship of molybdenite Re content to (A) Au grade in intrusion-related 10 11 12 938 deposits; (B) Au grade in porphyry deposits; (C) Cu grade in IOCG and skarn 13 14 939 deposits; and (D) Cu grade in porphyry deposits. 15 16 940 5. (A) Schematic diagram of the relationship of molybdenite Re content to Mo 17 18 19 941 grade, showing bulk rock Re concentrations (dashed lines) assuming all Re and 20 21 942 Mo exist as molybdenite. Rocks enriched in Re and Mo while maintaining the 22 23 24 943 Re/Mo ratio of bulk Earth crust plot on the solid black line; rocks preferentially 25 26 944 enriched in one element compared to the other will plot in the gray (Re enriched) 27 28 29 945 or red (Mo enriched) zones. The dashed red line with a slope of -1 shows the 30 31 946 theoretical positions of two rocks with equal bulk Re concentration diluted 32 33 34 947 through more (point a) or less (point b) molybdenite. This differs significantly 35 36 948 from the regression line of actual porphyry Re-Mo data in (B) (red line, slope = - 37 38 949 0.4, R2 = 0.29), showing that Re enrichment in Mo-poor (Cu-dominated) 39 40 41 950 compared to Mo-rich porphyries is significantly more than can be attributed to 42 43 951 dilution of Re through more or less molybdenite. However, virtually all 44 45 46 952 porphyries are enriched in Re compared to crustal averages. See text for 47 48 953 discussion. 49 50 51 954 6. Rhenium contents of molybdenites plotted by age of hydrothermal system, 52 53 955 omitting those deposits for which no dates are available and deposit categories 54 55 956 represented by fewer than four members. 56 57 58 59 60 61 62 63 42 64 65 1 2 3 4 957 7. Variable Re concentrations in molybdenite crystals along individual veins in a 5 6 7 958 sample from the Bagdad porphyry Cu-Mo deposit, Arizona, based on electron 8 9 959 probe microanalyzer data Modified from Rathkopf (2015 [32]) and Rathkopf et al. 10 11 12 960 (2017 [3]). 13 14 961 8. Dependence of range of molybdenite Re content at the Bagdad porphyry Cu-Mo 15 16 962 deposit on number of samples analyzed. Analyses are by EPMA (Rathkopf et al., 17 18 19 963 2017 [3]), NTIMS (Barra et al., 2003 [31]), and LA-ICP-MS (Barton, unpublished 20 21 964 data). 22 23 24 965 9. Bulk Re content of different igneous rock types, using whole-rock geochemical 25 26 966 data from GeoROC. 27 28 29 967 30 31 968 Table Captions 32 33 34 969 1. Statistics of Re distribution in molybdenites, by deposit type. 35 36 970 2. Statistics of Re distribution in molybdenites, by type of associated igneous rocks. 37 38 971 39 40 41 972 Digital Appendices / Supplemental Data 42 43 973 A. Excel spreadsheet database of >3,000 Re concentrations in molybdenite, with deposit 44 45 46 974 type, metal grades, deposit ages, references, and sample and analytical types so far as 47 48 975 could be determined. 49 50 51 976 B. References to literature used in compilation of Re concentrations in database. 52 53 977 C. Explanation of the criteria and references used to assign classifications to deposits not 54 55 978 clearly affiliated with one particular category. 56 57 58 59 60 61 62 63 43 64 65 Table 1 Click here to access/download;Table;Table1_new_ReMolyDatabase.docx

Table 1. Statistics from deposit-wide geometric means Statistics from individual Re data points Deposit type: # of Re # of 25th 75th Geometric 25th median 75th Geometric data deposits percentile percentile mean percentile percentile mean Breccia pipe 13 9 6.3 38 10 6.3 16 35 10 Barren granite / granodiorite 244 85 4.2 45 12 2.3 11 30 8.4 Greisen 106 18 0.2 3.2 1.3 0.1 0.5 5.1 0.8 Intrusion-related 73 16 4.3 102 24 14 31 113 29 IOCG 144 20 21 204 77 105 679 1065 363 Orogenic/ metamorphic 29 5 14 152 54 3.4 10 46 15 Pegmatite 34 14 15 325 53 15 69 430 67 Porphyry, all 1551 291 36 588 147 46 174 459 139 Porphyry Au and Au-Cu 10 5 186 1020 321 25 187 757 130 Porphyry Cu-Au 100 28 174 1660 428 191 551 1189 408 Porphyry Cu 328 86 200 962 471 133 397 847 340 Porphyry Cu-Mo 789 88 83 529 191 84 200 412 171 Porphyry Mo 317 80 11 49 23 11 25 57 26 Porphyry W/Sn 7 4 12 75 16 0.8 1.3 38 3.7 Quartz vein-hosted, all 367 125 2.8 86 15 2.3 19 81 12 Quartz vein-hosted Au 11 5 2.8 85 18 2.6 2.8 60 8.5 Quartz vein-hosted Cu 9 5 8.6 95 29 77 79 92 46 Quartz vein-hosted Mo 108 49 3.3 57 11 4.1 11 37 9.5 Quartz vein-hosted W/Sn 36 16 0.9 5.3 2.1 0.4 1.6 7.5 1.5 Sediment-hosted 21 6 10 131 23 10 11 34 19 Skarn, all 220 58 20 146 52 19 58 180 51 Skarn Au 20 6 406 671 542 343 565 860 596 Skarn Cu and Cu-Au 41 11 41 223 77 24 45 127 49 Skarn Cu-Mo 30 4 61 515 176 53 185 674 156 Skarn Fe 6 3 707 1430 555 365 1300 1400 543 Skarn Mo 39 9 21 72 40 25 61 98 55 Skarn Pb-Zn 10 4 11 34 17 3.6 14 32 9.6 Skarn W-Sn 68 18 7.3 50 17 4.7 42 81 20 VMS 7 3 4.5 849 27 1.4 1.8 5.2 2.5

Table 2 Click here to access/download;Table;Table2_new_ReMolyDatabase.docx

Table 2. Based on deposit-wide geometric means Based on individual Re statistics Percentiles Percentiles System and rock type # of data # of 25th 50th 75th Geometric 25th 50th 75th Geometric points deposits mean mean Barren granite/ Felsic 127 45 7.5 14 40 12 3.9 12 30 9.5 granodiorite Intermediate 42 12 4.0 7.8 18 11 3.5 13 37 17 Intrusion-related Felsic 20 4 17 97 235 37 15 142 182 48 Intermediate 32 8 23 37 162 33 19 61 92 45 Porphyry Felsic 357 72 16 49 251 60 17 71 261 69 Intermediate 1009 147 75 220 701 212 71 200 496 172 Quartz vein- Felsic 238 74 3.6 24 76 13 2.5 18 74 11 hosted Intermediate 41 19 16 103 123 43 50 110 160 68 Skarn Felsic 77 21 14 29 50 29 24 44 91 49 Intermediate 45 15 89 335 566 159 53 261 665 152

Figure 1 Click here to access/download;Figure;Fig1ReMolyHistogram.tif Figure 2 Click here to access/download;Figure;Fig2ReMolyDepType_New.tif Figure 3 Click here to access/download;Figure;Fig3ReMolyIgneousType.tif Figure 4 Click here to access/download;Figure;Fig4ReMolyMetGradeNew.tif Figure 5 Click here to access/download;Figure;Fig5ReMolyMoGrade.tif Figure 6 Click here to access/download;Figure;Fig6ReMolyAge_New.tif Figure 7 Click here to access/download;Figure;Fig7ReVariationSample.tif Figure 8 Click here to access/download;Figure;Fig8ReMolyBagdadComparison.tif Figure 9 Click here to access/download;Figure;Fig9GeoROC_new_ReMo.tif Appendix A

0 = none or unknown Deposit-wide grades Deposit name ppm Re error, ppm n, Re Re_min Re_max Deposit Type Associated Igneous Rocks %Cu %Mo g/t Au Age, Ma Source Sample type Analysis type A34 10.887 0.026 1 Unknown Cu 0 0 0 0 2648 (Markey et al., 1998) Mo powder NTIMS A34 11.14 0.027 1 Unknown Cu 0 0 0 0 2648 (Markey et al., 1998) Mo powder NTIMS A34 11.297 0.026 1 Unknown Cu 0 0 0 0 2648 (Markey et al., 1998) Mo powder NTIMS A34 18.915 0.069 1 Unknown Cu 0 0 0 0 2648 (Markey et al., 1998) Mo powder NTIMS A34 20.954 0.045 1 Unknown Cu 0 0 0 0 2648 (Markey et al., 1998) Mo powder NTIMS A950 52.256 0.214 1 Unknown Cu 0 0 0 0 2696 (Markey et al., 1998) Mo powder NTIMS A950 57.826 0.133 1 Unknown Cu 0 0 0 0 2696 (Markey et al., 1998) Mo powder NTIMS A950 60.503 0.248 1 Unknown Cu 0 0 0 0 2696 (Markey et al., 1998) Mo powder NTIMS A950 95.79 0.22 1 Unknown Cu 0 0 0 0 2696 (Markey et al., 1998) Mo powder NTIMS A950 97 0.21 1 Unknown Cu 0 0 0 0 2696 (Markey et al., 1998) Mo powder NTIMS A950 98.97 0.85 1 Unknown Cu 0 0 0 0 2696 (Markey et al., 1998) Mo powder NTIMS Abdar 4247 162 1 Porphyry Cu diorite 0 0 0 6.3 (Aghazadeh et al., 2015) hand-picked grains unknown Abdar 4467 44 1 Porphyry Cu diorite 0 0 0 6.3 (Aghazadeh et al., 2015) hand-picked grains unknown Adanac 8 1 Porphyry Mo quartz monzonite 0.001 0.062 0 73 (Sinclair et al., 2009) various NAA Adanac 12 2 Porphyry Mo quartz monzonite 0.001 0.062 0 73 (Sinclair et al., 2009) various NAA Adanac 22 1 Porphyry Mo quartz monzonite 0.001 0.062 0 73 (Sinclair et al., 2009) various NAA Agarak 820 106 57 6310 Porphyry Cu-Au diorite; granite; granodiorite 0.56 0.025 0.6 50 (Berzina et al., 2005) various various Aigedzor 780 1 Porphyry Cu-Mo 0 0 0 0 0 (Fleischer, 1960) unknown colorimetry Airshoko 2.7 1 Greisen Mo-Sn-W 0 0 0 0 0 (Fleischer, 1960) unknown colorimetry Aitik 20 1.01 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 42.6 12.6 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 48.1 5.6 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 54.04 0.04 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2005) hand samples NTIMS Aitik 61.3 0.4 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 67.03 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 75.9 0.07 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2005) hand samples NTIMS Aitik 119.61 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 132.8 4.2 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 132.9 12.6 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 171.9 3.8 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 190.7 15.1 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 215.7 0.3 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2005) hand samples NTIMS Aitik 284.3 4.8 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 288.7 4.53 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 741.9 23.5 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 784.4 8.1 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 1474 1 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2005) hand samples NTIMS Aitik 1484 6 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2005) hand samples NTIMS Aitik 84.4 48.800 1 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Nigatu, 2011) micro-drilled hand samples ICP-MS Aitik 20 1.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 289 5.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 120 2.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 67 2.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 148 2.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 172 4.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 784 8.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 92 5.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 467 53.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 60 6.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 1587 25.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 1468 119.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 133 13.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 284 5.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 43 13.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 191 15.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 742 23.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 133 4.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 84 49.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 48 6.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 367 208.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 46 9.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 61 0.400 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 223 3.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aitik 63 3.000 Porphyry Cu porphyry; quartz monzodiorite 0.18 0.002 0.116 1887 (Wanhainen et al., 2014) micro-drilled hand samples ID-ICP-MS Aittojärvi 23.01 0.05 1 Granite Mo 0 0 0 0 2796 (Markey et al., 1998) hand-picked heavy liquid concentrate NTIMS Aittojärvi 23.21 0.05 1 Granite Mo 0 0 0 0 2796 (Markey et al., 1998) hand-picked heavy liquid concentrate NTIMS Aittojärvi 23.73 0.09 1 Granite Mo 0 0 0 0 2796 (Markey et al., 1998) hand-picked heavy liquid concentrate NTIMS Ajax West 3161 1 Porphyry Cu diorite; gabbro; monzonite; picrite 0.288 0.005 0.185 205 (Sinclair et al., 2009) various NAA Ajo 700 600 1 Porphyry Cu andesite 0.576 0.009 0.16 63.1 (McCandless et al., 1993) hand-picked grains EPMA Akchatau 1.2 1 Greisen 0 0 0.055 0 289.3 (Fleischer, 1960) unknown colorimetry Akchatau 2.267 0.021 1 Greisen 0 0 0.055 0 289.3 (Chen et al., 2010) hand samples ICP-MS Akchatau 6.942 0.055 1 Greisen 0 0 0.055 0 289.3 (Chen et al., 2010) hand samples ICP-MS Aksug 460 1 Porphyry Cu-Mo granodiorite; quartz diorite; tonalite 0.67 0.015 0.12 402.5 (Berzina et al., 2005) various various Aktogai 850 30 50 2700 Porphyry Cu 0 0.38 0.008 0.034 333 (Berzina et al., 2005) various various Alattu 174.3 1 Porphyry Cu-Mo 0 0 0 0 0 (Lavrov and Kuleshevich, 2010) unknown SEM Alford 64.2 1 IOCG 0 0.2 0.36 0 1574 (Skirrow et al., 2007) unknown NTIMS Alford 66.44 1 IOCG 0 0.2 0.36 0 1574 (Skirrow et al., 2007) unknown NTIMS Allebuoda 0.5495 0.0005 1 Granite Mo granite 0 0.002 0 1835 (Stein, 2006) hand samples NTIMS Allebuoda 0.5542 0.0005 1 Granite Mo granite 0 0.002 0 1835 (Stein, 2006) hand samples NTIMS Allebuoda 0.615 0.001 1 Granite Mo granite 0 0.002 0 1835 (Stein, 2006) hand samples NTIMS Allebuoda 0.651 0.001 1 Granite Mo granite 0 0.002 0 1835 (Stein, 2006) hand samples NTIMS Allebuoda 1.1894 0.0004 1 Granite Mo granite 0 0.002 0 1835 (Stein, 2006) hand samples NTIMS Allebuoda 1.204 0.001 1 Granite Mo granite 0 0.002 0 1835 (Stein, 2006) hand samples NTIMS Allebuoda 1.758 0.002 1 Granite Mo granite 0 0.002 0 1835 (Stein, 2006) hand samples NTIMS Allebuoda 3.809 0.002 1 Granite Mo granite 0 0.002 0 1835 (Stein, 2006) hand samples NTIMS Allebuoda 3.835 0.003 1 Granite Mo granite 0 0.002 0 1835 (Stein, 2006) hand samples NTIMS Allebuoda 3.897 0.001 1 Granite Mo granite 0 0.002 0 1835 (Stein, 2006) hand samples NTIMS Allebuoda 4.288 0.002 1 Granite Mo granite 0 0.002 0 1835 (Stein, 2006) hand samples NTIMS Allebuoda 4.705 0.002 1 Granite Mo granite 0 0.002 0 1835 (Stein, 2006) hand samples NTIMS Alpeiner Scharte 0.00546 1 Quartz vein-hosted Mo granitoid 0 0 0 303.4 (Langthaler et al., 2004) micro-drilled hand samples NTIMS Alpeiner Scharte 0.0356 1 Quartz vein-hosted Mo granitoid 0 0 0 303.4 (Langthaler et al., 2004) micro-drilled hand samples NTIMS Altenberg 0.0852 1 Greisen Sn 0 0 0 0 326.4 (Romer et al., 2007) unknown NTIMS Altenberg 0.1207 1 Greisen Sn 0 0 0 0 326.4 (Romer et al., 2007) unknown NTIMS Amanan-Makit 43 5 10 70 Porphyry Mo 0 0 0 0 0 (Berzina et al., 2005) various various Ambalavayal 0.131 0.011 1 Granite Mo 0 0 0 0 0 (Barra, 2005) unknown ICP-MS Ambalavayal 0.383 0.009 1 Granite Mo 0 0 0 0 0 (Barra, 2005) unknown ICP-MS American Eagle 800 400 1 Porphyry Cu granodiorite 0 0 0 82.55 (McCandless et al., 1993) hand-picked grains EPMA American Eagle 3500 3500 1 Porphyry Cu granodiorite 0 0 0 82.55 (McCandless et al., 1993) hand-picked grains EPMA Amudzhikan 82 6 40 170 Porphyry Mo 0 0 0.31 0 0 (Berzina et al., 2005) various various Andacollo 2316 1 Porphyry Cu-Au andesite, dacite 0.71 0.015 0.331 93 (Mathur et al., 2010) hand-picked grains NTIMS Andrzej 7 1 Granite Mo 0 0 0 0 298 (Mikulski and Stein, 2007) micro-drilled hand samples NTIMS Ankavan 220 11 150 340 Porphyry Cu-Mo granodiorite; syenogranite; lamprophyre 0 0 0 33 (Berzina et al., 2005) various various Anticlimax 9 1 Porphyry Mo 0 0 0 0 0 (Sinclair et al., 2009) various NAA Anticlimax 54 2 Porphyry Mo 0 0 0 0 0 (Sinclair et al., 2009) various NAA Anticlimax 96 1 Porphyry Mo 0 0 0 0 0 (Sinclair et al., 2009) various NAA Antietam Reservoir 12.8 1 Granite Mo 0 0 0 0 0 (Mathur et al., 2010) hand-picked grains NTIMS Antietam Reservoir 0.35 1 Granite Mo 0 0 0 0 0 (Mathur et al., 2010) hand-picked grains NTIMS Antietam Reservoir 0.25 1 Granite Mo 0 0 0 0 0 (Mathur et al., 2010) hand-picked grains NTIMS Arburese 0.489 0.001 1 Porphyry Mo leucogranite 0 0 0 290 (Boni et al., 2003) hand samples unknown Arendal 1200 1 Skarn Fe 0 0 0 0 0 (Paganelli, 1963) unknown colorimetry Arendal 1400 1 Skarn Fe 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Arendal 1400 1 Skarn Fe 0 0 0 0 0 (Paganelli, 1963) unknown colorimetry Assarel 692.8 0.2 1 Porphyry Cu granodiorite 0.44 0 1.19 91.435 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Assarel 739 1 Porphyry Cu granodiorite 0.44 0 1.19 91.435 (Voudouris et al., 2013) thin sections EPMA Assarel 784.8 0.2 1 Porphyry Cu granodiorite 0.44 0 1.19 91.435 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Atsuho 80 1 Granite Mo granitoid 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Atsuho 120 1 Granite Mo granitoid 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Axioupolis 300 1 Porphyry Mo alkali-granite 0 0 0 0 (Voudouris et al., 2010) hand samples EPMA Axioupolis 344 9 10 1000 Porphyry Mo alkali-granite 0 0 0 0 (Voudouris et al., 2013) thin sections EPMA Axioupolis 400 1 Porphyry Mo alkali-granite 0 0 0 0 (Voudouris et al., 2010) hand samples EPMA Bagdad 4.63 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 12.47 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 18.67 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 20 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Fleischer, 1959) flotation concentrate unknown Bagdad 20.59 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 21.91 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 329.7 3 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Barra et al., 2003) hand-picked grains NTIMS Bagdad 26.87 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 29.08 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 31.75 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 31.77 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 33.06 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 33.53 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 34.35 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 34.57 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 35.7 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 36.61 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 40.15 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 41.17 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 42.16 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 44.26 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 44.29 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 44.97 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 45.64 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 46.91 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 47.06 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 48.03 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 48.4 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 50.39 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 51.78 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 55.69 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 56.01 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 57.28 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 58.71 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 60.35 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 62.73 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 65.44 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 65.65 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 66.49 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 66.52 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 67.31 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 67.45 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 67.66 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 68.45 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 69.13 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 69.93 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 69.99 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 70.44 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 359.1 4 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Barra et al., 2003) hand-picked grains NTIMS Bagdad 71.2 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 372 4 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Barra et al., 2003) hand-picked grains NTIMS Bagdad 71.57 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 72.33 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 72.97 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 73.29 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 466.9 5 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Barra et al., 2003) hand-picked grains NTIMS Bagdad 506.5 5 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Barra et al., 2003) hand-picked grains NTIMS Bagdad 76.46 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 76.99 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 77.41 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 77.99 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 78.64 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 78.75 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 79.41 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 80.37 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 81.1 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 84.38 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 85.34 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 551.1 6 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Barra et al., 2003) hand-picked grains NTIMS Bagdad 85.64 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 87.47 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 87.61 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 87.73 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 89.14 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 89.36 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 89.82 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 90.18 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 90.18 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 90.66 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 642.3 6 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Barra et al., 2003) hand-picked grains NTIMS Bagdad 92.41 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 92.48 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 93.17 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 93.89 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 96.75 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 97.82 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 97.93 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 99.3 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 99.54 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 99.86 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 100.16 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 102.26 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 102.67 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 103.15 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 107.1 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 110.35 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 110.94 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 113.63 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 114.04 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 114.32 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 115.19 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 115.92 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 117.63 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 117.98 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 118.85 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 123.23 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 123.26 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 123.76 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 126.59 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 129.18 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 129.34 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 131.45 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 134.9 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 135.18 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 137.16 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 137.25 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 137.39 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 137.49 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 138.17 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 138.78 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 143.98 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 144.16 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 144.81 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 145.01 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 145.19 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 146.33 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 148.92 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 148.95 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 154.52 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 156.33 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 156.33 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 156.71 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 159.11 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 159.15 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 159.16 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 165 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 166.17 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 167.34 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 173.45 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 173.82 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 174.71 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 176.02 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 176.4 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 176.45 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 180.02 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 180.02 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 184.62 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 185.13 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 186.64 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 192.26 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 196.16 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 196.82 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 197.25 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 201.02 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 201.43 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 202.23 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 205.9 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 206.28 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 206.74 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 206.89 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 208.11 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 211.77 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 214.5 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 216.54 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 219 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 220.1 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 222.21 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 222.95 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 224.86 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 227.59 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 229.18 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 229.58 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 233.75 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 234.38 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 236.54 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 237.42 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 239.26 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 239.57 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 241.55 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 247.32 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 248.1 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 248.2 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 248.56 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 250.2 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 250.97 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 252.03 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 253.25 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 253.46 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 253.72 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 253.9 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 257.69 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 258.95 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 262.58 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 263.36 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 263.6 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 265.9 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 266.5 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 267.15 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 268.35 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 272.37 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 273.07 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 274.75 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 276.33 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 278.12 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 288.61 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 289.24 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 293.52 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 293.93 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 294.24 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 294.53 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 298.71 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 301.92 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 303.5 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 320.82 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 321.32 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 322.11 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 332.98 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 340.46 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 344.96 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 345.43 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 349.76 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 355.43 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 360.2 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 363.11 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 364.08 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 364.54 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 370.67 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 373.97 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 374.67 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 374.71 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 381.22 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 387.08 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 391.86 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 394.95 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 396.29 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 396.31 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 398.17 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 400 500 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (McCandless et al., 1993) hand-picked grains EPMA Bagdad 404.79 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 408.43 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 408.66 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 409.35 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 411.71 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 417.84 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 422.79 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 423.53 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 431.48 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 431.5 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 438.87 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 439.25 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 442.65 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 458.54 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 461.16 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 462.2 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 465.01 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 465.85 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 468.5 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 469.62 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 487.8 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 492.08 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 494.32 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 495.73 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 500 100 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (McCandless et al., 1993) hand-picked grains EPMA Bagdad 510.99 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 511.64 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 516.2 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 522.42 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 541.29 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 542.27 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 554.05 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 564.11 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 570.41 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 579.2 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 581.78 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 592.6 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 611.78 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 618.6 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (McCandless and Ruiz, 1993) unknown unknown Bagdad 624.77 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 628.04 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 634.2 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 637.05 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 644.65 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 649.04 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 653.47 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 662.68 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 680.37 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 693.51 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 696.43 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 771.82 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 778.89 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 783.11 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 793.82 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 841.6 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 846.9 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 855.38 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 864.1 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 878.76 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 905.23 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 917.27 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 947.77 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 966.31 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 992.32 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1025.13 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1095.04 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1137.38 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1150.05 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1166.15 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1181.76 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1197.7 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1200.36 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1210.97 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1212.32 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1214.75 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1220.71 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1306.54 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1323.9 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1457.23 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1717.5 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1752.21 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1890.34 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 1967.04 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 2061.44 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 2220.97 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 4455.74 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 0 0.021 1 4.233 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 0.1 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 0.1 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 0.1 1 4.248 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 0.1 1 4.272 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 0.1 1 40.38 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 0.1 1 50.54 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 0.1 1 68.43 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 0.1 1 9.87 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 0.57 1 9.878 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 3.97 1 9.921 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (Rathkopf, 2015) polished mounts EPMA Bagdad 94.07 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 73.75 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 50.30 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 50.84 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 27.22 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 15.85 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 25.11 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 29.23 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 91.01 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 126.31 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 198.21 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 18.22 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 19.03 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 20.29 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 18.49 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 23.96 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 20.55 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 46.33 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 19.40 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 29.45 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 35.76 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagdad 22.49 1 Porphyry Cu-Mo quartz monzonite; andesite 0.19 0.02 0.001 73.85 (I. Barton, unpubl. data) polished mounts LA-ICP-MS Bagh Khoshk 451.9 3.5 1 Porphyry Cu granodiorite 0.23 0.11 0 17.85 (Aghazadeh et al., 2015) hand-picked grains unknown Bagh Khoshk 480 4 1 Porphyry Cu granodiorite 0.23 0.11 0 17.85 (Aghazadeh et al., 2015) hand-picked grains unknown Bagh Khoshk 527.6 4.8 1 Porphyry Cu granodiorite 0.23 0.11 0 17.85 (Aghazadeh et al., 2015) hand-picked grains unknown Bagh Khoshk 546 4.7 1 Porphyry Cu granodiorite 0.23 0.11 0 17.85 (Aghazadeh et al., 2015) hand-picked grains unknown Bagh Khoshk 610.3 5.6 1 Porphyry Cu granodiorite 0.23 0.11 0 17.85 (Aghazadeh et al., 2015) hand-picked grains unknown Bagh Khoshk 657.3 5.5 1 Porphyry Cu granodiorite 0.23 0.11 0 17.85 (Aghazadeh et al., 2015) hand-picked grains unknown Baie des Moutons 1 1 Porphyry Mo 0 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Baishan 73.5 0.7 1 Porphyry Mo granite 0 0.06 0 225.5 (Zhang et al., 2005) hand samples ICP-MS Baishan 107.1 1.1 1 Porphyry Mo granite 0 0.06 0 225.5 (Zhang et al., 2005) hand samples ICP-MS Baishan 167.2 1.6 1 Porphyry Mo granite 0 0.06 0 225.5 (Zhang et al., 2005) hand samples ICP-MS Baishan 188 1.8 1 Porphyry Mo granite 0 0.06 0 225.5 (Zhang et al., 2005) hand samples ICP-MS Baishan 194.5 1.7 1 Porphyry Mo granite 0 0.06 0 225.5 (Zhang et al., 2005) hand samples ICP-MS Baishan 211.96 1.83 1 Porphyry Mo granite 0 0.06 0 225.5 (Han et al., 2014b) unknown ICP-MS Baishan 236.7 2.5 1 Porphyry Mo granite 0 0.06 0 225.5 (Zhang et al., 2005) hand samples ICP-MS Baishan 238.2 2.6 1 Porphyry Mo granite 0 0.06 0 225.5 (Zhang et al., 2005) hand samples ICP-MS Baishan 240.39 1.80 1 Porphyry Mo granite 0 0.06 0 225.5 (Han et al., 2014b) unknown ICP-MS Baishan 249.7 2.8 1 Porphyry Mo granite 0 0.06 0 225.5 (Zhang et al., 2005) hand samples ICP-MS Baishan 257.34 1.97 1 Porphyry Mo granite 0 0.06 0 225.5 (Han et al., 2014b) unknown ICP-MS Baishan 261.24 1.95 1 Porphyry Mo granite 0 0.06 0 225.5 (Han et al., 2014b) unknown ICP-MS Baishan 270.83 2.33 1 Porphyry Mo granite 0 0.06 0 225.5 (Han et al., 2014b) unknown ICP-MS Baishan 396.28 2.92 1 Porphyry Mo granite 0 0.06 0 225.5 (Han et al., 2014b) unknown ICP-MS Baishan 561.04 4.18 1 Porphyry Mo granite 0 0.06 0 225.5 (Han et al., 2014b) unknown ICP-MS Baishan 572.77 4.37 1 Porphyry Mo granite 0 0.06 0 225.5 (Han et al., 2014b) unknown ICP-MS Baishan 655.93 5.45 1 Porphyry Mo granite 0 0.06 0 225.5 (Han et al., 2014b) unknown ICP-MS Baishiding 242.3 6 127.3 383.9 Porphyry Mo monzogranite 0 0.12 0 426.4 (Zhong et al., 2017) various various Băiţa Bihor 8.61 0.01 1 Skarn Cu-Mo 0 0 0 0 79.415 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Băiţa Bihor 28.17 0.04 1 Skarn Cu-Mo 0 0 0 0 79.415 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Băiţa Bihor 47.96 0.05 1 Skarn Cu-Mo 0 0 0 0 79.415 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Băiţa Bihor 58.59 0.07 1 Skarn Cu-Mo 0 0 0 0 79.415 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Băiţa Bihor 61.94 0.07 1 Skarn Cu-Mo 0 0 0 0 79.415 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Băiţa Bihor 97.18 0.03 1 Skarn Cu-Mo 0 0 0 0 79.415 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Băiţa Bihor 135.87 0.05 1 Skarn Cu-Mo 0 0 0 0 79.415 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Băiţa Plai 16.6 0.04 1 Granite Mo 0 0 0 0 79.5 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Baizhangyan 7.9 5 4.8 10.9 Skarn W-Mo granite 0 0 0 136.3 (Zhong et al., 2017) various various Balışeyh 4.21 1 Granite Mo quartz monzonite, granitoid 0 0 0 73.6 (Delibaş and Genç, 2012) hand samples NTIMS Balzapamba 580.1 5 1 Porphyry Cu granodiorite; quartz diorite 0 0 0 27 (Schütte et al., 2012) concentrate, unknown method NTIMS Bamford 6.3 1 Breccia pipe W-Mo-Bi granite 0 0 0 0 (Riley, 1967) hand samples TIMS Banchang 12.2 1 Skarn Cu granite 0.66 0 0 145.55 (Mao et al., 2008) hand samples ICP-MS Banchang 25.87 1 Skarn Cu granite 0.66 0 0 145.55 (Mao et al., 2008) hand samples ICP-MS Banchang 25.9 1 Skarn Cu granite 0.66 0 0 145.55 (Mao et al., 2008) hand samples ICP-MS Banchang 33.31 1 Skarn Cu granite 0.66 0 0 145.55 (Mao et al., 2008) hand samples ICP-MS Banchang 80.35 1 Skarn Cu granite 0.66 0 0 145.55 (Mao et al., 2008) hand samples ICP-MS Banchang 106.08 1 Skarn Cu granite 0.66 0 0 145.55 (Mao et al., 2008) hand samples ICP-MS Bancroft 566 1 Granite U 0 0 0 0 1060 (Golden et al., 2013) unknown unknown Bandkeli 1.2 1 Unknown 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Bangpu 166.8 2.3 1 Porphyry Cu-Mo 0 0 0 0 0 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Bangpu 189.8 2.7 1 Porphyry Cu-Mo 0 0 0 0 0 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Bangpu 196.2 2.9 1 Porphyry Cu-Mo 0 0 0 0 0 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Bangpu 243.2 3.4 1 Porphyry Cu-Mo 0 0 0 0 0 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Bangpu 250.5 2.8 1 Porphyry Cu-Mo 0 0 0 0 0 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Baogaocun 35.249 0.315 Porphyry Mo granite 0 0.09 0 103.9 (Xu et al., 2016) unknown unknown Baoshan 6.292 0.057 Skarn Cu quartz monzonite, granite 0 0 0 250.3 (Ren et al., 2017) hand-picked magnetic concentrate ICP-MS Baoshan 5.483 0.052 Skarn Cu quartz monzonite, granite 0 0 0 250.3 (Ren et al., 2017) hand-picked magnetic concentrate ICP-MS Baoshan 5.092 0.045 Skarn Cu quartz monzonite, granite 0 0 0 250.3 (Ren et al., 2017) hand-picked magnetic concentrate ICP-MS Baoshan 5.976 0.046 Skarn Cu quartz monzonite, granite 0 0 0 250.3 (Ren et al., 2017) hand-picked magnetic concentrate ICP-MS Baoshan 4.929 0.024 Skarn Cu quartz monzonite, granite 0 0 0 250.3 (Ren et al., 2017) hand-picked magnetic concentrate ICP-MS Başnayayla 108.86 1 Porphyry Cu granite 0 0 0 0 (Delibaş and Genç, 2012) hand samples NTIMS Başnayayla 148.53 1 Porphyry Cu granite 0 0 0 0 (Delibaş and Genç, 2012) hand samples NTIMS Baxiannao 0.6902 0.0065 1 Quartz vein-hosted W-Sn granite 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Baxiannao 2.279 0.019 1 Quartz vein-hosted W-Sn granite 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Baxiannao 2.338 0.019 1 Quartz vein-hosted W-Sn granite 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Baxiannao 2.472 0.019 1 Quartz vein-hosted W-Sn granite 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Baxiannao 2.608 0.02 1 Quartz vein-hosted W-Sn granite 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS BC Moly (Lime Creek) 69 1 Porphyry Mo quartz monzonite 0 0 0 44.85 (Schindler, 1975) various NAA BC Moly (Lime Creek) 77.8 1 Porphyry Mo quartz monzonite 0 0 0 44.85 (Schindler, 1975) various NAA Bega 0.26 1 Quartz vein-hosted Bi 0 0 0 0 0 (Riley, 1967) hand samples TIMS Beikengchang 3.3 6 1 7.1 Skarn Mo granite 0 0.06 0 141.7 (Zhong et al., 2017) various various Bell Mount 3.2 1 Unknown 0 0 0 0 0 (Riley, 1967) hand samples TIMS Berg 67 1 Porphyry Cu-Mo latite; quartz diorite; quartz monzonite 0.39 0.03 0.05 48.25 (Sinclair et al., 2009) various NAA Berg 215 1 Porphyry Cu-Mo latite; quartz diorite; quartz monzonite 0.39 0.03 0.05 48.25 (Sinclair et al., 2009) various NAA Berg 152 1 Porphyry Cu-Mo latite; quartz diorite; quartz monzonite 0.39 0.03 0.05 48.25 (Sinclair et al., 2009) various NAA Bergaul 35.9 1 Porphyry Cu-Mo 0 0 0 0 0 (Lavrov and Kuleshevich, 2010) unknown SEM Bethlehem 190 1 Porphyry Cu-Mo dacite; granodiorite; quartz diorite 0.45 0.016 0.005 200 (Terada et al., 1971) hand-picked grains NAA Bethlehem 335 1 Porphyry Cu-Mo dacite; granodiorite; quartz diorite 0.45 0.016 0.005 200 (Schindler, 1975) various NAA Bethlehem 340 1 Porphyry Cu-Mo dacite; granodiorite; quartz diorite 0.45 0.016 0.005 200 (Schindler, 1975) various NAA Bethlehem 430 1 Porphyry Cu-Mo dacite; granodiorite; quartz diorite 0.45 0.016 0.005 200 (Schindler, 1975) various NAA Bethlehem 490 1 Porphyry Cu-Mo dacite; granodiorite; quartz diorite 0.45 0.016 0.005 200 (Terada et al., 1971) hand-picked grains NAA Bethlehem 980 1 Porphyry Cu-Mo dacite; granodiorite; quartz diorite 0.45 0.016 0.005 200 (Terada et al., 1971) hand-picked grains NAA Bethlehem 1153 1 Porphyry Cu-Mo dacite; granodiorite; quartz diorite 0.45 0.016 0.005 200 (Schindler, 1975) various NAA Bethlehem 1171 1 Porphyry Cu-Mo dacite; granodiorite; quartz diorite 0.45 0.016 0.005 200 (Schindler, 1975) various NAA Bethlehem—Huestis 417 1 Porphyry Cu-Mo dacite; granodiorite; quartz diorite 0.45 0.016 0.005 200 (Sinclair et al., 2009) various NAA Bethlehem—Iona 1015 1 Porphyry Cu-Mo dacite; granodiorite; quartz diorite 0.45 0.016 0.005 200 (Sinclair et al., 2009) various NAA Bethlehem—JA 200 1 Porphyry Cu-Mo aplite; granodiorite; quartz diorite; quartz monzonite 0.46 0.016 0.005 203 (Schindler, 1975) various NAA Bethlehem—JA 200 1 Porphyry Cu-Mo aplite; granodiorite; quartz diorite; quartz monzonite 0.46 0.016 0.005 203 (Sinclair et al., 2009) various NAA Bethlehem—JA 221 1 Porphyry Cu-Mo aplite; granodiorite; quartz diorite; quartz monzonite 0.46 0.016 0.005 203 (Schindler, 1975) various NAA Bethlehem—JA 222 1 Porphyry Cu-Mo aplite; granodiorite; quartz diorite; quartz monzonite 0.46 0.016 0.005 203 (Schindler, 1975) various NAA Bethlehem—JA 222 1 Porphyry Cu-Mo aplite; granodiorite; quartz diorite; quartz monzonite 0.46 0.016 0.005 203 (Sinclair et al., 2009) various NAA Bethlehem—JA 246 1 Porphyry Cu-Mo aplite; granodiorite; quartz diorite; quartz monzonite 0.46 0.016 0.005 203 (Schindler, 1975) various NAA Bethlehem—JA 246 1 Porphyry Cu-Mo aplite; granodiorite; quartz diorite; quartz monzonite 0.46 0.016 0.005 203 (Sinclair et al., 2009) various NAA Big Bell 2.7 1 Intrusion-related Au 0 0 0 5.1 0 (Riley, 1967) hand samples TIMS Biggenden 355 1 Skarn Au granite; diorite 0 0 0 330 (Riley, 1967) hand samples TIMS Biggenden 630 1 Skarn Au granite; diorite 0 0 0 330 (Luck and Allègre, 1982) unknown ID-ion probe Bingham 7.5 1 Porphyry Cu monzonite; quartz monzonite; latite 0.882 0.044 0.497 37 (Hiskey and Meloche, 1940) hand samples colorimetry Bingham 31 1 Porphyry Cu monzonite; quartz monzonite; latite 0.882 0.044 0.497 37 (Fleischer, 1959) flotation concentrate unknown Bingham 31 1 Porphyry Cu monzonite; quartz monzonite; latite 0.882 0.044 0.497 37 (Hiskey and Meloche, 1940) hand samples colorimetry Bingham 44 1 Porphyry Cu monzonite; quartz monzonite; latite 0.882 0.044 0.497 37 (Fleischer, 1959) flotation concentrate unknown Bingham 44 1 Porphyry Cu monzonite; quartz monzonite; latite 0.882 0.044 0.497 37 (Hiskey and Meloche, 1940) hand samples colorimetry Bingham 379.6 1 Porphyry Cu monzonite; quartz monzonite; latite 0.882 0.044 0.497 37 (McCandless and Ruiz, 1993) unknown unknown Bingham 400 300 1 Porphyry Cu monzonite; quartz monzonite; latite 0.882 0.044 0.497 37 (McCandless et al., 1993) hand-picked grains EPMA Bingham 400 300 1 Porphyry Cu monzonite; quartz monzonite; latite 0.882 0.044 0.497 37 (McCandless et al., 1993) hand-picked grains EPMA Bingham 700 500 1 Porphyry Cu monzonite; quartz monzonite; latite 0.882 0.044 0.497 37 (McCandless et al., 1993) hand-picked grains EPMA Bivongi 10 1 Granite Mo granite 0 0 0 0 (Paganelli, 1963) unknown colorimetry Blåfoddalen 10.9 1 Quartz vein-hosted Mo-W syenite 0 0 0 0 (Holwell et al., 2012) hand-picked magnetic/heavy liquids concentrate ID-NTIMS Blomskog 10.625 0.007 1 Pegmatite granite; pegmatite 0 0 0 915 (Bingen et al., 2006) NTIMS Blue Tier 0.96 1 Granite Sn 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Blue Tier 0.71 Granite Sn 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Blue Tier 0.38 Granite Sn 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Boddington 1.3 1 Porphyry Cu-Au monzogranite 0.0902 0 1.064 2655.5 (Golden et al., 2013) unknown unknown Boddington 3.8 1 Porphyry Cu-Au monzogranite 0.0902 0 1.064 2655.5 (Golden et al., 2013) unknown unknown Boddington 3.9 1 Porphyry Cu-Au monzogranite 0.0902 0 1.064 2655.5 (Golden et al., 2013) unknown unknown Boddington 11 1 Porphyry Cu-Au monzogranite 0.0902 0 1.064 2655.5 (Golden et al., 2013) unknown unknown Boddington 126 16 8.4 347 Porphyry Cu-Au monzogranite 0.0902 0 1.064 2655.5 (Ciobanu et al., 2013) hand samples LA-ICP-MS Boddington 328 1 Porphyry Cu-Au monzogranite 0.0902 0 1.064 2655.5 (Golden et al., 2013) unknown unknown Boddington 344 1 Porphyry Cu-Au monzogranite 0.0902 0 1.064 2655.5 (Golden et al., 2013) unknown unknown Boddington 350 15 150 713 Porphyry Cu-Au monzogranite 0.0902 0 1.064 2655.5 (Ciobanu et al., 2013) hand samples LA-ICP-MS Boddington 435 1 Porphyry Cu-Au monzogranite 0.0902 0 1.064 2655.5 (Golden et al., 2013) unknown unknown Boddington 467 35 94 1181 Porphyry Cu-Au monzogranite 0.0902 0 1.064 2655.5 (Ciobanu et al., 2013) hand samples LA-ICP-MS Boddington 832 1 Porphyry Cu-Au monzogranite 0.0902 0 1.064 2655.5 (Golden et al., 2013) unknown unknown Bohutin 1.2 Granodiorite Mo tonalite, granodiorite, granitoid 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Bohutin 2 Granodiorite Mo tonalite, granodiorite, granitoid 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Bohutin 24 Granodiorite Mo tonalite, granodiorite, granitoid 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Bohutin 38 Granodiorite Mo tonalite, granodiorite, granitoid 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Bondar-e-Hanza 527 6 1 Porphyry Cu-Mo diorite; granodiorite 0.3 0.008 0 28.38 (Aghazadeh et al., 2015) hand-picked grains unknown Bondar-e-Hanza 690 6 1 Porphyry Cu-Mo diorite; granodiorite 0.3 0.008 0 28.38 (Aghazadeh et al., 2015) hand-picked grains unknown Bor 846 1 1 Porphyry Cu 0 0.64 0.002 0.24 86.14 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Bor 930 2 1 Porphyry Cu 0 0.64 0.002 0.24 86.14 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Bor 1520 3 Porphyry Cu 0 0.64 0.002 0.24 86.14 (Berzina et al., 2005) various various Bora Creek 8.7 1 Granite Mo quartz monzonite 0 0 0 0 (Riley, 1967) hand samples TIMS Borly 2712 50 1 Porphyry Cu granite; granodiorite; quartz diorite 0.34 0.011 0.3 315.85 (Chen et al., 2010) hand samples ICP-MS Borly 2772 40 1 Porphyry Cu granite; granodiorite; quartz diorite 0.34 0.011 0.3 315.85 (Chen et al., 2010) hand samples ICP-MS Borly 3160 19 250 5500 Porphyry Cu granite; granodiorite; quartz diorite 0.34 0.011 0.3 315.85 (Berzina et al., 2005) various various Borów 11 1 Granite Mo granite 0 0 0 299 (Mikulski and Stein, 2007) micro-drilled hand samples NTIMS Borów 12 1 Granite Mo granite 0 0 0 299 (Mikulski and Stein, 2007) micro-drilled hand samples NTIMS Boshchekul 825 23 230 1500 Porphyry Cu-Au andesite; breccia; diabase; diorite; gabbro; granodiorite; rhyolite; syenite; tonalite; latite 0.66 0.01 0.27 481 (Berzina et al., 2005) various various Boss Mountain 49 1 Porphyry Mo monzogranite 0 0.13 0 104 (Sinclair et al., 2009) various NAA Boss Mountain 54 1 Porphyry Mo monzogranite 0 0.13 0 104 (Schindler, 1975) various NAA Boss Mountain 61 1 Porphyry Mo monzogranite 0 0.13 0 104 (Schindler, 1975) various NAA Boss Mountain 80 5 Porphyry Mo monzogranite 0 0.13 0 104 (Sinclair et al., 2009) various NAA Boss Mountain 157 1 Porphyry Mo monzogranite 0 0.13 0 104 (Sinclair et al., 2009) various NAA Boy Scout 64 1 Pegmatite 0 0 0.4 0 0 (Giles and Schilling, 1972) hand samples colorimetry Brejui 45.65 0.98 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brejui 52.02 0.38 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brejui 75.01 0.48 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brejui 75.08 0.48 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brejui 80.46 0.78 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brejui 81.31 0.48 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brejui 89.17 0.48 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brejui 90.98 0.59 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brejui 98.61 0.28 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brejui 105 0.52 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brejui 106.09 0.24 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brejui 110.74 0.19 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brejui 117.26 0.41 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brejui 128.17 0.8 1 Skarn W granite 0 0 0 494.65 (Suzuki et al., 2000) unknown ID-ICP-MS Brenda 63.4 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.161 0.032 0.013 194.5 (Schindler, 1975) various NAA Brenda 95 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.161 0.032 0.013 194.5 (Sinclair et al., 2009) various NAA Brenda 115 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.161 0.032 0.013 194.5 (Sinclair et al., 2009) various NAA Brenda 145 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.161 0.032 0.013 194.5 (Sinclair et al., 2009) various NAA Broken Hill 0.88 0.03 1 Sediment-hosted 0 0.1 0 0.1 0 (Suzuki et al., 2000) unknown ID-ICP-MS Broken Hill 1.52 0.03 1 Sediment-hosted 0 0.1 0 0.1 0 (Suzuki et al., 2000) unknown ID-ICP-MS Bronson Slope 180 1 Porphyry Cu-Au quartz diorite; quartz monzodiorite 0.15 0.013 0.72 195 (Sinclair et al., 2009) various NAA Brownstone 177 1 Skarn W 0 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Brownstone 327 1 Skarn W 0 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Brownstone 382 1 Skarn W 0 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Brownstone 389 1 Skarn W 0 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Brownstone 428 1 Skarn W 0 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Bugdaya 8 70 0.5 51 Porphyry Mo 0 0 0.073 0 153.35 (Berzina et al., 2005) various various Busshoji 25 1 Quartz vein-hosted Mo granitoid 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Busshoji 35 1 Quartz vein-hosted Mo granitoid 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Cadia East 1057 1 1 Porphyry Au-Cu quartz monzonite 0.37 0 0.43 442 (Wilson et al., 2007) hand samples NTIMS Cadia Hill 170.5 0.2 1 Porphyry Au-Cu quartz monzonite 0.16 0 0.63 442 (Wilson et al., 2007) hand samples NTIMS Cadia Hill 203.5 0.2 1 Porphyry Au-Cu quartz monzonite 0.16 0 0.63 442 (Wilson et al., 2007) hand samples NTIMS Cadia Quarry 12.108 0.009 1 Porphyry Au-Cu quartz monzonite 0.4 0 0.21 455 (Wilson et al., 2007) hand samples NTIMS Cadia Quarry 12.708 0.003 1 Porphyry Au-Cu quartz monzonite 0.4 0 0.21 455 (Wilson et al., 2007) hand samples NTIMS Cadia Quarry 25.07 0.02 1 Porphyry Au-Cu quartz monzonite 0.4 0 0.21 455 (Wilson et al., 2007) hand samples NTIMS Cadia Quarry 25.44 0.06 1 Porphyry Au-Cu quartz monzonite 0.4 0 0.21 455 (Wilson et al., 2007) hand samples NTIMS Cadia Quarry 861 1 1 Porphyry Au-Cu quartz monzonite 0.4 0 0.21 455 (Wilson et al., 2007) hand samples NTIMS Callie Soak 2.31 1 Unknown Mo 0 0 0 0 0 (Riley, 1967) hand samples TIMS Calova 111.3 0.1 1 Porphyry Cu 0 0 0 0 72.2 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Cananea 90.7 0.1 1 Porphyry Cu granitoid; porphyry 0.42 0.008 0.012 59.25 (Barra et al., 2005) hand-picked grains NTIMS Cananea 95.7 0.1 1 Porphyry Cu granitoid; porphyry 0.42 0.008 0.012 59.25 (Barra et al., 2005) hand-picked grains NTIMS Cananea 120 1 Porphyry Cu granitoid; porphyry 0.42 0.008 0.012 59.25 (Fleischer, 1959) flotation concentrate unknown Cananea 13 1 Porphyry Cu granitoid; porphyry 0.42 0.008 0.012 59.25 (Giles and Schilling, 1972) hand samples colorimetry Candelaria 73 1 IOCG Cu-Ag-Au (Pb-Fe) diorite; granodiorite; quartz monzonite 1.14 0 0.22 114.7 (Mathur et al., 2000) hand-picked grains NTIMS Candelaria 73.11 1 IOCG Cu-Ag-Au (Pb-Fe) diorite; granodiorite; quartz monzonite 1.14 0 0.22 114.7 (Mathur et al., 2002) hand-picked grains NTIMS Candelaria 77 1 IOCG Cu-Ag-Au (Pb-Fe) diorite; granodiorite; quartz monzonite 1.14 0 0.22 114.7 (Mathur et al., 2000) hand-picked grains NTIMS Candelaria 77.21 1 IOCG Cu-Ag-Au (Pb-Fe) diorite; granodiorite; quartz monzonite 1.14 0 0.22 114.7 (Mathur et al., 2002) hand-picked grains NTIMS Cangrejos 1019 8 1 Porphyry Au-Cu diorite; quartz diorite 0 0 0 0 (Schütte et al., 2012) concentrate, unknown method NTIMS Caosiyao 8.501 1 Porphyry Mo granite 0.078 148 (Wu et al., 2017) concentrate, unknown method ICP-MS Caosiyao 14.37 1 Porphyry Mo granite 0.078 148 (Wu et al., 2017) concentrate, unknown method ICP-MS Caosiyao 8.591 1 Porphyry Mo granite 0.078 148 (Wu et al., 2017) concentrate, unknown method ICP-MS Caosiyao 1.296 1 Porphyry Mo granite 0.078 148 (Wu et al., 2017) concentrate, unknown method ICP-MS Caosiyao 4.432 1 Porphyry Mo granite 0.078 148 (Wu et al., 2017) concentrate, unknown method ICP-MS Caosiyao 4.926 1 Porphyry Mo granite 0.078 148 (Wu et al., 2017) concentrate, unknown method ICP-MS Caosiyao 9.353 1 Porphyry Mo granite 0.078 150 (G. Wang et al., 2017) hand samples ICP-MS Caosiyao 9.065 1 Porphyry Mo granite 0.078 150 (G. Wang et al., 2017) hand samples ICP-MS Caosiyao 9.655 1 Porphyry Mo granite 0.078 150 (G. Wang et al., 2017) hand samples ICP-MS Caosiyao 11.09 1 Porphyry Mo granite 0.078 150 (G. Wang et al., 2017) hand samples ICP-MS Caosiyao 13.72 1 Porphyry Mo granite 0.078 150 (G. Wang et al., 2017) hand samples ICP-MS Carmi 10 1 Porphyry Mo quartz monzonite 0 0.064 0 62 (Sinclair et al., 2009) various NAA Carmi 58 1 Porphyry Mo quartz monzonite 0 0.064 0 62 (Sinclair et al., 2009) various NAA Carmi 139 1 Porphyry Mo quartz monzonite 0 0.064 0 62 (Sinclair et al., 2009) various NAA Carpenters Gully 94 1 Granite Mo-W 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Cash 53.56 0.43 1 Porphyry Cu-Mo granodiorite; intrusive igneous rock; quartz monzonite 0.28 0.021 0.17 76.41 (Selby and Creaser, 2001a) hand-picked magnetic/heavy liquids concentrate NTIMS Cash 128.6 2.7 1 Porphyry Cu-Mo granodiorite; intrusive igneous rock; quartz monzonite 0.28 0.021 0.17 76.41 (Selby and Creaser, 2001a) hand-picked magnetic/heavy liquids concentrate NTIMS Cash 54 1 Porphyry Cu-Mo granodiorite; intrusive igneous rock; quartz monzonite 0.28 0.021 0.17 76.41 (Sinclair et al., 2009) various NAA Cash 129 1 Porphyry Cu-Mo granodiorite; intrusive igneous rock; quartz monzonite 0.28 0.021 0.17 76.41 (Sinclair et al., 2009) various NAA Casino 65.49 1.06 1 Porphyry Cu-Mo granitoid; granodiorite; latite; quartz monzonite 0.25 0.035 0.3 74.715 (Selby and Creaser, 2001a) hand-picked magnetic/heavy liquids concentrate NTIMS Casino 185.5 1.7 1 Porphyry Cu-Mo granitoid; granodiorite; latite; quartz monzonite 0.25 0.035 0.3 74.715 (Selby and Creaser, 2001a) hand-picked magnetic/heavy liquids concentrate NTIMS Casino 246.3 3.2 1 Porphyry Cu-Mo granitoid; granodiorite; latite; quartz monzonite 0.25 0.035 0.3 74.715 (Selby and Creaser, 2001a) hand-picked magnetic/heavy liquids concentrate NTIMS Casino 289.2 2.2 1 Porphyry Cu-Mo granitoid; granodiorite; latite; quartz monzonite 0.25 0.035 0.3 74.715 (Selby and Creaser, 2001a) hand-picked magnetic/heavy liquids concentrate NTIMS Casino 65 1 Porphyry Cu-Mo granitoid; granodiorite; latite; quartz monzonite 0.25 0.035 0.3 74.715 (Sinclair et al., 2009) various NAA Casino 289 1 Porphyry Cu-Mo granitoid; granodiorite; latite; quartz monzonite 0.25 0.035 0.3 74.715 (Sinclair et al., 2009) various NAA Casino 197 2 Porphyry Cu-Mo granitoid; granodiorite; latite; quartz monzonite 0.25 0.035 0.3 74.715 (Sinclair et al., 2009) various NAA Cassiar Moly 3 1 Porphyry Mo quartz monzonite 0 0.026 0 82.55 (Sinclair et al., 2009) various NAA Cassiar Moly 14 1 Porphyry Mo quartz monzonite 0 0.026 0 82.55 (Sinclair et al., 2009) various NAA Catface 59 1 Porphyry Cu granodiorite; quartz diorite 0.37 0.007 0.05 48.75 (Sinclair et al., 2009) various NAA Celina 17 Intrusion-related Au granodiorite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Celina 31 Intrusion-related Au granodiorite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Celina 28 Intrusion-related Au granodiorite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Celina 113 Intrusion-related Au granodiorite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Cerbia 97.7 0.07 1 Granite Mo 0 0 0 0 159.1 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Cerna Hora 145.1 0.400 1 Quartz vein-hosted 0 0 0 0 589.5 (Ackerman et al., 2017) hand-picked grains ICP-MS Cerna Hora 30 Quartz vein-hosted 0 0 0 0 589.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Cerna Hora 49 Quartz vein-hosted 0 0 0 0 589.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Cerna Hora 47 Quartz vein-hosted 0 0 0 0 589.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Cerna Hora 14 Quartz vein-hosted 0 0 0 0 589.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Cerna Hora 15 Quartz vein-hosted 0 0 0 0 589.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Cerna Hora 15 Quartz vein-hosted 0 0 0 0 589.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Cerna Voda 33.64 0.080 1 Granite Mo granodiorite 0 0 0 296 (Ackerman et al., 2017) hand-picked grains ICP-MS Cerna Voda 31.38 0.070 1 Granite Mo granodiorite 0 0 0 296 (Ackerman et al., 2017) hand-picked grains ICP-MS Cerna Voda 16 Granite Mo granodiorite 0 0 0 296 (Pasava et al., 2016) polished mounts LA-ICP-MS Cerna Voda 4.3 Granite Mo granodiorite 0 0 0 296 (Pasava et al., 2016) polished mounts LA-ICP-MS Cerna Voda 16 Granite Mo granodiorite 0 0 0 296 (Pasava et al., 2016) polished mounts LA-ICP-MS Cerna Voda 11 Granite Mo granodiorite 0 0 0 296 (Pasava et al., 2016) polished mounts LA-ICP-MS Cerna Voda 5.4 Granite Mo granodiorite 0 0 0 296 (Pasava et al., 2016) polished mounts LA-ICP-MS Cerna Voda 12 Granite Mo granodiorite 0 0 0 296 (Pasava et al., 2016) polished mounts LA-ICP-MS Cerro Verde 3060 1 Porphyry Cu dacite; andesite 0.67 0.01 0 59.25 (Mathur et al., 2000) hand-picked grains NTIMS Cerro Verde 3280 2 3060 3497 Porphyry Cu dacite; andesite 0.67 0.01 0 59.25 (Berzina et al., 2005) various various Cerro Verde 3497 1 Porphyry Cu dacite; andesite 0.67 0.01 0 59.25 (Mathur et al., 2000) hand-picked grains NTIMS Chagele 3.37 Porphyry Mo granite 0 0 0 61.5 (Wang et al., 2016) hand samples MC-ICP-MS Chagele 5.21 Porphyry Mo granite 0 0 0 61.5 (Wang et al., 2016) hand samples MC-ICP-MS Chah Firouzeh 3273 40 1 Porphyry Cu monzodiorite; quartz diorite 0.35 0 0 16.19 (Aghazadeh et al., 2015) hand-picked grains unknown Chalice 75 1 Orogenic Au mozogranite 0 0 0 2631 (Bucci et al., 2004) hand-picked grains NTIMS Chambishi SE 730.5 2.1 730.5 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Chang'anchong 7.139 0.054 1 Porphyry Cu-Mo 0 0 0 0 34.35 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Chang'anchong 7.455 0.064 1 Porphyry Cu-Mo 0 0 0 0 34.35 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Chang'anchong 36.15 0.32 1 Porphyry Cu-Mo 0 0 0 0 34.35 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Chang'anchong 41.44 0.5 1 Porphyry Cu-Mo 0 0 0 0 34.35 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Chang'anchong 105.1 0.9 1 Porphyry Cu-Mo 0 0 0 0 34.35 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Chang'anchong 126.3 1.8 1 Porphyry Cu-Mo 0 0 0 0 34.35 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Chang'anchong 374.8 2.9 1 Porphyry Cu-Mo 0 0 0 0 34.35 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Chaucha 70.44 6 1 Porphyry Cu granodiorite 0.4 0.03 0 11 (Schütte et al., 2012) concentrate, unknown method NTIMS Chaucha 354.6 3 1 Porphyry Cu granodiorite 0.4 0.03 0 11 (Schütte et al., 2012) concentrate, unknown method NTIMS Chengmenshan 10.34 0.21 1 Porphyry Cu andesite; granitoid; granodiorite; monzogranite; quartz monzonite; tonalite 0.76 0.047 0.25 142.5 (Mao et al., 1999) various various Chengmenshan 10.76 0.09 1 Porphyry Cu andesite; granitoid; granodiorite; monzogranite; quartz monzonite; tonalite 0.76 0.047 0.25 142.5 (Mao et al., 1999) various various Chengmenshan 13.17 0.29 1 Porphyry Cu andesite; granitoid; granodiorite; monzogranite; quartz monzonite; tonalite 0.76 0.047 0.25 142.5 (Mao et al., 1999) various various Chengmenshan 14.87 0.16 1 Porphyry Cu andesite; granitoid; granodiorite; monzogranite; quartz monzonite; tonalite 0.76 0.047 0.25 142.5 (Mao et al., 1999) various various Chengmenshan 284.4 3 1 Porphyry Cu andesite; granitoid; granodiorite; monzogranite; quartz monzonite; tonalite 0.76 0.047 0.25 142.5 (Mao et al., 2006) hand samples ICP-MS Chibuluma South 83.2 0.2 51.9239092 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Chibuluma South 40.8 0.1 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Chibuluma South 41.24 0.11 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Chilu 10.1 5 4.3 16.2 Porphyry Mo granite 0 0.01 0 105.9 (Zhong et al., 2017) various various Chino 17.5 1 Porphyry Cu diorite 0.6203 0.008 0.056 58.6 (Fleischer, 1959) flotation concentrate unknown Christmas 2100 1300 1 Porphyry Cu andesite 1.1 0 0.01 63.5 (McCandless et al., 1993) hand-picked grains EPMA Chuquicamata 193 1 Porphyry Cu-Mo granodiorite; monzogranite; diorite 0.77 0.04 0.013 32.3 (Mathur et al., 2000) hand-picked grains NTIMS Chuquicamata 220 3 194 245 Porphyry Cu-Mo granodiorite; monzogranite; diorite 0.77 0.04 0.013 32.3 (Berzina et al., 2005) various various Chuquicamata 245 1 Porphyry Cu-Mo granodiorite; monzogranite; diorite 0.77 0.04 0.013 32.3 (Mathur et al., 2000) hand-picked grains NTIMS Ciclova 80.31 0.04 1 Quartz vein-hosted Mo 0 0 0 0 82.71 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Cinovec 0.169 0.001 1 Greisen Sn-W granite 0 0 0 323.5 (Ackerman et al., 2017) hand-picked grains ICP-MS Cinovec 0.17 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Cinovec 0.3 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Cinovec 0.18 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Cinovec 0.18 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Cinovec 0.29 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Cinovec 0.16 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Clark Lake 122.3 0.364 1 Porphyry Cu-Mo granodiorite; tonalite 1.33 0 0.37 2715.2 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS Clark Lake 116.1 0.901 1 Porphyry Cu-Mo granodiorite; tonalite 1.33 0 0.37 2715.2 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS Clark Lake 119.6 0.569 1 Porphyry Cu-Mo granodiorite; tonalite 1.33 0 0.37 2715.2 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS Clark Lake 121.8 0.464 1 Porphyry Cu-Mo granodiorite; tonalite 1.33 0 0.37 2715.2 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS Clark Lake 121.9 0.412 1 Porphyry Cu-Mo granodiorite; tonalite 1.33 0 0.37 2715.2 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS Clear Creek—Pukelman Zone 142 0.5 1 Intrusion-related Au monzogranite 0 0 0.21 95.7 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Clear Creek—Pukelman Zone 142.2 0.4 1 Intrusion-related Au monzogranite 0 0 0.21 95.7 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Clear Creek—Pukelman Zone 149 0.5 1 Intrusion-related Au monzogranite 0 0 0.21 95.7 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Clear Creek—Pukelman Zone 176.3 0.6 1 Intrusion-related Au monzogranite 0 0 0.21 95.7 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Clear Creek—Pukelman Zone 177.8 0.6 1 Intrusion-related Au monzogranite 0 0 0.21 95.7 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Clear Creek—Pukelman Zone 180.5 0.9 1 Intrusion-related Au monzogranite 0 0 0.21 95.7 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Clear Creek—Pukelman Zone 184.9 2.6 1 Intrusion-related Au monzogranite 0 0 0.21 95.7 (Selby et al., 2003) hand-picked grains NTIMS Clear Creek—Pukelman Zone 192.6 2.9 1 Intrusion-related Au monzogranite 0 0 0.21 95.7 (Selby et al., 2003) hand-picked grains NTIMS Clear Creek—Pukelman Zone 211.7 3 1 Intrusion-related Au monzogranite 0 0 0.21 95.7 (Selby et al., 2003) hand-picked grains NTIMS Clear Creek—Saddle Zone 419.8 4.4 1 Intrusion-related Au monzogranite 0 0 0 95.7 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Clear Creek—Saddle Zone 434.5 2.7 1 Intrusion-related Au monzogranite 0 0 0 95.7 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Cleo 35.56 0.02 1 Quartz vein-hosted Au 0 0 0 0 0 (Brown et al., 2002) hand-picked magnetic/heavy liquids concentrate NTIMS Climax 1.2 1 Porphyry Mo granite 0 0.24 0 26.6 (Fleischer, 1959) hand-picked magnetic/heavy liquids concentrate unknown Climax 1.2 1 Porphyry Mo granite 0 0.24 0 26.6 (Hiskey and Meloche, 1940) hand-picked magnetic/heavy liquids concentrate colorimetry Climax 5 1 Porphyry Mo granite 0 0.24 0 26.6 (Fleischer, 1959) hand-picked magnetic/heavy liquids concentrate unknown Climax 5 1 Porphyry Mo granite 0 0.24 0 26.6 (Hiskey and Meloche, 1940) Mo powder colorimetry Climax 6.97 0.03 1 Porphyry Mo granite 0 0.24 0 26.6 (Suzuki et al., 1993) hand samples ID-ICP-MS Climax 7 1 Porphyry Mo granite 0 0.24 0 26.6 (Suzuki et al., 1993) hand samples ID-ICP-MS Climax 8.7 1 Porphyry Mo granite 0 0.24 0 26.6 (Terada et al., 1971) hand-picked grains NAA Climax 20 1 Porphyry Mo granite 0 0.24 0 26.6 (Fleischer, 1959) flotation concentrate unknown Climax 28 1 Porphyry Mo granite 0 0.24 0 26.6 (Fleischer, 1959) flotation concentrate unknown Climax 74 1 Porphyry Mo granite 0 0.24 0 26.6 (Luck and Allègre, 1982) unknown ID-ion probe Climax 133 1 Porphyry Mo granite 0 0.24 0 26.6 (Golden et al., 2013) unknown unknown Collahuasi 367 1 Porphyry Cu dacite; granitoid; granodiorite; porphyry; quartz monzonite 0.79 0.04 0.01 37.1 (Masterman et al., 2004) hand-picked grains NTIMS Collahuasi 410 2 368 448 Porphyry Cu dacite; granitoid; granodiorite; porphyry; quartz monzonite 0.79 0.04 0.01 37.1 (Berzina et al., 2005) various various Collahuasi 447 1 Porphyry Cu dacite; granitoid; granodiorite; porphyry; quartz monzonite 0.79 0.04 0.01 37.1 (Mathur et al., 2000) hand-picked grains NTIMS Collahuasi 447 1 Porphyry Cu dacite; granitoid; granodiorite; porphyry; quartz monzonite 0.79 0.04 0.01 37.1 (Mathur et al., 2010) hand-picked grains NTIMS Collahuasi 633 1 Porphyry Cu dacite; granitoid; granodiorite; porphyry; quartz monzonite 0.79 0.04 0.01 37.1 (Mathur et al., 2010) hand-picked grains NTIMS Collahuasi 748 1 Porphyry Cu dacite; granitoid; granodiorite; porphyry; quartz monzonite 0.79 0.04 0.01 37.1 (Mathur et al., 2010) hand-picked grains NTIMS Collahuasi 367 1 Porphyry Cu dacite; granitoid; granodiorite; porphyry; quartz monzonite 0.79 0.04 0.01 37.1 (Mathur et al., 2010) hand-picked grains NTIMS Copaquirre 81 1 Porphyry Cu-Mo dacite; quartz monzonite 0.3 0.07 0 35 (Mathur et al., 2000) hand-picked grains NTIMS Copaquirre 84 2 81 86 Porphyry Cu-Mo dacite; quartz monzonite 0.3 0.07 0 35 (Berzina et al., 2005) various various Copaquirre 85 1 Porphyry Cu-Mo dacite; quartz monzonite 0.3 0.07 0 35 (Mathur et al., 2000) hand-picked grains NTIMS Copper Creek 20 1 Porphyry Cu dacite 0.75 0.005 4E-04 60.7 (Fleischer, 1959) flotation concentrate unknown Copper Creek 27.5 1 Porphyry Cu dacite 0.75 0.005 4E-04 60.7 (Fleischer, 1959) flotation concentrate unknown Copper Creek 27.5 1 Porphyry Cu dacite 0.75 0.005 4E-04 60.7 (Hiskey and Meloche, 1940) unknown colorimetry Copper Creek 40 1 Porphyry Cu dacite 0.75 0.005 4E-04 60.7 (Fleischer, 1959) flotation concentrate unknown Copper Creek 40 1 Porphyry Cu dacite 0.75 0.005 4E-04 60.7 (Hiskey and Meloche, 1940) unknown colorimetry Copper Creek 533.7 0.4 1 Porphyry Cu dacite 0.75 0.005 4E-04 60.7 (Barra et al., 2005) hand-picked grains NTIMS Copper Creek 856.3 1 Porphyry Cu dacite 0.75 0.005 4E-04 60.7 (McCandless and Ruiz, 1993) unknown unknown Copper Creek 1200 700 1 Porphyry Cu dacite 0.75 0.005 4E-04 60.7 (McCandless et al., 1993) hand-picked grains EPMA Copper Creek 1500 1500 1 Porphyry Cu dacite 0.75 0.005 4E-04 60.7 (McCandless et al., 1993) hand-picked grains EPMA Copper Creek 2107 1 Porphyry Cu dacite 0.75 0.005 4E-04 60.7 (McCandless and Ruiz, 1993) unknown unknown Copper Creek 4200 1800 1 Porphyry Cu dacite 0.75 0.005 4E-04 60.7 (McCandless et al., 1993) hand-picked grains EPMA Copper Creek 0 1 Porphyry Cu dacite 0.75 0.005 4E-04 60.7 (Hiskey and Meloche, 1940) unknown colorimetry Copper Hill 30 1 Breccia pipe 0 0.17 0 0.65 392.5 (Fleischer, 1959) flotation concentrate unknown Costelloe 3.16 0.01 1 Granite Mo granite 0 0 0 383.3 (Feely et al., 2010) magnetic concentrate NTIMS Costelloe 3.163 Granite Mo granite 383.3 (Selby et al., 2007) various various Cuajone 60 1 Porphyry Cu-Mo 0 0.69 0.021 0 52.4 (Berzina et al., 2005) various various Cuatro Hermanos 468.7 0.4 1 Porphyry Cu andesite; rhyolite 0.431 0.035 0 55.7 (Barra et al., 2005) hand-picked grains NTIMS Cumobabi 189 0.2 1 Porphyry Cu-Mo quartz monzonite; diorite; granite 0.266 0.099 0 58.7 (Barra et al., 2005) hand-picked grains NTIMS Cumobabi 368.2 0.3 1 Porphyry Cu-Mo quartz monzonite; diorite; granite 0.266 0.099 0 58.7 (Barra et al., 2005) hand-picked grains NTIMS Da'ao 0.02933 1 Greisen W-Mo 0 0 0 0 151.3 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Da'ao 1.17456 1 Greisen W-Mo 0 0 0 0 151.3 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Dabaoshan 64.8 Porphyry, skarn Mo granodiorite 0.39 0.02 0 163.9 (Zhong et al., 2017) various various Dabaoshan 64.7 Porphyry, skarn Mo granodiorite 0.39 0.02 0 163.9 (Zhong et al., 2017) various various Dabaoshan 102.4 Porphyry, skarn Mo granodiorite 0.39 0.02 0 163.9 (Zhong et al., 2017) various various Daheishan 17.28 0.13 1 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014b) unknown ICP-MS Daheishan 18.46 0.15 1 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014b) unknown ICP-MS Daheishan 19.04 0.14 1 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014b) unknown ICP-MS Daheishan 19.06 0.17 1 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014b) unknown ICP-MS Daheishan 20.8 0.15 1 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014b) unknown ICP-MS Daheishan 24.91 0.20 1 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014b) unknown ICP-MS Daheishan 29.89 0.24 1 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014b) unknown ICP-MS Daheishan 19.04 0.140 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014c) hand samples ICP-MS Daheishan 24.91 0.200 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014c) hand samples ICP-MS Daheishan 19.06 0.170 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014c) hand samples ICP-MS Daheishan 18.46 0.150 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014c) hand samples ICP-MS Daheishan 17.28 0.130 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014c) hand samples ICP-MS Daheishan 20.8 0.150 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014c) hand samples ICP-MS Daheishan 29.89 0.240 Porphyry Mo andesite; diorite; granodiorite 0 0.06 0 168 (Han et al., 2014c) hand samples ICP-MS Dahu 1.531 1 Quartz vein-hosted Au granite 0 0.24 6.8 227.95 (Mao et al., 2008) hand samples ICP-MS Dahu 1.868 1 Quartz vein-hosted Au granite 0 0.24 6.8 227.95 (Mao et al., 2008) hand samples ICP-MS Dahu 2.305 1 Quartz vein-hosted Au granite 0 0.24 6.8 227.95 (Mao et al., 2008) hand samples ICP-MS Dahutang 0.5495 0.0057 1 Granite W granodiorite 0 0 0 141.1 (Mao et al., 2013) hand-picked magnetic concentrate ICP-MS Dahutang 2.417 0.024 1 Granite W granodiorite 0 0 0 141.1 (Mao et al., 2013) hand-picked magnetic concentrate ICP-MS Dahutang 2.508 0.022 1 Granite W granodiorite 0 0 0 141.1 (Mao et al., 2013) hand-picked magnetic concentrate ICP-MS Dahutang 4.059 0.036 1 Granite W granodiorite 0 0 0 141.1 (Mao et al., 2013) hand-picked magnetic concentrate ICP-MS Dahutang 7.872 0.067 1 Granite W granodiorite 0 0 0 141.1 (Mao et al., 2013) hand-picked magnetic concentrate ICP-MS Daito 78 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito 98 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito 110.39 0.83 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Suzuki et al., 1996) hand samples ID-ICP-MS Daito 110.88 0.93 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Suzuki et al., 1996) hand samples ID-ICP-MS Daito 133.4 7 Quartz vein-hosted granodiorite 0 0 0 56.65 (Ishihara, 1988) various NAA/spectrophotometry Daito 130.9 9 Quartz vein-hosted granodiorite 0 0 0 56.65 (Ishihara, 1988) various NAA/spectrophotometry Daito—Daito 7 21 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Daito-hi 89 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Daito-hi 190 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Dogakidani 62 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Eiko-hi 32 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Eiko-hi 160 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Eiko-hi 238.2 6 Quartz vein-hosted granodiorite 0 0 0 56.65 (Ishihara, 1988) various NAA/spectrophotometry Daito—Hinotani 1 33 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Hinotani 1 130 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Hinotani 2 100 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Hinotani 3 280 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Hinotani 3 160 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Hinotani 4 50 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Hinotani 4 190 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Orisakadani 67 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Orisakadani 140 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Orisakadani 116 2 Quartz vein-hosted granodiorite 0 0 0 56.65 (Ishihara, 1988) various NAA/spectrophotometry Daito—Tsutsumioku 290 1 Quartz vein-hosted granodiorite 0 0 0 56.65 (Terada et al., 1971) hand-picked grains NAA Daito—Tsutsumioku 188 2 Quartz vein-hosted granodiorite 0 0 0 56.65 (Ishihara, 1988) various NAA/spectrophotometry Dal'nensk 2.2 1 Greisen Mo-Sn-W 0 0 0 0 0 (Fleischer, 1960) unknown colorimetry Dal’neye 650 1 Porphyry Cu 0 0.39 0.003 0.37 0 (Berzina et al., 2005) various various Dalen 350.6 0.2 1 Quartz vein-hosted Mo 0 0 0 0 1019 (Bingen et al., 2006) micro-drilled hand samples NTIMS Dar Alu 817 8 1 Porphyry Cu granodiorite 0.39 0.005 0 12.96 (Aghazadeh et al., 2015) hand-picked grains unknown Darreh Zar 944.4 8.6 1 Porphyry Cu-Mo diorite; granodiorite 0.36 0.005 0 15.66 (Aghazadeh et al., 2015) hand-picked grains unknown Dastakert 220 8 130 300 Porphyry Cu-Mo diabase; diorite; lamprophyre; pegmatite 0 0 0 22 (Berzina et al., 2005) various various Datuanshan 149.8 2.2 1 Skarn Cu granite 0 0 0 139.3 (Mao et al., 2006) hand samples ICP-MS Datuanshan 261 2.5 1 Skarn Cu granite 0 0 0 139.3 (Mao et al., 2006) hand samples ICP-MS Datuanshan 278.9 3.9 1 Skarn Cu granite 0 0 0 139.3 (Mao et al., 2006) hand samples ICP-MS Datuanshan 754 15 1 Skarn Cu granite 0 0 0 139.3 (Mao et al., 2006) hand samples ICP-MS Datuanshan 981.4 8.6 1 Skarn Cu granite 0 0 0 139.3 (Mao et al., 2006) hand samples ICP-MS Datuanshan 1000 8.5 1 Skarn Cu granite 0 0 0 139.3 (Mao et al., 2006) hand samples ICP-MS Davenda 73 13 47 105 Porphyry Mo 0 0 0.5 0 0 (Berzina et al., 2005) various various Dawan 17.14 0.32 1 Porphyry, skarn Mo rhyolite 0 0.12 0 148.1 (Mao et al., 1999) various various Dawangzhuang 12.72 1 Skarn Mo granite 0 0 0 144.5 (Mao et al., 2008) hand samples ICP-MS Dawangzhuang 18.07 1 Skarn Mo granite 0 0 0 144.5 (Mao et al., 2008) hand samples ICP-MS Dawangzhuang 18.35 1 Skarn Mo granite 0 0 0 144.5 (Mao et al., 2008) hand samples ICP-MS Dawangzhuang 19.44 1 Skarn Mo granite 0 0 0 144.5 (Mao et al., 2008) hand samples ICP-MS Dawangzhuang 19.45 1 Skarn Mo granite 0 0 0 144.5 (Mao et al., 2008) hand samples ICP-MS Dawangzhuang 49.73 1 Porphyry Mo granite 0 0 0 144.5 (Mao et al., 2008) hand samples ICP-MS Dayinjian 31.99 1 Porphyry Mo granite 0 0.1 0 122.1 (Mao et al., 2008) hand samples ICP-MS Dazhuangke 11.24 0.2 1 Breccia pipe Mo monzodiorite 0 0.08 0 149.215 (Mao et al., 1999) various various Dazhuangke 15.97 0.16 1 Breccia pipe Mo monzodiorite 0 0.08 0 149.215 (Mao et al., 1999) various various Dazhuangke 20.19 0.32 1 Breccia pipe Mo monzodiorite 0 0.08 0 149.215 (Mao et al., 1999) various various Deepwater 13.2 1 Pegmatite Bi 0 0 0 0 0 (Riley, 1967) hand samples TIMS Derflice 73.8 0.200 1 Granite Mo granodiorite 0 0 0 578 (Ackerman et al., 2017) hand-picked grains ICP-MS Derflice 92 Granite Mo granodiorite 0 0 0 578 (Pasava et al., 2016) polished mounts LA-ICP-MS Derflice 33 Granite Mo granodiorite 0 0 0 578 (Pasava et al., 2016) polished mounts LA-ICP-MS Derflice 21 Granite Mo granodiorite 0 0 0 578 (Pasava et al., 2016) polished mounts LA-ICP-MS Derflice 14 Granite Mo granodiorite 0 0 0 578 (Pasava et al., 2016) polished mounts LA-ICP-MS Derflice 19 Granite Mo granodiorite 0 0 0 578 (Pasava et al., 2016) polished mounts LA-ICP-MS Devgaon 35.4 0.02 1 Granitoid Mo granite 0 0 0 0 (Stein et al., 2006) unknown unknown Devgaon 40.38 0.02 1 Granitoid Mo granite 0 0 0 0 (Stein et al., 2006) unknown unknown Devgaon 50.54 0.03 1 Granitoid Mo granite 0 0 0 0 (Stein et al., 2006) unknown unknown Devgaon 68.43 0.06 1 Granitoid Mo granite 0 0 0 0 (Stein et al., 2006) unknown unknown Devgaon 107.87 0.05 1 Granitoid Mo granite 0 0 0 0 (Stein et al., 2006) unknown unknown Dexing 596.9 5 51.25 987.2 Porphyry Cu granodiorite 0.52 0.01 0 171.1 (Zhong et al., 2017) various various Dexing 217.8 5 113.2 410.1 Porphyry Cu granodiorite 0.52 0.01 0 171.1 (Zhong et al., 2017) various various Dexing 290.3 5 62.9 586.8 Porphyry Cu granodiorite 0.52 0.01 0 171.1 (Zhong et al., 2017) various various Dexing 591.4 1 Porphyry Cu granodiorite 0.52 0.01 171 (Zhou et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing 196.6 1 Porphyry Cu granodiorite 0.52 0.01 171 (Zhou et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing 384.7 1 Porphyry Cu granodiorite 0.52 0.01 171 (Zhou et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing 386.6 1 Porphyry Cu granodiorite 0.52 0.01 171 (Zhou et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing 172.3 1 Porphyry Cu granodiorite 0.52 0.01 171 (Zhou et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing 417.6 1 Porphyry Cu granodiorite 0.52 0.01 171 (Zhou et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing—Fujiawu 236.4 1 Porphyry Cu 0 0.46 0.016 0.12 170.4 (Guo et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing—Fujiawu 180.8 1 Porphyry Cu 0 0.46 0.016 0.12 170.4 (Guo et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing—Fujiawu 655.1 1 Porphyry Cu 0 0.46 0.016 0.12 170.4 (Guo et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing—Fujiawu 307.7 1 Porphyry Cu 0 0.46 0.016 0.12 170.4 (Guo et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing—Fujiawu 359.4 1 Porphyry Cu 0 0.46 0.016 0.12 170.4 (Guo et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing—Tongchang 1577 1 Porphyry Cu granodiorite 0.48 0 0 0 (Guo et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing—Tongchang 660 2 498 822 Porphyry Cu granodiorite 0.48 0 0 0 (Berzina et al., 2005) various various Dexing—Tongchang 1228 1 Porphyry Cu granodiorite 0.48 0 0 0 (Guo et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing—Tongchang 418.7 1 Porphyry Cu granodiorite 0.48 0 0 0 (Guo et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing—Tongchang 1462 1 Porphyry Cu granodiorite 0.48 0 0 0 (Guo et al., 2012) hand samples ICP-MS Dexing—Tongchang 81.9 1 Porphyry Cu granodiorite 0.48 0 0 0 (Guo et al., 2012) hand samples ICP-MS Dexing—Zhushahong 256.4 1 Porphyry Cu 0 0.46 0.016 0.12 170.4 (Guo et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing—Zhushahong 163.9 1 Porphyry Cu 0 0.46 0.016 0.12 170.4 (Guo et al., 2012) hand-picked magnetic concentrate ICP-MS Dexing—Zhushahong 100.5 1 Porphyry Cu 0 0.46 0.016 0.12 170.4 (Guo et al., 2012) hand samples ICP-MS Dexing—Zhushahong 937.4 1 Porphyry Cu 0 0.46 0.016 0.12 170.4 (Guo et al., 2012) hand samples ICP-MS Dexing—Zhushahong 221.4 1 Porphyry Cu 0 0.46 0.016 0.12 170.4 (Guo et al., 2012) hand samples ICP-MS Diamond Joe 200 100 1 Porphyry Cu 0 0 0 0 0 (McCandless et al., 1993) hand-picked grains EPMA Dimbulah 35 1 Unknown W-Mo 0 0 0 0 0 (Riley, 1967) hand samples TIMS Dimbulah 35.6 1 Unknown W-Mo 0 0 0 0 0 (Riley, 1967) hand samples TIMS Diyanqinamu 42.58 1 Porphyry Mo quartz monzonite, diorite, dacite 0.097 156.2 (C. Leng et al., 2015) hand-picked flotation concentrate ICP-MS Diyanqinamu 52.9 1 Porphyry Mo quartz monzonite, diorite, dacite 0.097 156.2 (C. Leng et al., 2015) hand-picked flotation concentrate ICP-MS Diyanqinamu 50.94 1 Porphyry Mo quartz monzonite, diorite, dacite 0.097 156.2 (C. Leng et al., 2015) hand-picked flotation concentrate ICP-MS Diyanqinamu 19.59 1 Porphyry Mo quartz monzonite, diorite, dacite 0.097 156.2 (C. Leng et al., 2015) hand-picked flotation concentrate ICP-MS Diyanqinamu 89.13 1 Porphyry Mo quartz monzonite, diorite, dacite 0.097 156.2 (C. Leng et al., 2015) hand-picked flotation concentrate ICP-MS Diyanqinamu 58.15 1 Porphyry Mo quartz monzonite, diorite, dacite 0.097 156.2 (C. Leng et al., 2015) hand-picked flotation concentrate ICP-MS Diyanqinamu 50.19 1 Porphyry Mo quartz monzonite, diorite, dacite 0.097 156.2 (C. Leng et al., 2015) hand-picked flotation concentrate ICP-MS Diyanqinamu 50.85 1 Porphyry Mo quartz monzonite, diorite, dacite 0.097 156.2 (C. Leng et al., 2015) hand-picked flotation concentrate ICP-MS Diyanqinamu 54.98 1 Porphyry Mo quartz monzonite, diorite, dacite 0.097 156.2 (C. Leng et al., 2015) hand-picked flotation concentrate ICP-MS Diyanqinamu 45.54 1 Porphyry Mo quartz monzonite, diorite, dacite 0.097 156.2 (C. Leng et al., 2015) hand-picked flotation concentrate ICP-MS Dognecea 1524 1 Skarn Fe 0 0 0 0 76.51 (Ciobanu et al., 2002) hand samples NTIMS Dolni Bory 74.6 0.200 1 Pegmatite 0 0 0 0 0 (Ackerman et al., 2017) hand-picked grains ICP-MS Dongbeigou 28.38 0.175 Porphyry Mo granodiorite, quartz monzonite 0 0 0 128.1 (Zhang et al., 2016) hand-picked magnetic concentrate ICP-MS Dongbeigou 9.42 0.071 Porphyry Mo granodiorite, quartz monzonite 0 0 0 128.1 (Zhang et al., 2016) hand-picked magnetic concentrate ICP-MS Dongbeigou 20.61 0.117 Porphyry Mo granodiorite, quartz monzonite 0 0 0 128.1 (Zhang et al., 2016) hand-picked magnetic concentrate ICP-MS Dongbeigou 5.10 0.036 Porphyry Mo granodiorite, quartz monzonite 0 0 0 128.1 (Zhang et al., 2016) hand-picked magnetic concentrate ICP-MS Dongbeigou 21.66 0.134 Porphyry Mo granodiorite, quartz monzonite 0 0 0 128.1 (Zhang et al., 2016) hand-picked magnetic concentrate ICP-MS Dongfengbeishan 0.944 1 Porphyry Mo quartz diorite, monzogranite 0.21 194 (Guo et al., 2018) hand-picked grains ICP-MS Dongfengbeishan 1.237 1 Porphyry Mo quartz diorite, monzogranite 0.21 194 (Guo et al., 2018) hand-picked grains ICP-MS Dongfengbeishan 0.399 1 Porphyry Mo quartz diorite, monzogranite 0.21 194 (Guo et al., 2018) hand-picked grains ICP-MS Dongfengbeishan 1.375 1 Porphyry Mo quartz diorite, monzogranite 0.21 194 (Guo et al., 2018) hand-picked grains ICP-MS Dongfengbeishan 0.222 1 Porphyry Mo quartz diorite, monzogranite 0.21 194 (Guo et al., 2018) hand-picked grains ICP-MS Donggebi 10.92 0.9 1 Porphyry Mo granite 0 0.115 0 234.65 (Han et al., 2014b) unknown ICP-MS Donggebi 33.12 0.27 1 Porphyry Mo granite 0 0.115 0 234.65 (Han et al., 2014b) unknown ICP-MS Donggebi 38.24 0.32 1 Porphyry Mo granite 0 0.115 0 234.65 (Han et al., 2014b) unknown ICP-MS Donggebi 41.03 0.34 1 Porphyry Mo granite 0 0.115 0 234.65 (Han et al., 2014b) unknown ICP-MS Donggebi 41.97 0.31 1 Porphyry Mo granite 0 0.115 0 234.65 (Han et al., 2014b) unknown ICP-MS Donggebi 56.39 0.45 1 Porphyry Mo granite 0 0.115 0 234.65 (Han et al., 2014a) unknown ICP-MS Donggebi 59.27 0.52 1 Porphyry Mo granite 0 0.115 0 234.65 (Han et al., 2014b) unknown ICP-MS Donggebi 63.18 0.56 1 Porphyry Mo granite 0 0.115 0 234.65 (Han et al., 2014a) unknown ICP-MS Donggebi 88.54 0.660 Porphyry Mo granite 0 0.115 0 234.65 (H. Sun et al., 2017) hand samples ICP-MS Donggebi 98.18 0.790 Porphyry Mo granite 0 0.115 0 234.65 (H. Sun et al., 2017) hand samples ICP-MS Donggebi 16.74 0.130 Porphyry Mo granite 0 0.115 0 234.65 (H. Sun et al., 2017) hand samples ICP-MS Donggebi 84.32 1.300 Porphyry Mo granite 0 0.115 0 234.65 (H. Sun et al., 2017) hand samples ICP-MS Donggebi 15.96 0.140 Porphyry Mo granite 0 0.115 0 234.65 (H. Sun et al., 2017) hand samples ICP-MS Donggebi 15.96 Porphyry Mo granite 0 0.115 0 234.65 (H. Sun et al., 2017) hand samples ICP-MS Donggebi 29.36 Porphyry Mo granite 0 0.115 0 234.65 (H. Sun et al., 2017) hand samples ICP-MS Donggebi 29.36 0.230 Porphyry Mo granite 0 0.115 0 234.65 (H. Sun et al., 2017) hand samples ICP-MS Donggebi 23.57 0.180 Porphyry Mo granite 0 0.115 0 234.65 (Zhang et al., 2015) hand-picked grains ICP-MS Donggebi 23.58 0.210 Porphyry Mo granite 0 0.115 0 234.65 (Zhang et al., 2015) hand-picked grains ICP-MS Donggebi 22.66 0.210 Porphyry Mo granite 0 0.115 0 234.65 (Zhang et al., 2015) hand-picked grains ICP-MS Donggebi 23.56 0.190 Porphyry Mo granite 0 0.115 0 234.65 (Zhang et al., 2015) hand-picked grains ICP-MS Donggebi 24.08 0.190 Porphyry Mo granite 0 0.115 0 234.65 (Zhang et al., 2015) hand-picked grains ICP-MS Donggebi 21.2 0.170 Porphyry Mo granite 0 0.115 0 234.65 (Zhang et al., 2015) hand-picked grains ICP-MS Donggou 4.1 1 Porphyry Mo granite 0 0.11 0 114.6 (Mao et al., 2008) hand samples ICP-MS Donggou 4.259 1 Porphyry Mo granite 0 0.11 0 114.6 (Mao et al., 2008) hand samples ICP-MS Drammen 7.5 1 Granite Mo granite 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Dublin Gulch 282.5 0.8 1 Intrusion-related Au granodiorite 0 0 0.916 94.2 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Dublin Gulch 284.7 0.9 1 Intrusion-related Au granodiorite 0 0 0.916 94.2 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Dublin Gulch 514.3 22.1 1 Intrusion-related Au granodiorite 0 0 0.916 94.2 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Dublin Gulch 695.8 72.2 1 Intrusion-related Au granodiorite 0 0 0.916 94.2 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Dumitri Potok 139.6 0.1 1 Porphyry Cu 0 0 0 0 80.805 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Dumitri Potok 202.3 0.2 1 Porphyry Cu 0 0 0 0 80.805 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Dumitri Potok 281.1 0.3 1 Porphyry Cu 0 0 0 0 80.805 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Duobaoshan 406.8 1 Porphyry Cu-Mo granodiorite 0.47 0.016 484 (Liu et al., 2012) unknown ICP-MS Duobaoshan 835.2 1 Porphyry Cu-Mo granodiorite 0.52 0.02 476 (Zeng et al., 2014) hand samples ICP-MS Duobaoshan 884.6 1 Porphyry Cu-Mo granodiorite 0.52 0.02 476 (Zeng et al., 2014) hand samples ICP-MS Duobaoshan 614 1 Porphyry Cu-Mo granodiorite 0.52 0.02 476 (Zeng et al., 2014) hand samples ICP-MS Duobaoshan 121.7 1 Porphyry Cu-Mo granodiorite 0.52 0.02 476 (Zeng et al., 2014) hand samples ICP-MS Duobaoshan 718.3 1 Porphyry Cu-Mo granodiorite 0.52 0.02 476 (Zeng et al., 2014) hand samples ICP-MS Duobaoshan 1159 1 Porphyry Cu-Mo granodiorite 0.52 0.02 476 (Zeng et al., 2014) hand samples ICP-MS Duobaoshan-Tongshan 303.2 1.5 1 Porphyry Cu-Mo andesite; granite; granodiorite; tuff 1.86 0 0.5 508.5 (Mao et al., 1999) various various Duobaoshan-Tongshan 497 6 1 Porphyry Cu-Mo andesite; granite; granodiorite; tuff 1.86 0 0.5 508.5 (Mao et al., 1999) various various Duobaoshan-Tongshan 537.9 25 1 Porphyry Cu-Mo andesite; granite; granodiorite; tuff 1.86 0 0.5 508.5 (Mao et al., 1999) various various Duobaoshan-Tongshan 567 19 1 Porphyry Cu-Mo andesite; granite; granodiorite; tuff 1.86 0 0.5 508.5 (Mao et al., 1999) various various Duobaoshan-Tongshan 822 21 1 Porphyry Cu-Mo andesite; granite; granodiorite; tuff 1.86 0 0.5 508.5 (Mao et al., 1999) various various Dzhindara 980 6 472 1650 Porphyry Cu 0 0 0 0 0 (Berzina et al., 2005) various various East Kounrad 25.92 0.21 1 Greisen 0 0.589 0.011 0.19 329.5 (Chen et al., 2010) hand samples ICP-MS East Kounrad 26.19 0.34 1 Greisen 0 0.589 0.011 0.19 329.5 (Chen et al., 2010) hand samples ICP-MS East Kounrad 27.3 0.26 1 Greisen 0 0.589 0.011 0.19 329.5 (Chen et al., 2010) hand samples ICP-MS East Kounrad 31.5 0.27 1 Greisen 0 0.589 0.011 0.19 329.5 (Chen et al., 2010) hand samples ICP-MS Eastern Artemov Massif 300 1 Porphyry Cu quartz diorite 0 0 0 0 (Grabezhev and Shagalov, 2010) hand samples EPMA Eastern Artemov Massif 300 1 Porphyry Cu quartz diorite 0 0 0 0 (Grabezhev and Shagalov, 2010) hand samples EPMA Eastern Artemov Massif 400 1 Porphyry Cu quartz diorite 0 0 0 0 (Grabezhev and Shagalov, 2010) hand samples EPMA Eastern Artemov Massif 500 1 Porphyry Cu quartz diorite 0 0 0 0 (Grabezhev and Shagalov, 2010) hand samples EPMA Eastern Artemov Massif 700 1 Porphyry Cu quartz diorite 0 0 0 0 (Grabezhev and Shagalov, 2010) hand samples EPMA Eastern Artemov Massif 700 1 Porphyry Cu quartz diorite 0 0 0 0 (Grabezhev and Shagalov, 2010) hand samples EPMA Eastern Artemov Massif 2200 1 Porphyry Cu quartz diorite 0 0 0 0 (Grabezhev and Shagalov, 2010) hand samples EPMA Eastern Artemov Massif 2300 1 Porphyry Cu quartz diorite 0 0 0 0 (Grabezhev and Shagalov, 2010) hand samples EPMA Eastern Artemov Massif 2800 1 Porphyry Cu quartz diorite 0 0 0 0 (Grabezhev and Shagalov, 2010) hand samples EPMA Eastern Artemov Massif 5000 1 Porphyry Cu quartz diorite 0 0 0 0 (Grabezhev and Shagalov, 2010) hand samples EPMA Eastern Artemov Massif 6300 1 Porphyry Cu quartz diorite 0 0 0 0 (Grabezhev and Shagalov, 2010) hand samples EPMA Ebisu 1.1 1 Quartz vein-hosted Mo-W granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Ebisu 2.3 1 Quartz vein-hosted Mo-W granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Ebisu 1.9 2 Quartz vein-hosted Mo-W granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry El Alacrán 7352 6 1 Porphyry Cu granitoid 0.35 0 0 60.85 (Barra et al., 2005) hand-picked grains NTIMS El Alacrán 10424 10 1 Porphyry Cu granitoid 0.35 0 0 60.85 (Barra et al., 2005) hand-picked grains NTIMS El Crestón 25.6 0.1 1 Porphyry Cu granite 0.06 0.074 0 53.6 (Barra et al., 2005) hand-picked grains NTIMS El Salvador 49.12 0.02 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 50.06 0.01 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 50.6 0.03 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 50.65 0.01 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 61.97 0.07 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 63.51 0.07 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 68.7 0.08 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 69.86 0.04 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 70.56 0.02 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 70.8 0.02 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 89.4 0.1 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 99.4 0.1 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 116 0.1 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 416.6 0.6 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Salvador 444.2 0.8 1 Porphyry Cu granodiorite 0.54 0 0 41.6333333 (Zimmerman et al., 2014) hand samples NTIMS El Teniente 46 1 Porphyry Cu andesite; basalt; dacite; gabbro; lamprophyre; latite; tonalite 0.92 0.019 0.005 5.01 (Mathur et al., 2010) hand-picked grains NTIMS El Teniente 115 1 Porphyry Cu andesite; basalt; dacite; gabbro; lamprophyre; latite; tonalite 0.92 0.019 0.005 5.01 (Mathur et al., 2010) hand-picked grains NTIMS El Teniente 115 1 Porphyry Cu andesite; basalt; dacite; gabbro; lamprophyre; latite; tonalite 0.92 0.019 0.005 5.01 (Mathur et al., 2010) hand-picked grains NTIMS El Teniente 160 1 Porphyry Cu andesite; basalt; dacite; gabbro; lamprophyre; latite; tonalite 0.92 0.019 0.005 5.01 (Mathur et al., 2010) hand-picked grains NTIMS El Teniente 254 1 Porphyry Cu andesite; basalt; dacite; gabbro; lamprophyre; latite; tonalite 0.92 0.019 0.005 5.01 (Mathur et al., 2010) hand-picked grains NTIMS El Teniente 390 6 182 1154 Porphyry Cu andesite; basalt; dacite; gabbro; lamprophyre; latite; tonalite 0.92 0.019 0.005 5.01 (Berzina et al., 2005) various various El Teniente 725 1 Porphyry Cu andesite; basalt; dacite; gabbro; lamprophyre; latite; tonalite 0.92 0.019 0.005 5.01 (Mathur et al., 2010) hand-picked grains NTIMS El Tierrero 2280.2 7 Skarn Au granodiorite; quartz diorite 0 0 15 146 (Chiaradia et al., 2009) hand samples NTIMS El Tierrero 2512.4 5 Skarn Au granodiorite; quartz diorite 0 0 15 146 (Chiaradia et al., 2009) hand samples NTIMS El Tierrero 2550 4 Skarn Au granodiorite; quartz diorite 0 0 15 146 (Chiaradia et al., 2009) hand samples NTIMS Elatsite 272.88 0.06 1 Porphyry Cu diorite; syenite 0.39 0 0.26 92.055 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Elatsite 1250 19 273 2740 Porphyry Cu diorite; syenite 0.39 0 0.26 92.055 (Berzina et al., 2005) various various Elatsite 1287.1 0.2 1 Porphyry Cu diorite; syenite 0.39 0 0.26 92.055 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Elatsite 1407.8 0.3 1 Porphyry Cu diorite; syenite 0.39 0 0.26 92.055 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Elatsite 1877.3 0.6 1 Porphyry Cu diorite; syenite 0.39 0 0.26 92.055 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Elatsite 2329.3 0.5 1 Porphyry Cu diorite; syenite 0.39 0 0.26 92.055 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Elatsite 2330 1 1 Porphyry Cu diorite; syenite 0.39 0 0.26 92.055 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Elatsite 2499 2 1 Porphyry Cu diorite; syenite 0.39 0 0.26 92.055 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Elatsite 2740.1 0.6 1 Porphyry Cu diorite; syenite 0.39 0 0.26 92.055 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Eleys 2.41 1 Unknown 0 0 0 0 0 (Riley, 1967) hand samples TIMS Elpin 4500 1 Porphyry Cu 0 0 0 0 0 (Berzina et al., 2005) various various Elsmore 67 1 Granite Sn 0 0 0 0 0 (Riley, 1967) hand samples TIMS Ely 1000 200 1 Porphyry Cu quartz monzonite; rhyolite 0.613 0.01 0.27 112.7 (McCandless et al., 1993) hand-picked grains EPMA Endako 6.5 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Selby and Creaser, 2001b) hand-picked magnetic/heavy liquids concentrate NTIMS Endako 9.8 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Selby and Creaser, 2001b) hand-picked magnetic/heavy liquids concentrate NTIMS Endako 11.2 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Selby and Creaser, 2001b) hand-picked magnetic/heavy liquids concentrate NTIMS Endako 15 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Sinclair et al., 2009) various NAA Endako 20 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Selby and Creaser, 2001b) hand-picked magnetic/heavy liquids concentrate NTIMS Endako 27.2 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Selby and Creaser, 2001b) hand-picked magnetic/heavy liquids concentrate NTIMS Endako 24 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Terada et al., 1971) hand-picked grains NAA Endako 27 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Terada et al., 1971) hand-picked grains NAA Endako 30.4 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Selby and Creaser, 2001b) hand-picked magnetic/heavy liquids concentrate NTIMS Endako 30.6 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Selby and Creaser, 2001b) hand-picked magnetic/heavy liquids concentrate NTIMS Endako 30.6 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Selby and Creaser, 2001b) hand-picked magnetic/heavy liquids concentrate NTIMS Endako 31.1 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Selby and Creaser, 2001b) hand-picked magnetic/heavy liquids concentrate NTIMS Endako 32 1 22 43 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Berzina et al., 2005) various various Endako 32 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Schindler, 1975) various NAA Endako 32.85 0.14 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Lawley and Selby, 2012) magnetic and heavy-liquid concentrate NTIMS Endako 35 10 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Sinclair et al., 2009) various NAA Endako 36.1 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Schindler, 1975) various NAA Endako 37.5 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Selby and Creaser, 2001b) hand-picked magnetic/heavy liquids concentrate NTIMS Endako 37.5 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Selby and Creaser, 2001b) hand-picked magnetic/heavy liquids concentrate NTIMS Endako 38.4 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Selby and Creaser, 2001b) hand-picked magnetic/heavy liquids concentrate NTIMS Endako 67 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Sinclair et al., 2009) various NAA Endako 76.9 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Selby and Creaser, 2001b) hand-picked magnetic/heavy liquids concentrate NTIMS Endako 204 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Sinclair et al., 2009) various NAA Endako 302 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Sinclair et al., 2009) various NAA Endako 397 1 Porphyry Mo granite; quartz monzonite 0.002 0.203 0 146.9 (Sinclair et al., 2009) various NAA Endani 17 1 Quartz vein-hosted granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Erdenetuin-Obo 104 1 Porphyry Cu diorite; granite; granodiorite 0.45 0.012 0 230 (Berzina et al., 2005) various various Erdenetuin-Obo 188 1 Porphyry Cu diorite; granite; granodiorite 0.45 0.012 0 230 (Berzina et al., 2005) various various Erdenetuin-Obo 199 1 Porphyry Cu diorite; granite; granodiorite 0.45 0.012 0 230 (Berzina et al., 2005) various various Ertsberg 121.16 1 Porphyry Cu-Au 0 0.6 0 0.64 2.88 (Mathur et al., 2005) hand-picked grains NTIMS Escondida 331 1 Porphyry Cu-Mo granodiorite; porphyry; quartz monzonite; rhyolite 1.1194 0.025 0.25 34.85 (Romero et al., 2011) concentrate, unknown method NTIMS Escondida 1355 1 Porphyry Cu-Mo granodiorite; porphyry; quartz monzonite; rhyolite 1.1194 0.025 0.25 34.85 (Berzina et al., 2005) various various Escondida 1355 1 Porphyry Cu-Mo granodiorite; porphyry; quartz monzonite; rhyolite 1.1194 0.025 0.25 34.85 (Mathur et al., 2000) hand-picked grains NTIMS Escondida 1449.5 1 Porphyry Cu-Mo granodiorite; porphyry; quartz monzonite; rhyolite 1.1194 0.025 0.25 34.85 (Romero et al., 2011) concentrate, unknown method NTIMS Escondida Norte 432.5 1 Porphyry Cu dacite; granodiorite; porphyry 1.119 0.025 0.25 37.2 (Romero et al., 2011) concentrate, unknown method NTIMS Escondida Norte 595.2 1 Porphyry Cu dacite; granodiorite; porphyry 1.119 0.025 0.25 37.2 (Romero et al., 2011) concentrate, unknown method NTIMS Escondida Norte 1804.4 1 Porphyry Cu dacite; granodiorite; porphyry 1.119 0.025 0.25 37.2 (Romero et al., 2011) concentrate, unknown method NTIMS Everton 265 1 Granodiorite Mo 0 0 0.3 0 376 (Luck and Allègre, 1982) unknown ID-ion probe Everton 530 1 Granodiorite Mo 0 0 0.3 0 376 (Riley, 1967) hand samples TIMS Everton 540 1 Granodiorite Mo 0 0 0.3 0 376 (Riley, 1967) hand samples TIMS Everton 630 1 Granodiorite Mo 0 0 0.3 0 376 (Riley, 1967) hand samples TIMS Fakos 1100 1 Porphyry Cu quartz monzonite 0 0 0.03 21 (Voudouris et al., 2010) hand samples EPMA Fakos 1396 5 910 2220 Porphyry Cu quartz monzonite 0 0 0.03 21 (Voudouris et al., 2013) thin sections EPMA Fakos 1900 1 Porphyry Cu quartz monzonite 0 0 0.03 21 (Voudouris et al., 2010) hand samples EPMA Fakos 11000 1 Porphyry Cu quartz monzonite 0 0 0.03 21 (Fornadel et al., 2012) hand samples EPMA Fenghuangshan 1.314 0.022 1 Skarn Cu 0 0 0 0 0 (S. Li et al., 2014) hand-picked grains ICP-MS Fenghuangshan 66.421 0.56 1 Skarn Cu 0 0 0 0 0 (S. Li et al., 2014) hand-picked grains ICP-MS Fenghuangshan 44.519 0.351 1 Skarn Cu 0 0 0 0 0 (S. Li et al., 2014) hand-picked grains ICP-MS Fenghuangshan 127.021 0.969 1 Skarn Cu 0 0 0 0 0 (S. Li et al., 2014) hand-picked grains ICP-MS Fenghuangshan 381.991 3.372 1 Skarn Cu 0 0 0 0 0 (S. Li et al., 2014) hand-picked grains ICP-MS Fengshandong 436.5 3.6 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.38 0.05 0.37 144 (Xie et al., 2007) hand-picked magnetic concentrate ICP-MS Flammefjeld 192.9 0.1 1 Porphyry Mo 0 0 0 0 48 (Brooks et al., 2004) hand-picked grains NTIMS Flekkefjord 5 1 Granite Mo granite 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Flekkefjord 5 1 Granite Mo granite 0 0 0 0 (Hiskey and Meloche, 1940) hand samples colorimetry Flekkefjord 12.1 1 Granite Mo granite 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Flinders Island 0.46 1 Intrusion-related Au granodiorite 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Flinders Island 0.48 Intrusion-related Au granodiorite 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Flottorp 13.05 0.008 1 Quartz vein-hosted Mo 0 0 0 0 951.5 (Bingen et al., 2006) micro-drilled hand samples NTIMS Flottorp 26.28 0.03 1 Quartz vein-hosted Mo 0 0 0 0 951.5 (Bingen et al., 2006) micro-drilled hand samples NTIMS Fojtka u Liberce 1.1 Granodiorite Mo granodiorite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Fojtka u Liberce 0.75 Granodiorite Mo granodiorite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Fojtka u Liberce 0.58 Granodiorite Mo granodiorite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Fojtka u Liberce 0.63 Granodiorite Mo granodiorite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Fojtka u Liberce 3.2 Granodiorite Mo granodiorite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Fort Knox 12.35 0.02 1 Intrusion-related Au granite; granodiorite 0 0 0.93 89.65 (Selby et al., 2002) unknown NTIMS Fort Knox 13.59 0.04 1 Intrusion-related Au granite; granodiorite 0 0 0.93 89.65 (Selby et al., 2002) unknown NTIMS Fort Knox 15.29 0.01 1 Intrusion-related Au granite; granodiorite 0 0 0.93 89.65 (Selby et al., 2002) unknown NTIMS Fort Knox 35.89 0.07 1 Intrusion-related Au granite; granodiorite 0 0 0.93 89.65 (Selby et al., 2002) unknown NTIMS Fort Knox 36.94 0.09 1 Intrusion-related Au granite; granodiorite 0 0 0.93 89.65 (Selby et al., 2002) unknown NTIMS Fort Knox 41.34 0.06 1 Intrusion-related Au granite; granodiorite 0 0 0.93 89.65 (Selby et al., 2002) unknown NTIMS Freiberg district 0.11 1 Five-element 0 0 0 0 0 (Mathur et al., 2010) hand-picked grains NTIMS Freiberg district 0.53 1 Five-element 0 0 0 0 0 (Mathur et al., 2010) hand-picked grains NTIMS Fukagadani 32 1 Quartz vein-hosted Mo granodiorite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Fukuoka 100.56 0.48 1 Granite Mo 0 0 0 0 89.4 (Suzuki et al., 1996) hand samples ID-ICP-MS Fukuoka-Suien 92 1 Quartz vein-hosted Cu granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Fukuoka-Suien 99 1 Quartz vein-hosted Cu granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Fusamata 0.3813 0.0074 1 Pegmatite 0 0 0 0 109 (Suzuki et al., 1996) hand samples ID-ICP-MS Fusamata 0.703 0.012 1 Pegmatite 0 0 0 0 109 (Suzuki et al., 1996) hand samples ID-ICP-MS Gaby-Papa Grande 442.9 4 1 Porphyry Au 0 0.12 0.025 0.75 19.3 (Schütte et al., 2012) concentrate, unknown method NTIMS Galeno (Cajamarca) 810 1 Porphyry Cu 0 0.474 0.01 0.11 17 (Voudouris et al., 2013) thin sections EPMA Gameleira 10.37 1 IOCG Cu-Au (Fe-Mo) alkali-granite 0 0 0 2614 (Marschik et al., 2005) hand-picked grains NTIMS Gameleira 10 1 IOCG Cu-Au (Fe-Mo) alkali-granite 0 0 0 2614 (Mathur et al., 2010) hand-picked grains NTIMS Gaotongling 8.419 0.060 Quartz vein-hosted Mo syenogranite 0 0.1 0 102.5 (Xu et al., 2016) unknown unknown Gaotongling 6.486 0.054 Quartz vein-hosted Mo syenogranite 0 0.1 0 102.5 (Xu et al., 2016) unknown unknown Gaotongling 6.325 0.028 Quartz vein-hosted Mo syenogranite 0 0.1 0 102.5 (Xu et al., 2016) unknown unknown Gaotongling 10.16 0.091 Quartz vein-hosted Mo syenogranite 0 0.1 0 102.5 (Xu et al., 2016) unknown unknown Gaotongling 7.149 0.037 Quartz vein-hosted Mo syenogranite 0 0.1 0 102.5 (Xu et al., 2016) unknown unknown Gaotongling 10.71 0.076 Quartz vein-hosted Mo syenogranite 0 0.1 0 102.5 (Xu et al., 2016) unknown unknown Gaotongling 11.58 0.110 Quartz vein-hosted Mo syenogranite 0 0.1 0 102.5 (Xu et al., 2016) unknown unknown Gaotongling 3.19 0.040 Quartz vein-hosted Mo syenogranite 0 0.1 0 102.5 (Xu et al., 2016) unknown unknown Gaotongling 11.43 0.110 Quartz vein-hosted Mo syenogranite 0 0.1 0 102.5 (Xu et al., 2016) unknown unknown Gaotongling 13.27 0.140 Quartz vein-hosted Mo syenogranite 0 0.1 0 102.5 (Xu et al., 2016) unknown unknown Gaotongling 7.95 0.080 Quartz vein-hosted Mo syenogranite 0 0.1 0 102.5 (Xu et al., 2016) unknown unknown Garfield 3.5 1 Unknown Mo 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Garfield 3.5 1 Unknown Mo 0 0 0 0 0 (Hiskey and Meloche, 1940) unknown colorimetry Garfield 6 1 Unknown Mo 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Garfield 6 1 Unknown Mo 0 0 0 0 0 (Hiskey and Meloche, 1940) unknown colorimetry Garfield 7 1 Unknown Mo 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Garfield 7 1 Unknown Mo 0 0 0 0 0 (Hiskey and Meloche, 1940) unknown colorimetry Garfield 37 1 Unknown Mo 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Garfield 37 1 Unknown Mo 0 0 0 0 0 (Hiskey and Meloche, 1940) unknown colorimetry Garfield 0 1 Unknown Mo 0 0 0 0 0 (Hiskey and Meloche, 1940) unknown colorimetry Garfield 0 1 Unknown Mo 0 0 0 0 0 (Hiskey and Meloche, 1940) unknown colorimetry Garimpo Fernando 78.87 1 IOCG alkali-granite 0 0 0 2597 (Marschik et al., 2005) hand-picked grains NTIMS Garimpo Fernando 141.68 1 IOCG alkali-granite 0 0 0 2597 (Marschik et al., 2005) hand-picked grains NTIMS Garimpo Fernando 78 1 IOCG alkali-granite 0 0 0 2597 (Mathur et al., 2010) hand-picked grains NTIMS Gaspé 84 1 Porphyry, skarn Cu 0 0.441 0.029 0 385 (Schindler, 1975) various NAA Gaspé 145 1 Porphyry, skarn Cu 0 0.441 0.029 0 385 (Schindler, 1975) various NAA Gaspé 190 1 Porphyry, skarn Cu 0 0.441 0.029 0 385 (Schindler, 1975) various NAA Gaspé 181 1 Porphyry, skarn Cu 0 0.441 0.029 0 385 (Giles and Schilling, 1972) hand samples colorimetry Getchell 26 1 Sediment-hosted granodiorite 0 0 20.1 88 (Giles and Schilling, 1972) hand samples colorimetry Getchell 34 1 Sediment-hosted granodiorite 0 0 20.1 88 (Giles and Schilling, 1972) hand samples colorimetry Giant Pebble 329 1 Porphyry Cu-Au 0 0.43 0.018 0.41 89.7 (Lang et al., 2013) unknown unknown Giant Pebble 480 1 Porphyry Cu-Au 0 0.43 0.018 0.41 89.7 (Lang et al., 2013) unknown unknown Giant Pebble 553 1 Porphyry Cu-Au 0 0.43 0.018 0.41 89.7 (Lang et al., 2013) unknown unknown Giant Pebble 616 1 Porphyry Cu-Au 0 0.43 0.018 0.41 89.7 (Lang et al., 2013) unknown unknown Giant Pebble 1399 1 Porphyry Cu-Au 0 0.43 0.018 0.41 89.7 (Lang et al., 2013) unknown unknown Giant Pebble 2070 1 Porphyry Cu-Au 0 0.43 0.018 0.41 89.7 (Lang et al., 2013) unknown unknown Gibraltar 238 1 Porphyry Cu-Au quartz diorite; tonalite; trondhjemite 0.32 0.01 0.07 207 (Sinclair et al., 2009) various NAA Gibraltar 443 1 Porphyry Cu-Au quartz diorite; tonalite; trondhjemite 0.32 0.01 0.07 207 (Sinclair et al., 2009) various NAA Gibraltar 750 1 Porphyry Cu-Au quartz diorite; tonalite; trondhjemite 0.32 0.01 0.07 207 (Sinclair et al., 2009) various NAA Glacier Gulch 34 1 Porphyry Mo quartz monzonite 0.04 0.21 0 70 (Sinclair et al., 2009) various NAA Glacier Gulch 41 1 Porphyry Mo quartz monzonite 0.04 0.21 0 70 (Sinclair et al., 2009) various NAA Gladstone 177 1 Unknown gabbro; monzonite; monzodiorite; pyroxenite; syenite 0.28 0 0 195.75 (Riley, 1967) hand samples TIMS Glen Eden 1.7 1 Granite Mo 0 0 0.06 0 0 (Riley, 1967) hand samples TIMS Glen Eden 3.5 1 Granite Mo 0 0 0.06 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Glen Eden 1.7 Granite Mo 0 0 0.06 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Godthaab 55.2 1 Unknown 0 0 0 0 1840 (Luck and Allègre, 1982) unknown ID-ion probe Gold Acres 200 100 1 Sediment-hosted quartz monzonite 0 0 3.501 82.55 (McCandless et al., 1993) hand-picked grains EPMA Gonnosfanadiga 19.8 1 Granite Mo granite 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Graniczna 58 1 Granite Mo 0 0 0 0 298 (Mikulski and Stein, 2007) micro-drilled hand samples NTIMS Granisle 522 1 Porphyry Cu granodiorite; intrusive igneous rock; quartz diorite 0.43 0.009 0.12 51.25 (Sinclair et al., 2009) various NAA Granisle 528 1 Porphyry Cu granodiorite; intrusive igneous rock; quartz diorite 0.43 0.009 0.12 51.25 (Sinclair et al., 2009) various NAA Grasberg 1405.5 1 Porphyry Cu-Au monzodiorite, diorite, monzonite 1.3 0 1.42 2.54 (Mathur et al., 2005) hand-picked grains NTIMS Grasberg 2235 1 Porphyry Cu-Au monzodiorite, diorite, monzonite 1.3 0 1.42 2.54 (Mathur et al., 2000) hand-picked grains NTIMS Gravelotte 200 200 1 Pegmatite Mo 0 0 0 0 771 (McCandless et al., 1993) hand-picked grains EPMA Gravelotte 300 200 1 Pegmatite Mo 0 0 0 0 771 (McCandless et al., 1993) hand-picked grains EPMA Guadalupe 553 1 Porphyry Cu 0 0 0 0 55 (Golden et al., 2013) unknown unknown Guaysimi–David 135 2 Skarn Au granodiorite; quartz diorite 0 0 15 146 (Chiaradia et al., 2009) hand samples NTIMS Gursli 12.637 0.008 1 Granite Mo 0 0 0 0 942.5 (Bingen et al., 2006) micro-drilled hand samples NTIMS Gursli 22.36 0.01 1 Granite Mo 0 0 0 0 942.5 (Bingen et al., 2006) micro-drilled hand samples NTIMS Gursli 29.12 0.02 1 Granite Mo 0 0 0 0 942.5 (Bingen et al., 2006) micro-drilled hand samples NTIMS Gursli 32.57 0.02 1 Granite Mo 0 0 0 0 942.5 (Bingen et al., 2006) micro-drilled hand samples NTIMS Haft Cheshmeh 111.7 1 1 Porphyry Cu-Mo granodiorite 0.26 0.03 0 27.61 (Aghazadeh et al., 2015) hand-picked grains unknown Haft Cheshmeh 241 1.8 1 Porphyry Cu-Mo granodiorite 0.26 0.03 0 27.61 (Aghazadeh et al., 2015) hand-picked grains unknown Hagi 5.4 1 Quartz vein-hosted granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Haley Station 6.9 1 Unknown 0 0 0 0 870.1 (Golden et al., 2013) unknown unknown Halifax Bay 6.7 1 Unknown 0 0 0 0 0 (Riley, 1967) hand samples TIMS Hankus 420 1 Pegmatite 0 0 0 0 0 (Lavrov and Kuleshevich, 2010) unknown SEM Harrachov 0.17 Granite Mo granite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Harrachov 0.51 Granite Mo granite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Harrachov 0.15 Granite Mo granite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Harrachov 0.04 Granite Mo granite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Harrachov 0.07 Granite Mo granite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Hata 10.05 0.073 1 Quartz vein-hosted Mo 0 0 0 0 0 (Suzuki et al., 1996) hand samples ID-ICP-MS Hata 12.904 0.074 1 Quartz vein-hosted Mo 0 0 0 0 0 (Suzuki et al., 1996) hand samples ID-ICP-MS Hata 34.08 0.32 1 Quartz vein-hosted Mo 0 0 0 0 0 (Suzuki et al., 1996) hand samples ID-ICP-MS Hata 137 1 Quartz vein-hosted Mo 0 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Heemskirk 0.011 1 Granite Sn 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Heemskirk 0.009 Granite Sn 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Henderson 11.190313 0.01725 50 Porphyry Mo rhyolite; granite 0 0.168 0 28.465 (Markey et al., 2007) flotation concentrate NTIMS Henderson 11.36 0.04 1 Porphyry Mo rhyolite; granite 0 0.168 0 28.465 (Lawley and Selby, 2012) Mo powder NTIMS Henderson 11.39 0.04 1 Porphyry Mo rhyolite; granite 0 0.168 0 28.465 (Lawley and Selby, 2012) Mo powder NTIMS Henderson 100 100 1 Porphyry Mo rhyolite; granite 0 0.168 0 28.465 (McCandless et al., 1993) hand-picked grains EPMA Henderson 100 100 1 Porphyry Mo rhyolite; granite 0 0.168 0 28.465 (McCandless et al., 1993) hand-picked grains EPMA Herberton 7.3 1 Breccia pipe 0 0 0 0 0 (Riley, 1967) hand samples TIMS Higashiyama 38.52 0.1 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Suzuki et al., 1996) hand samples ID-ICP-MS Higashiyama 39.65 0.28 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Suzuki et al., 1996) hand samples ID-ICP-MS Higashiyama 48 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama 80 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama 71 18 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Ishihara, 1988) various NAA/spectrophotometry Higashiyama 155 2 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Ishihara, 1988) various NAA/spectrophotometry Higashiyama—Ashidani 140 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Ishihara, 1988) various NAA/spectrophotometry Higashiyama—Higashiyama 140 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Higashiyama 150 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Ishihara, 1988) various NAA/spectrophotometry Higashiyama—Kawahira 30 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Kawahira 97 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Kawahira 66 2 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Ishihara, 1988) various NAA/spectrophotometry Higashiyama—Maruyama 5 89 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Maruyama shin 190 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Onobe 1 150 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Onobe 2 38 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Onobe 2 65 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Onobe 3 21 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Onobe 3 120 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Onobe 4 42 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Onobe 4 79 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Onobe 5 74 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Onobe Tate-hi 27 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Onobe Uwa-hi 49 1 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Terada et al., 1971) hand-picked grains NAA Higashiyama—Yoshitoko 23.5 2 Quartz vein-hosted granite; granodiorite 0 0 0 62.15 (Ishihara, 1988) various NAA/spectrophotometry Highmont 95.7 1 Porphyry Cu-Mo granodiorite; quartz monzonite 0.266 0.041 0.004 208 (Schindler, 1975) various NAA Highmont 137 1 Porphyry Cu-Mo granodiorite; quartz monzonite 0.266 0.041 0.004 208 (Sinclair et al., 2009) various NAA Highmont 176 1 Porphyry Cu-Mo granodiorite; quartz monzonite 0.266 0.041 0.004 208 (Sinclair et al., 2009) various NAA Highmont 530 1 Porphyry Cu-Mo granodiorite; quartz monzonite 0.266 0.041 0.004 208 (Sinclair et al., 2009) various NAA Hilltop 90 16 29 139 Porphyry, epithermal 0 0 0 0 0 (Ciobanu et al., 2013) hand samples LA-ICP-MS Hilltop 107 17 37 318 Porphyry, epithermal 0 0 0 0 0 (Ciobanu et al., 2013) hand samples LA-ICP-MS Hilltop 449.67 3 34 724 Porphyry, epithermal 0 0 0 0 0 (Ciobanu et al., 2013) hand samples LA-ICP-MS Hilltop 1186 24 34 3370 Porphyry, epithermal 0 0 0 0 0 (Ciobanu et al., 2013) hand samples LA-ICP-MS Hilltop 77 6 41 101 Porphyry, epithermal 0 0 0 0 0 (Ciobanu et al., 2013) hand samples LA-ICP-MS Hilltop 580 17 172 727 Porphyry, epithermal 0 0 0 0 0 (Ciobanu et al., 2013) hand samples LA-ICP-MS Hilltop 827 58 34 3370 Porphyry, epithermal 0 0 0 0 0 (Ciobanu et al., 2013) hand samples LA-ICP-MS Hilltop 428 11 184 1531 Porphyry, epithermal 0 0 0 0 0 (Ciobanu et al., 2013) hand samples LA-ICP-MS Hirase 5.8 39 Quartz vein-hosted granite 0 0 0 65.4 (Ishihara, 1988) various NAA/spectrophotometry Hirase 9.4 1 Quartz vein-hosted granite 0 0 0 65.4 (Suzuki et al., 1996) hand samples ID-ICP-MS Hirase 9.406 0.048 1 Quartz vein-hosted granite 0 0 0 65.4 (Suzuki et al., 1996) hand samples ID-ICP-MS Hirase 11 1 Quartz vein-hosted granite 0 0 0 65.4 (Suzuki et al., 1996) hand samples ID-ICP-MS Hirase 11.2 1 Quartz vein-hosted granite 0 0 0 65.4 (Terada et al., 1967) unknown NAA Hirase 11.2 1 Quartz vein-hosted granite 0 0 0 65.4 (Terada et al., 1967) unknown NAA Hirase 11.24 0.024 1 Quartz vein-hosted granite 0 0 0 65.4 (Suzuki et al., 1996) hand samples ID-ICP-MS Hirase 11.3 1 Quartz vein-hosted granite 0 0 0 65.4 (Terada et al., 1967) unknown NAA Hirase 11.4 1 Quartz vein-hosted granite 0 0 0 65.4 (Terada et al., 1967) unknown NAA Hiyoshi 2.2 1 Quartz vein-hosted granite; peridotite 0 0 0 0.0057385 (Terada et al., 1971) hand-picked grains NAA Hnilec 3.6 1 Granite W-Mo granite 0 0 0 264.6 (Kohut and Stein, 2005) concentrate, unknown method NTIMS Hnilec 4.2 1 Granite W-Mo granite 0 0 0 264.6 (Kohut and Stein, 2005) concentrate, unknown method NTIMS Hokuto 11 1 Granite Mo granite 0 0 0 124 (Ishihara, 1988) various NAA/spectrophotometry Hokuto 12.96 0.09 1 Granite Mo granite 0 0 0 124 (Suzuki et al., 1996) hand samples ID-ICP-MS Hokuto 13.5 0.14 1 Granite Mo granite 0 0 0 124 (Suzuki et al., 1996) hand samples ID-ICP-MS Hongling 135.7 1.014 Quartz vein-hosted Mo Unknown 0 0 0 0 (Xu et al., 2016) unknown unknown Hongling 142.4 1.790 Quartz vein-hosted Mo Unknown 0 0 0 0 (Xu et al., 2016) unknown unknown Hongmenling 0.3144 0.003 Porphyry Mo-W granite, syenogranite 0 0.24 0 72 (Xu et al., 2016) unknown unknown Hongmenling 0.3472 0.003 Porphyry Mo-W granite, syenogranite 0 0.24 0 72 (Xu et al., 2016) unknown unknown Horado 13 1 Skarn Pb-Zn granitoid 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Huangjiawan 10.438 1 Sediment-hosted 0 0 5.5 0 557 (Mao et al., 2002) hand samples NTIMS Huangjiawan 10.268 1 Sediment-hosted 0 0 5.5 0 557 (Mao et al., 2002) hand samples NTIMS Huangjiawan 12.682 1 Sediment-hosted 0 0 5.5 0 557 (Mao et al., 2002) hand samples NTIMS Huangjiawan 10.901 1 Sediment-hosted 0 0 5.5 0 557 (Mao et al., 2002) hand samples NTIMS Huangjiawan 12.193 1 Sediment-hosted 0 0 5.5 0 557 (Mao et al., 2002) hand samples NTIMS Huangjiawan 11.358 Sediment-hosted 0 0 5.5 0 557 (Mao et al., 2002) hand samples NTIMS Huangjiawan 10.856 Sediment-hosted 0 0 5.5 0 557 (Mao et al., 2002) hand samples NTIMS Huanglongpu 256 3.5 1 Carbonatite Mo (Pb) 0 0 0 0 221 (Mao et al., 1999) various various Huanglongpu 278.1 5 1 Carbonatite Mo (Pb) 0 0 0 0 221 (Stein et al., 1997) flotation concentrate ICP-MS Huanglongpu 281.8 5 1 Carbonatite Mo (Pb) 0 0 0 0 221 (Stein et al., 1997) flotation concentrate ICP-MS Huanglongpu 282.7 5 1 Carbonatite Mo (Pb) 0 0 0 0 221 (Stein et al., 1997) flotation concentrate ICP-MS Huanglongpu 283.5 6.9 1 Carbonatite Mo (Pb) 0 0 0 0 221 (Mao et al., 1999) various various Huanglongpu 283.8 6.2 192 Carbonatite Mo (Pb) 0 0 0 0 221 (Du et al., 2004) flotation concentrate NTIMS Huanglongpu 284.4 5 1 Carbonatite Mo (Pb) 0 0 0 0 221 (Stein et al., 1997) flotation concentrate ICP-MS Huanglongpu 284.43 1.22 19 281.8 289.1 Carbonatite Mo (Pb) 0 0 0 0 221 (Markey et al., 1998) hand-picked heavy liquid concentrate NTIMS Huanglongpu 284.5 5 1 Carbonatite Mo (Pb) 0 0 0 0 221 (Stein et al., 1997) flotation concentrate ICP-MS Huanglongpu 285.3 5 1 Carbonatite Mo (Pb) 0 0 0 0 221 (Stein et al., 1997) flotation concentrate ICP-MS Huanglongpu 289.1 6 1 Carbonatite Mo (Pb) 0 0 0 0 221 (Stein et al., 1997) flotation concentrate ICP-MS Huanglongpu 319.9 2.42 1 Carbonatite Mo (Pb) 0 0 0 0 221 (Lawley and Selby, 2012) magnetic and heavy-liquid concentrate NTIMS Huanglongpu 438.6 6 1 Carbonatite Mo (Pb) 0 0 0 0 221 (Mao et al., 1999) various various Huanglongpu 530.6 12.9 1 Carbonatite Mo (Pb) 0 0 0 0 221 (Mao et al., 1999) various various Huanglongpu 633.1 5.4 1 Carbonatite Mo (Pb) 0 0 0 0 221 (Mao et al., 1999) various various Huangshaping 0.46 1 Skarn Pb-Zn 0 0 0 0 161.6 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Huangshaping 2.59 1 Skarn Pb-Zn 0 0 0 0 161.6 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Huangshaping 3.107 1 Skarn Pb-Zn 0 0 0 0 161.6 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Huangshaping 46.826 1 Skarn Pb-Zn 0 0 0 0 161.6 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Huangshaping 5 7 1.2 8.7 Skarn Pb-Zn 0 0 0 0 161.6 (Zhong et al., 2017) various various Huangshaping 14.3 4 3.1 46.8 Skarn Pb-Zn 0 0 0 0 161.6 (Zhong et al., 2017) various various Huatong 14.58 0.084 Skarn Cu granite 0.88 0.13 0 127.4 (Zhang et al., 2016) hand-picked magnetic concentrate ICP-MS Huatong 4.88 0.042 Skarn Cu granite 0.88 0.13 0 127.4 (Zhang et al., 2016) hand-picked magnetic concentrate ICP-MS Huatong 91.02 0.819 Skarn Cu granite 0.88 0.13 0 127.4 (Zhang et al., 2016) hand-picked magnetic concentrate ICP-MS Huatong 2.11 0.012 Skarn Cu granite 0.88 0.13 0 127.4 (Zhang et al., 2016) hand-picked magnetic concentrate ICP-MS Huatong 35.52 0.261 Skarn Cu granite 0.88 0.13 0 127.4 (Zhang et al., 2016) hand-picked magnetic concentrate ICP-MS Hubsky 1.29 Greisen 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Hubsky 0.54 Greisen 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Hubsky 0.46 Greisen 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Hubsky 0.51 Greisen 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Hubsky 0.3 Greisen 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Hubsky 0.4 Greisen 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Huckleberry 247 1 Porphyry Cu granodiorite 0.48 0.015 0.025 82.75 (Sinclair et al., 2009) various NAA Huckleberry 258 1 Porphyry Cu granodiorite 0.48 0.015 0.025 82.75 (Sinclair et al., 2009) various NAA Hukeng 2.85 1 Quartz vein-hosted W 0 0 0 0 150.2 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Hukeng 7.45 1 Quartz vein-hosted W 0 0 0 0 150.2 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Huky u Rakovnika 9.79 0.020 1 Carbonatite-related 0 0 0 0 373 (Ackerman et al., 2017) hand-picked grains ICP-MS Hurky u Nove Bystrice 2.5 0.010 1 Quartz vein-hosted 0 0 0 0 325 (Ackerman et al., 2017) hand-picked grains ICP-MS Hurky u Nove Bystrice 0.64 Quartz vein-hosted 0 0 0 0 325 (Pasava et al., 2016) polished mounts LA-ICP-MS Hurky u Nove Bystrice 0.65 Quartz vein-hosted 0 0 0 0 325 (Pasava et al., 2016) polished mounts LA-ICP-MS Hurky u Nove Bystrice 0.9 Quartz vein-hosted 0 0 0 0 325 (Pasava et al., 2016) polished mounts LA-ICP-MS Hurky u Nove Bystrice 0.36 Quartz vein-hosted 0 0 0 0 325 (Pasava et al., 2016) polished mounts LA-ICP-MS Hurky u Nove Bystrice 0.37 Quartz vein-hosted 0 0 0 0 325 (Pasava et al., 2016) polished mounts LA-ICP-MS Hurky u Nove Bystrice 0.46 Quartz vein-hosted 0 0 0 0 325 (Pasava et al., 2016) polished mounts LA-ICP-MS Hurley 17.5 1 Unknown 0 0 0 0 0 (Hiskey and Meloche, 1940) flotation concentrate colorimetry Hvaleroyene 90 1 Granite Mo Granite 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Ichihata 0.04 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Ida 1.9 1 Quartz vein-hosted Mo granite 0.49 0 0.098 0 (Terada et al., 1971) hand-picked grains NAA Ida 5.8 1 Quartz vein-hosted Mo granite 0.49 0 0.098 0 (Terada et al., 1971) hand-picked grains NAA Idaho Creek 43.22 0.25 1 Porphyry Cu-Mo quartz monzonite 0 0 0 0 (Selby and Creaser, 2001a) hand-picked magnetic/heavy liquids concentrate NTIMS Iju 938 10 1 Porphyry Cu quartz diorite 0.31 0.002 0 9.13 (Aghazadeh et al., 2015) hand-picked grains unknown Iju 945 8 1 Porphyry Cu quartz diorite 0.31 0.002 0 9.13 (Aghazadeh et al., 2015) hand-picked grains unknown Inca de Oro 344 1 Porphyry Cu 0 0 0 0 63 (Mathur et al., 2010) hand-picked grains NTIMS Inca de Oro 574 1 Porphyry Cu 0 0 0 0 63 (Mathur et al., 2010) hand-picked grains NTIMS Ingerbelle 1620 1 Porphyry Cu-Au monzodiorite 0.473 0.002 0.17 198.5 (Sinclair et al., 2009) various NAA Inveran 0.531 0.001 1 Granite Mo granite 0 0 0 399.5 (Feely et al., 2010) magnetic concentrate NTIMS Io-zima 1900 1 Volcanic sublimate rhyolite 0.002 0.41 0.001 0.00001 (Terada et al., 1971) hand-picked grains NAA Io-zima 3700 1 Volcanic sublimate rhyolite 0.002 0.41 0.001 0.00001 (Terada et al., 1971) hand-picked grains NAA Ishizuchi 8.6 1 Quartz vein-hosted Cu granodiorite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Island Copper 1198 1 Porphyry Cu-Au granitoid; rhyodacite 0.41 0.017 0.19 170.95 (Arancibia and Clark, 1996) flotation concentrate calculated from concentrate assay Island Copper 1704 1 Porphyry Cu-Au granitoid; rhyodacite 0.41 0.017 0.19 170.95 (Sinclair et al., 2009) various NAA Island Copper 1863 1 Porphyry Cu-Au granitoid; rhyodacite 0.41 0.017 0.19 170.95 (Sinclair et al., 2009) various NAA Iyadani 55 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Iyadani 59 1 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Jachymov 0.87 0.003 1 Five-element/greisen granite 0 0 0 325 (Ackerman et al., 2017) hand-picked grains ICP-MS Jachymov 0.09 Five-element/greisen granite 0 0 0 325 (Pasava et al., 2016) polished mounts LA-ICP-MS Jachymov 0.04 Five-element/greisen granite 0 0 0 325 (Pasava et al., 2016) polished mounts LA-ICP-MS Jachymov 0.52 Five-element/greisen granite 0 0 0 325 (Pasava et al., 2016) polished mounts LA-ICP-MS Jachymov 0.36 Five-element/greisen granite 0 0 0 325 (Pasava et al., 2016) polished mounts LA-ICP-MS Jachymov 0.1 Five-element/greisen granite 0 0 0 325 (Pasava et al., 2016) polished mounts LA-ICP-MS Jalonvaara 46.9 1 Porphyry Cu-Mo 0 0 0 1.65 2730 (Lavrov and Kuleshevich, 2010) unknown SEM Jalonvaara 176.6 1 Porphyry Cu-Mo 0 0 0 1.65 2730 (Lavrov and Kuleshevich, 2010) unknown SEM Jaspinal's Mountain Station 8.9 1 Unknown 0 0 0 0 0 (Riley, 1967) hand samples TIMS Jiama 393.3 3.4 1 Porphyry Cu 0 0 0 0 15.18 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Jiama 397.1 3.8 1 Porphyry Cu 0 0 0 0 15.18 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Jiama 401.1 3.9 1 Porphyry Cu 0 0 0 0 15.18 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Jiama 428.5 4.2 1 Porphyry Cu 0 0 0 0 15.18 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Jiama 430.7 4.1 1 Porphyry Cu 0 0 0 0 15.18 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Jiama 448.7 4.1 1 Porphyry Cu 0 0 0 0 15.18 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Jiama 559.5 5.4 1 Porphyry Cu 0 0 0 0 15.18 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Jidetun 6.29 1 Porphyry Mo monzogranite, granodiorite 168.9 (Z. Wang et al., 2017) hand-picked magnetic concentrate ICP-MS Jidetun 4.095 1 Porphyry Mo monzogranite, granodiorite 168.9 (Z. Wang et al., 2017) hand-picked magnetic concentrate ICP-MS Jidetun 7.325 1 Porphyry Mo monzogranite, granodiorite 168.9 (Z. Wang et al., 2017) hand-picked magnetic concentrate ICP-MS Jidetun 3.073 1 Porphyry Mo monzogranite, granodiorite 168.9 (Z. Wang et al., 2017) hand-picked magnetic concentrate ICP-MS Jidetun 9.747 1 Porphyry Mo monzogranite, granodiorite 168.9 (Z. Wang et al., 2017) hand-picked magnetic concentrate ICP-MS Jidetun 4.265 1 Porphyry Mo monzogranite, granodiorite 168.9 (Z. Wang et al., 2017) hand-picked magnetic concentrate ICP-MS Jidetun 7.836 1 Porphyry Mo monzogranite, granodiorite 168.9 (Z. Wang et al., 2017) hand-picked magnetic concentrate ICP-MS Jidetun 5.032 1 Porphyry Mo monzogranite, granodiorite 168.9 (Z. Wang et al., 2017) hand-picked magnetic concentrate ICP-MS Jigongcun 1514 Quartz vein-hosted Mo granodiorite 0 0 0 22.55 (Wang et al., 2016) hand samples MC-ICP-MS Jiguanshan 9.442 0.077 1 Porphyry Mo 0 0 0 0 0 (Wu et al., 2011) hand-picked magnetic concentrate ICP-MS Jiguanshan 9.549 0.081 1 Porphyry Mo 0 0 0 0 0 (Wu et al., 2011) hand-picked magnetic concentrate ICP-MS Jiguanshan 9.944 0.077 1 Porphyry Mo 0 0 0 0 0 (Wu et al., 2011) hand-picked magnetic concentrate ICP-MS Jiguanshan 11.451 0.144 1 Porphyry Mo 0 0 0 0 0 (Wu et al., 2011) hand-picked magnetic concentrate ICP-MS Jiguanshan 11.484 0.119 1 Porphyry Mo 0 0 0 0 0 (Wu et al., 2011) hand-picked magnetic concentrate ICP-MS Jiguanshan 17.794 0.151 1 Porphyry Mo 0 0 0 0 0 (Wu et al., 2011) hand-picked magnetic concentrate ICP-MS Jiguanshan 24.431 0.217 1 Porphyry Mo 0 0 0 0 0 (Wu et al., 2011) hand-picked magnetic concentrate ICP-MS Jiguanshan 28.842 0.261 1 Porphyry Mo 0 0 0 0 0 (Wu et al., 2011) hand-picked magnetic concentrate ICP-MS Jiguanshan 31.612 0.239 1 Porphyry Mo 0 0 0 0 0 (Wu et al., 2011) hand-picked magnetic concentrate ICP-MS Jiguanshan 32.224 0.249 1 Porphyry Mo 0 0 0 0 0 (Wu et al., 2011) hand-picked magnetic concentrate ICP-MS Jiguanshan 39.481 0.32 1 Porphyry Mo 0 0 0 0 0 (Wu et al., 2011) hand-picked magnetic concentrate ICP-MS Jiguanshan 42.265 0.311 1 Porphyry Mo 0 0 0 0 0 (Wu et al., 2011) hand-picked magnetic concentrate ICP-MS Jiguanshan 45.315 0.423 1 Porphyry Mo 0 0 0 0 0 (Wu et al., 2011) hand-picked magnetic concentrate ICP-MS Jiguanzui 425.7 3.2 1 Skarn Au-Cu quartz diorite 2.2 0 3.6 138 (Xie et al., 2011) hand-picked grains ICP-MS Jiguanzui 500.4 3.8 1 Skarn Au-Cu quartz diorite 2.2 0 3.6 138 (Xie et al., 2011) hand-picked grains ICP-MS Jiguanzui 785.9 6 1 Skarn Au-Cu quartz diorite 2.2 0 3.6 138 (Xie et al., 2011) hand-picked grains ICP-MS Jiguanzui 810.8 6.8 1 Skarn Au-Cu quartz diorite 2.2 0 3.6 138 (Xie et al., 2011) hand-picked grains ICP-MS Jiguanzui 1152 10 1 Skarn Au-Cu quartz diorite 2.2 0 3.6 138 (Xie et al., 2011) hand-picked grains ICP-MS Jinduncheng 12.9 0.4 1 Porphyry Mo granite; granodiorite; quartz monzonite 0.03 0.1 0 135.5 (Mao et al., 1999) various various Jinduncheng 15.8 0.5 1 Porphyry Mo granite; granodiorite; quartz monzonite 0.03 0.1 0 135.5 (Mao et al., 1999) various various Jinduncheng 17 5 13 20 Porphyry Mo granite; granodiorite; quartz monzonite 0.03 0.1 0 135.5 (Berzina et al., 2005) various various Jinduncheng 17.33 5 1 Porphyry Mo granite; granodiorite; quartz monzonite 0.03 0.1 0 135.5 (Stein et al., 1997) flotation concentrate ICP-MS Jinduncheng 17.39 0.32 96 Porphyry Mo granite; granodiorite; quartz monzonite 0.03 0.1 0 135.5 (Du et al., 2004) flotation concentrate NTIMS Jinduncheng 17.4 5 1 Porphyry Mo granite; granodiorite; quartz monzonite 0.03 0.1 0 135.5 (Stein et al., 1997) flotation concentrate ICP-MS Jinduncheng 19.7 0.5 1 Porphyry Mo granite; granodiorite; quartz monzonite 0.03 0.1 0 135.5 (Mao et al., 1999) various various Jingera 38 1 Breccia pipe Bi-Mo (U) granite 0 0 0 0 (Riley, 1967) hand samples TIMS Jiru 81.87 Porphyry Mo monzogranite 0 0 0 44.9 (Wang et al., 2016) hand samples MC-ICP-MS Jitoushan 15.1 8 6.4 19.1 Porphyry W-Mo granodiorite 0 0 0 136.6 (Zhong et al., 2017) various various Junin 294.4 2 1 Porphyry Cu-Mo granodiorite 0.71 0.026 0 6.5 (Schütte et al., 2012) concentrate, unknown method NTIMS Junin 408.8 3 1 Porphyry Cu-Mo granodiorite 0.71 0.026 0 6.5 (Schütte et al., 2012) concentrate, unknown method NTIMS Kabeliai 2.393 1 Granite Mo granite 0 0 0 1496 (Stein et al., 1998) unknown NTIMS Kabeliai 170 0.3 1 Granite Mo granite 0 0 0 1496 (Markey et al., 1998) hand-picked heavy liquid concentrate NTIMS Kabeliai 176.2 1.6 1 Granite Mo granite 0 0 0 1496 (Markey et al., 1998) hand-picked heavy liquid concentrate NTIMS Kabeliai 183.5 1.5 1 Granite Mo granite 0 0 0 1496 (Markey et al., 1998) hand-picked heavy liquid concentrate NTIMS Kabeliai 2.992 1 Granite Mo granite 0 0 0 1496 (Stein et al., 1998) unknown NTIMS Kadzharan 160 1 Porphyry Cu-Au diorite; gabbro; granite; granodiorite; lamprophyre; quartz monzonite; syenite 0.65 0.05 0.65 22 (Fleischer, 1960) unknown colorimetry Kadzharan 245 237 33 2620 Porphyry Cu-Au diorite; gabbro; granite; granodiorite; lamprophyre; quartz monzonite; syenite 0.65 0.05 0.65 22 (Berzina et al., 2005) various various Kadzharan 410 1 Porphyry Cu-Au diorite; gabbro; granite; granodiorite; lamprophyre; quartz monzonite; syenite 0.65 0.05 0.65 22 (Fleischer, 1960) unknown colorimetry Kafang 7.717 0.1 1 Sediment-hosted Cu-Sn granite 0 0 0 84.47 (Cheng et al., 2012) hand-picked magnetic concentrate ICP-MS Kafang 9.271 0.1 1 Sediment-hosted Cu-Sn granite 0 0 0 84.47 (Cheng et al., 2012) hand-picked magnetic concentrate ICP-MS Kafang 10.7 0.1 1 Sediment-hosted Cu-Sn granite 0 0 0 84.47 (Cheng et al., 2012) hand-picked magnetic concentrate ICP-MS Kafang 10.73 0.1 1 Sediment-hosted Cu-Sn granite 0 0 0 84.47 (Cheng et al., 2012) hand-picked magnetic concentrate ICP-MS Kafang 13.16 0.1 1 Sediment-hosted Cu-Sn granite 0 0 0 84.47 (Cheng et al., 2012) hand-picked magnetic concentrate ICP-MS Kafang 23.6 0.2 1 Skarn Cu-Sn granite 0 0 0 84.47 (Cheng et al., 2012) hand-picked magnetic concentrate ICP-MS Kafang 25.09 0.2 1 Skarn Cu-Sn granite 0 0 0 84.47 (Cheng et al., 2012) hand-picked magnetic concentrate ICP-MS Kafang 29.8 0.2 1 Skarn Cu-Sn granite 0 0 0 84.47 (Cheng et al., 2012) hand-picked magnetic concentrate ICP-MS Kafang 36.66 0.3 1 Skarn Cu-Sn granite 0 0 0 84.47 (Cheng et al., 2012) hand-picked magnetic concentrate ICP-MS Kafang 39.1 0.4 1 Skarn Cu-Sn granite 0 0 0 84.47 (Cheng et al., 2012) hand-picked magnetic concentrate ICP-MS Kahang Middle 1332 11 1 Porphyry Cu-Mo 0 0 0 0 15.17 (Aghazadeh et al., 2015) hand-picked grains unknown Kaifu 0.24 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Kaifu 0.3 1 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Kakeya 32 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Kakeya 37 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Kakeya 39 2 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Kal’makyr 1500 20 700 2000 Porphyry Cu-Mo 0 0.39 0.005 0.065 0 (Berzina et al., 2005) various various Kalinovskoe 228.1 1.000 Porphyry Cu-Mo diorite 0.46 0 0.1 429.8 (Tessalina and Plotinskaya, 2017) hand-picked grains ID-TIMS Kalinovskoe 81.5 0.200 Porphyry Cu-Mo diorite 0.46 0 0.1 429.8 (Tessalina and Plotinskaya, 2017) hand-picked grains ID-TIMS Kalinovskoe 147 0.400 Porphyry Cu-Mo diorite 0.46 0 0.1 429.8 (Tessalina and Plotinskaya, 2017) hand-picked grains ID-TIMS Kalmakyr 293 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 291 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 200 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 267 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 340 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 228 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 245 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 193 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 166 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 160 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 167 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 217 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 235 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 229 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 269 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 272 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Pasava et al., 2016) polished mounts LA-ICP-MS Kalmakyr 135 1.000 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Zhao et al., 2017) hand-picked magnetic concentrate ICP-MS Kalmakyr 98 1.000 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Zhao et al., 2017) hand-picked magnetic concentrate ICP-MS Kalmakyr 899 18.000 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Zhao et al., 2017) hand-picked magnetic concentrate ICP-MS Kalmakyr 676 5.000 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Zhao et al., 2017) hand-picked magnetic concentrate ICP-MS Kalmakyr 774 6.000 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Zhao et al., 2017) hand-picked magnetic concentrate ICP-MS Kalmakyr 670 6.000 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Zhao et al., 2017) hand-picked magnetic concentrate ICP-MS Kalmakyr 865 8.000 Porphyry Cu-Mo granodiorite 0.38 0.006 0.6 270 (Zhao et al., 2017) hand-picked magnetic concentrate ICP-MS Kamenny Privoz 46.13 0.120 1 Granite Mo granodiorite 0 0 0 354 (Ackerman et al., 2017) hand-picked grains ICP-MS Kamioka 5.1 1 Porphyry Mo granite 0 0 0 82.55 (Terada et al., 1971) hand-picked grains NAA Kamioka 6.1 Porphyry Mo granite 0 0 0 82.55 (Ishihara, 1988) various NAA/spectrophotometry Kamitani 56.98 0.35 1 Quartz vein-hosted Mo 0 0 0 0 60.55 (Suzuki et al., 1996) hand samples ID-ICP-MS Kamitani 58.82 0.37 1 Quartz vein-hosted Mo 0 0 0 0 60.55 (Suzuki et al., 1996) hand samples ID-ICP-MS Kamiyamasa—Kami-Yamasa 220 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Kamiyamasa—Kami-Yamasa 230 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Kamiyamasa—Kami-Yamasa 240 2 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Kamo 1.5 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Kamo 8.7 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Kamo 6.8 2 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Kamokura 81.7 3 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Kansanshi 89 1 Sediment-hosted 0 2.32 0 0 507.4 (Torrealday et al., 2000) concentrate, unknown method NTIMS Kansanshi 97 1 Sediment-hosted 0 2.32 0 0 507.4 (Torrealday et al., 2000) concentrate, unknown method NTIMS Kansanshi 227 1 Sediment-hosted 0 2.32 0 0 507.4 (Torrealday et al., 2000) concentrate, unknown method NTIMS Kansanshi 370 1 Sediment-hosted 0 2.32 0 0 507.4 (Torrealday et al., 2000) concentrate, unknown method NTIMS Kara Oba 1 1 Greisen W-Mo 0 0 0 0 0 (Fleischer, 1960) unknown colorimetry Kara Oba 5.8 1 Greisen W-Mo 0 0 0 0 0 (Fleischer, 1960) unknown colorimetry Kara Oba 3.3 10 Greisen W-Mo 0 0 0 0 0 (Fleischer, 1960) unknown colorimetry Karacaali 16.25 1 Granite Mo granite; granitoid 0 0 0 0 (Delibaş and Genç, 2012) hand samples NTIMS Karacaali 65.3 1 Granite Mo granite; granitoid 0 0 0 0 (Delibaş and Genç, 2012) hand samples NTIMS Karacaali 74.78 1 Granite Mo granite; granitoid 0 0 0 0 (Delibaş and Genç, 2012) hand samples NTIMS Kasejovice 0.6 Intrusion-related Au granodiorite 0 0 0 338.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Kasejovice 15 Granite Mo granodiorite 0 0 0 338.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Kasejovice 10 Granite Mo granodiorite 0 0 0 338.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Kataberget 7.982 0.006 1 Granite Mo granite 0 0 0 1884.5 (Stein, 2006) hand samples NTIMS Kataberget 8.489 0.003 1 Granite Mo granite 0 0 0 1884.5 (Stein, 2006) hand samples NTIMS Kataberget 8.65 0.003 1 Granite Mo granite 0 0 0 1884.5 (Stein, 2006) hand samples NTIMS Kataberget 11.153 0.006 1 Granite Mo granite 0 0 0 1884.5 (Stein, 2006) hand samples NTIMS Kataberget 15.124 0.009 1 Granite Mo granite 0 0 0 1884.5 (Stein, 2006) hand samples NTIMS Kawauchi 1.5 1 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Keketuohai 165.5 1.7 1 Pegmatite biotite gneiss; gabbro 0 0 0 0 (Liu et al., 2014) hand samples ICP-MS Keketuohai 174.1 1.4 1 Pegmatite biotite gneiss; gabbro 0 0 0 0 (Liu et al., 2014) hand samples ICP-MS Keketuohai 432.9 3.8 1 Pegmatite biotite gneiss; gabbro 0 0 0 0 (Liu et al., 2014) hand samples ICP-MS Keketuohai 517.2 5 1 Pegmatite biotite gneiss; gabbro 0 0 0 0 (Liu et al., 2014) hand samples ICP-MS Keketuohai 529.7 4.5 1 Pegmatite biotite gneiss; gabbro 0 0 0 0 (Liu et al., 2014) hand samples ICP-MS Keketuohai 551.5 7.7 1 Pegmatite biotite gneiss; gabbro 0 0 0 0 (Liu et al., 2014) hand samples ICP-MS Kemess South 3106 1 Porphyry Cu-Au granodiorite; quartz diorite; quartz monzodiorite; quartz monzonite; syenite 0.22 0.008 0.65 200.5 (Duuring et al., 2009) magnetic concentrate ID-MS, NTIMS Kemess South 4609 1 Porphyry Cu-Au granodiorite; quartz diorite; quartz monzodiorite; quartz monzonite; syenite 0.22 0.008 0.65 200.5 (Duuring et al., 2009) magnetic concentrate ID-MS, NTIMS Kenge 7.4 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley and Selby, 2012) hand-picked magnetic/heavy liquids/HF concentrate NTIMS Kenge 8.55 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley and Selby, 2012) hand-picked magnetic/heavy liquids/HF concentrate NTIMS Kenge 10.16 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley et al., 2013) hand-picked magnetic/heavy liquids concentrate NTIMS Kenge 13.35 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley and Selby, 2012) hand-picked magnetic/heavy liquids/HF concentrate NTIMS Kenge 30.22 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley et al., 2013) hand-picked magnetic/heavy liquids concentrate NTIMS Kenge 30.33 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley et al., 2013) hand-picked magnetic/heavy liquids concentrate NTIMS Kenge 31.22 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley et al., 2013) hand-picked magnetic/heavy liquids concentrate NTIMS Kenge 46.39 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley et al., 2013) hand-picked magnetic/heavy liquids concentrate NTIMS Kenge 82.07 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley et al., 2013) hand-picked magnetic/heavy liquids concentrate NTIMS Kenge 92.31 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley et al., 2013) hand-picked magnetic/heavy liquids concentrate NTIMS Kenge 1.96 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley and Selby, 2012) hand-picked magnetic/heavy liquids/HF concentrate NTIMS Kenge 1.72 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley and Selby, 2012) hand-picked magnetic/heavy liquids/HF concentrate NTIMS Kenge 3.35 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley and Selby, 2012) hand-picked magnetic/heavy liquids/HF concentrate NTIMS Kenge 10.29 1 Orogenic Au diorite; gabbro 0 0 1.33 1953 (Lawley and Selby, 2012) hand-picked magnetic/heavy liquids/HF concentrate NTIMS Kerver 304 2 1 Porphyry Cu granodiorite 0.23 0.007 0 7.25 (Aghazadeh et al., 2015) hand-picked grains unknown Kerver 1490 19 1 Porphyry Cu granodiorite 0.23 0.007 0 7.25 (Aghazadeh et al., 2015) hand-picked grains unknown Keskin 50 1 Skarn Pb-Zn granitoid 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Kilkieran 54.11 0.14 1 Granite Mo granite 0 0 0 402.2 (Feely et al., 2010) magnetic concentrate NTIMS Kilkivan 22.6 1 Epithermal granite 0 0 0 0 (Riley, 1967) hand samples TIMS Kimberley 2.8 1 Quartz vein-hosted Au 0 0 0 0 2600 (Frei et al., 1998) hand-picked magnetic/heavy liquids concentrate TIMS Kimberley 2.8 1 Quartz vein-hosted Au 0 0 0 0 2600 (Frei et al., 1998) hand-picked magnetic/heavy liquids concentrate TIMS Kimberley 2.8 1 Quartz vein-hosted Au 0 0 0 0 2600 (Frei et al., 1998) hand-picked magnetic/heavy liquids concentrate TIMS Kimberley 2.9 1 Quartz vein-hosted Au 0 0 0 0 2600 (Frei et al., 1998) hand-picked magnetic/heavy liquids concentrate TIMS Kimmeria 100 1 Porphyry Mo-W granodiorite 0 0 0 0 (Voudouris et al., 2010) hand samples EPMA Kimmeria 134 47 10 550 Porphyry Mo-W granodiorite 0 0 0 0 (Voudouris et al., 2013) thin sections EPMA Kimmeria 73 1 Porphyry Mo-W granodiorite 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Kimmeria 28 1 Porphyry Mo-W granodiorite 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Kimmeria 39 1 Porphyry Mo-W granodiorite 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Kimmeria 17 1 Porphyry Mo-W granodiorite 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry King Island 46 1 Skarn W 0 0 0.025 0 342.8 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA King Island 47 Skarn W 0 0 0.025 0 342.8 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Kingsgate 0.25 1 Breccia pipe 0 0 0 0 0 (Riley, 1967) hand samples TIMS Kinpozan (Kimpuzan) 210 1 Quartz vein-hosted granodiorite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Kinpozan (Kimpuzan) 210 1 Quartz vein-hosted granodiorite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Kitsault 57 1 Porphyry Mo quartz monzonite 0.004 0.192 0 44.85 (Sinclair et al., 2009) various NAA Kitsault 102 1 Porphyry Mo quartz monzonite 0.004 0.192 0 44.85 (Sinclair et al., 2009) various NAA Kivisuo 114.4 1 Quartz vein-hosted Au tonalite 0 0 0 2803 (Stein et al., 1998) unknown NTIMS Kivisuo 119.1 1 Quartz vein-hosted Au tonalite 0 0 0 2803 (Stein et al., 1998) unknown NTIMS Kliphoog 11.46 0.01 1 Quartz vein-hosted W granite 0 0 0 1019 (Raith and Stein, 2000) hand-picked magnetic concentrate NTIMS Kliphoog 51.94 0.04 1 Quartz vein-hosted W granite 0 0 0 1019 (Raith and Stein, 2000) hand-picked magnetic concentrate NTIMS Knaben 1.4 1 Granite Mo 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Knaben 13.3 1 Granite Mo 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Knaben 28 1 Granite Mo 0 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Kobayashiyama 5 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Kobayashiyama 5.3 1 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Kobberknuten 686 1 Magmatic/basalt-hosted metamorphic deposit 0 0 0 0 1051 (Stein and Bingen, 2002) unknown NTIMS Kobberknuten 698 1 Magmatic/basalt-hosted metamorphic deposit 0 0 0 0 1051 (Stein and Bingen, 2002) unknown NTIMS Kobberknuten 791 1 Magmatic/basalt-hosted metamorphic deposit 0 0 0 0 1051 (Stein and Bingen, 2002) unknown NTIMS Kobberknuten 832 1 Magmatic/basalt-hosted metamorphic deposit 0 0 0 0 1051 (Stein and Bingen, 2002) unknown NTIMS Kobberknuten 958 1 Magmatic/basalt-hosted metamorphic deposit 0 0 0 0 1051 (Stein and Bingen, 2002) unknown NTIMS Kobberknuten 981 1 Magmatic/basalt-hosted metamorphic deposit 0 0 0 0 1051 (Stein and Bingen, 2002) unknown NTIMS Kokurobe 1.6 1 Quartz vein-hosted granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Kokurobe 17 1 Quartz vein-hosted granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Kokurobe 8.9 5 Quartz vein-hosted granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Komaki 6.213 0.015 1 Quartz vein-hosted Mo granite 0 0 0 73.9 (Suzuki et al., 1996) hand samples ID-ICP-MS Komaki 6.525 0.049 1 Quartz vein-hosted Mo granite 0 0 0 73.9 (Suzuki et al., 1996) hand samples ID-ICP-MS Komaki 10 1 Quartz vein-hosted Mo granite 0 0 0 73.9 (Terada et al., 1971) hand-picked grains NAA Komaki 12 1 Quartz vein-hosted Mo granite 0 0 0 73.9 (Terada et al., 1971) hand-picked grains NAA Komaki—Honko 9.7 1 Quartz vein-hosted Mo granite 0 0 0 73.9 (Terada et al., 1971) hand-picked grains NAA Komaki—Honko 20 1 Quartz vein-hosted Mo granite 0 0 0 73.9 (Terada et al., 1971) hand-picked grains NAA Komaki—Honko 15.1 6 Quartz vein-hosted Mo granite 0 0 0 73.9 (Ishihara, 1988) various NAA/spectrophotometry Komaki—Ichiman (Ichimanko) 21 1 Quartz vein-hosted Mo granite 0 0 0 73.9 (Terada et al., 1971) hand-picked grains NAA Komaki—Ichiman (Ichimanko) 29 1 Quartz vein-hosted Mo granite 0 0 0 73.9 (Terada et al., 1971) hand-picked grains NAA Komaki—Ichiman (Ichimanko) 26.7 3 Quartz vein-hosted Mo granite 0 0 0 73.9 (Ishihara, 1988) various NAA/spectrophotometry Komaki—Tenma 13 1 Quartz vein-hosted Mo granite 0 0 0 73.9 (Terada et al., 1971) hand-picked grains NAA Komaki—Tenma 15 1 Quartz vein-hosted Mo granite 0 0 0 73.9 (Terada et al., 1971) hand-picked grains NAA Komaki—Tenma 13.7 3 Quartz vein-hosted Mo granite 0 0 0 73.9 (Ishihara, 1988) various NAA/spectrophotometry Kongo-san 0.64 1 Quartz vein-hosted Mo 0 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Kongo-san 5 1 Quartz vein-hosted Mo 0 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Konkola West 5.291 0.014 5.291 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Konos 6500 1 Porphyry Cu-Mo dacite; diorite 0 0 0.04 0 (Voudouris et al., 2010) hand samples EPMA Konos 15621 7 750 31100 Porphyry Cu-Mo dacite; diorite 0 0 0.04 0 (Voudouris et al., 2013) thin sections EPMA Konos 25900 1 Porphyry Cu-Mo dacite; diorite 0 0 0.04 0 (Voudouris et al., 2010) hand samples EPMA Korongvale 9.2 1 Granite Au 0 0 0 0 0 (Riley, 1967) hand samples TIMS Kounrad 100 1 Porphyry Cu 0 0.6 0.01 0.756 329.5 (Fleischer, 1959) flotation concentrate unknown Kounrad 100 1 Porphyry Cu 0 0.6 0.01 0.756 329.5 (Fleischer, 1959) flotation concentrate unknown Kounrad 150 1 Porphyry Cu 0 0.6 0.01 0.756 329.5 (Fleischer, 1959) flotation concentrate unknown Kounrad 150 1 Porphyry Cu 0 0.6 0.01 0.756 329.5 (Fleischer, 1959) flotation concentrate unknown Kounrad 150 1 Porphyry Cu 0 0.6 0.01 0.756 329.5 (Fleischer, 1960) unknown colorimetry Kounrad 1540 20 620 4050 Porphyry Cu 0 0.6 0.01 0.756 329.5 (Berzina et al., 2005) various various Kowary 22 1 Granite Mo granite 0 0 0 313 (Mikulski and Stein, 2007) micro-drilled hand samples NTIMS Kozi Hora 0.486 0.002 1 Quartz vein-hosted 0 0 0 0 316 (Ackerman et al., 2017) hand-picked grains ICP-MS Kozi Hora 0.499 0.002 1 Quartz vein-hosted 0 0 0 0 316 (Ackerman et al., 2017) hand-picked grains ICP-MS Krasno 3.063 0.009 1 Greisen Sn-W granite 0 0 0 325 (Ackerman et al., 2017) hand-picked grains ICP-MS Krupka 9.82 0.020 1 Greisen Sn-W granite 0 0 0 323.5 (Ackerman et al., 2017) hand-picked grains ICP-MS Krupka 9.89 0.020 1 Greisen Sn-W granite 0 0 0 323.5 (Ackerman et al., 2017) hand-picked grains ICP-MS Krupka 0.385 0.001 1 Greisen Sn-W granite 0 0 0 323.5 (Ackerman et al., 2017) hand-picked grains ICP-MS Krupka 0.85 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.88 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.57 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.93 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.35 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.34 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.03 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.04 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.11 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.12 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.13 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.12 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 5.7 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.07 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.05 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.09 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.09 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 1.2 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.59 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.93 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.2 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.51 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.33 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.28 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.63 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.69 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.49 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.99 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.55 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Krupka 0.41 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Kucing Liar 98.41 1 Skarn Cu 0 1.124 0 1.074 2.54 (Mathur et al., 2005) hand-picked grains NTIMS Kucing Liar 98.91 1 Skarn Cu 0 1.124 0 1.074 2.54 (Mathur et al., 2005) hand-picked grains NTIMS Kuh Panj 1699 14 1 Porphyry Cu granodiorite; quartz diorite 0.2 0.001 0 9.17 (Aghazadeh et al., 2015) hand-picked grains unknown Kuittila 72.5 1 Intrusion-related Au tonalite 0 0.3 4 2794 (Stein et al., 1998) unknown NTIMS Kuittila 85 1 Intrusion-related Au tonalite 0 0.3 4 2794 (Stein et al., 1998) unknown NTIMS Kulitu 17.013 0.13 1 Porphyry Cu-Mo monzogranite 0 0 0 0 (Zhang et al., 2009) hand samples ICP-MS Kulitu 17.228 0.152 1 Porphyry Cu-Mo monzogranite 0 0 0 0 (Zhang et al., 2009) hand samples ICP-MS Kulitu 22.296 0.222 1 Porphyry Cu-Mo monzogranite 0 0 0 0 (Zhang et al., 2009) hand samples ICP-MS Kulitu 23.178 0.213 1 Porphyry Cu-Mo monzogranite 0 0 0 0 (Zhang et al., 2009) hand samples ICP-MS Kulitu 31.701 0.287 1 Porphyry Cu-Mo monzogranite 0 0 0 0 (Zhang et al., 2009) hand samples ICP-MS Kulitu 38.1 0.333 1 Porphyry Cu-Mo monzogranite 0 0 0 0 (Zhang et al., 2009) hand samples ICP-MS Kuridala 241 1 IOCG 0 0 0 0 0 (Riley, 1967) hand samples TIMS Kvinesdal 10.328 0.007 1 Granite Mo 0 0 0 0 959 (Bingen et al., 2006) micro-drilled hand samples NTIMS La Caridad 71.3 0.1 1 Porphyry Cu-Au quartz monzonite 0.452 0.025 0 53.8 (Barra et al., 2005) hand-picked grains NTIMS La Caridad 73.6 0.1 1 Porphyry Cu-Au quartz monzonite 0.452 0.025 0 53.8 (Barra et al., 2005) hand-picked grains NTIMS La Caridad 195.2 0.2 1 Porphyry Cu-Au quartz monzonite 0.452 0.025 0 53.8 (Barra et al., 2005) hand-picked grains NTIMS Lady Ella 187.1 5 1 IOCG granite 1.5 0 1.3 1490 (Duncan et al., 2011) micro-drilled hand samples NTIMS Lahnanen 5.1 1 Granodiorite Mo tonalite 0 0.14 0 1880 (Luck and Allègre, 1982) unknown ID-ion probe Lainejaur 2500 1 Unknown 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Lakange 476.7 21.600 Porphyry Cu-Mo granodiorite 0 0 0 13.12 (Leng et al., 2015) hand-picked flotation concentrate ICP-MS Lakange 810.7 15.100 Porphyry Cu-Mo granodiorite 0 0 0 13.12 (Leng et al., 2015) hand-picked flotation concentrate ICP-MS Lakange 676.2 7.600 Porphyry Cu-Mo granodiorite 0 0 0 13.12 (Leng et al., 2015) hand-picked flotation concentrate ICP-MS Lakange 343.6 3.500 Porphyry Cu-Mo granodiorite 0 0 0 13.12 (Leng et al., 2015) hand-picked flotation concentrate ICP-MS Lakange 837.5 9.400 Porphyry Cu-Mo granodiorite 0 0 0 13.12 (Leng et al., 2015) hand-picked flotation concentrate ICP-MS Lakange 409.9 3.400 Porphyry Cu-Mo granodiorite 0 0 0 13.12 (Leng et al., 2015) hand-picked flotation concentrate ICP-MS Lakange 402.4 4.000 Porphyry Cu-Mo granodiorite 0 0 0 13.12 (Leng et al., 2015) hand-picked flotation concentrate ICP-MS Lakange 505.7 7.600 Porphyry Cu-Mo granodiorite 0 0 0 13.12 (Leng et al., 2015) hand-picked flotation concentrate ICP-MS Lala 88 1 IOCG Cu-Au (Fe-Mo-Ag) 0 0.084 0 1 1086 (Chen and Zhou, 2012) hand-picked grains ICP-MS Lala 89.3 1 IOCG Cu-Au (Fe-Mo-Ag) 0 0.084 0 1 1086 (Chen and Zhou, 2012) hand-picked grains ICP-MS Lala 89.3 1 IOCG Cu-Au (Fe-Mo-Ag) 0 0.084 0 1 1086 (Chen and Zhou, 2012) hand-picked grains ICP-MS Lala 89.6 1 IOCG Cu-Au (Fe-Mo-Ag) 0 0.084 0 1 1086 (Chen and Zhou, 2012) hand-picked grains ICP-MS Lala 93.4 1 IOCG Cu-Au (Fe-Mo-Ag) 0 0.084 0 1 1086 (Chen and Zhou, 2012) hand-picked grains ICP-MS Lala 94.5 1 IOCG Cu-Au (Fe-Mo-Ag) 0 0.084 0 1 1086 (Chen and Zhou, 2012) hand-picked grains ICP-MS Lala 97.6 1 IOCG Cu-Au (Fe-Mo-Ag) 0 0.084 0 1 1086 (Chen and Zhou, 2012) hand-picked grains ICP-MS Langvatn 91 1 Magmatic/basalt-hosted metamorphic deposit gabbro 0 0 0 1041 (Bingen and Stein, 2002) hand samples NTIMS Langvatn 99 1 Magmatic/basalt-hosted metamorphic deposit gabbro 0 0 0 1041 (Bingen and Stein, 2002) hand samples NTIMS Langvatn 106 1 Magmatic/basalt-hosted metamorphic deposit gabbro 0 0 0 1041 (Bingen and Stein, 2002) hand samples NTIMS Langvatn 110 1 Magmatic/basalt-hosted metamorphic deposit gabbro 0 0 0 1041 (Bingen and Stein, 2002) hand samples NTIMS Langvatn 133 1 Magmatic/basalt-hosted metamorphic deposit gabbro 0 0 0 1041 (Bingen and Stein, 2002) hand samples NTIMS Langvatn 137 1 Magmatic/basalt-hosted metamorphic deposit gabbro 0 0 0 1041 (Golden et al., 2013) unknown unknown Lanjiagou 31.04 0.74 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Mao et al., 1999) various various Lanjiagou 33.29 0.37 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Han et al., 2009) hand samples ICP-MS Lanjiagou 33.8 0.3 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Mao et al., 1999) various various Lanjiagou 33.96 0.26 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Han et al., 2009) hand samples ICP-MS Lanjiagou 34.4 0.5 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Mao et al., 1999) various various Lanjiagou 35.05 0.31 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Han et al., 2009) hand samples ICP-MS Lanjiagou 35.59 0.36 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Han et al., 2009) hand samples ICP-MS Lanjiagou 35.83 0.29 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Han et al., 2009) hand samples ICP-MS Lanjiagou 36.07 0.33 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Han et al., 2009) hand samples ICP-MS Lanjiagou 36.25 0.39 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Han et al., 2009) hand samples ICP-MS Lanjiagou 37.49 0.34 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Han et al., 2009) hand samples ICP-MS Lanjiagou 40.53 0.36 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Han et al., 2009) hand samples ICP-MS Lanjiagou 44.74 0.57 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Mao et al., 1999) various various Lanjiagou 45.13 1.01 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Mao et al., 1999) various various Lanjiagou 45.83 0.41 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Han et al., 2009) hand samples ICP-MS Lanjiagou 47.85 0.5 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Han et al., 2009) hand samples ICP-MS Lanjiagou 53.1 1.2 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Mao et al., 1999) various various Lanjiagou 60.6 0.7 1 Quartz vein-hosted granite 0 0.13 0 190.5 (Mao et al., 1999) various various Larap 22 1 Porphyry Cu-Mo 0 0.35 0.05 0.4 33.653 (Terada et al., 1971) hand-picked grains NAA Lavrion 229 27 10 1310 Intrusion-related granodiorite 0 0 0 0 (Voudouris et al., 2013) thin sections EPMA Lavrion 600 1 Intrusion-related granodiorite 0 0 0 0 (Voudouris et al., 2010) hand samples EPMA Lavrion 1300 1 Intrusion-related granodiorite 0 0 0 0 (Voudouris et al., 2010) hand samples EPMA Leimengou 18.64 1 Porphyry Mo granite 0 0.07 0 130.45 (Mao et al., 2008) hand samples ICP-MS Leimengou 26.25 1 Porphyry Mo granite 0 0.07 0 130.45 (Mao et al., 2008) hand samples ICP-MS Lengshuigou 300.4 2.800 Porphyry Cu granodiorite 0.5875 0.023 0.395 147.8 (Xie et al., 2017) hand-picked grains ICP-MS Lengshuigou 198.9 1.800 Porphyry Cu granodiorite 0.5875 0.023 0.395 147.8 (Xie et al., 2017) hand-picked grains ICP-MS Lengshuigou 397.1 3.300 Porphyry Cu granodiorite 0.5875 0.023 0.395 147.8 (Xie et al., 2017) hand-picked grains ICP-MS Liikavaara 45.4 0.7 1 Porphyry Cu quartz monzodiorite 0.24 0.004 0.07 0 (Nigatu, 2011) micro-drilled hand samples ICP-MS Liikavaara 273.91 3.2 1 Porphyry Cu quartz monzodiorite 0.24 0.004 0.07 0 (Nigatu, 2011) micro-drilled hand samples ICP-MS Linka 38 1 Skarn W granite 0 0 0 153.35 (Giles and Schilling, 1972) hand samples colorimetry Lipovy Log 11.87 4 1 Pegmatite pegmatite 0 0 0 262 (Mao et al., 2003) hand samples ICP-MS Lipovy Log 12.42 8 1 Pegmatite pegmatite 0 0 0 262 (Mao et al., 2003) hand samples ICP-MS Lipovy Log 22.75 13 1 Pegmatite pegmatite 0 0 0 262 (Mao et al., 2003) hand samples ICP-MS Lipovy Log 23.76 20 1 Pegmatite pegmatite 0 0 0 262 (Mao et al., 2003) hand samples ICP-MS Lipovy Log 29.35 17 1 Pegmatite pegmatite 0 0 0 262 (Mao et al., 2003) hand samples ICP-MS Lir 2 1 Unknown 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Lishan 18.3 7 13.4 22.7 Porphyry Mo granodiorite 0 0.65 0 91.7 (Zhong et al., 2017) various various Liushan 2.01 0.2 1 Porphyry Mo diorite; granodiorite 0 0.24 0 288 (Han et al., 2014b) unknown ICP-MS Liushan 3.19 0.4 1 Porphyry Mo diorite; granodiorite 0 0.24 0 288 (Han et al., 2014b) unknown ICP-MS Liushan 4.54 0.4 1 Porphyry Mo diorite; granodiorite 0 0.24 0 288 (Han et al., 2014b) unknown ICP-MS Liushan 5.408 0.31 1 Porphyry Mo diorite; granodiorite 0 0.24 0 288 (Han et al., 2014b) unknown ICP-MS Liushan 9.16 0.9 1 Porphyry Mo diorite; granodiorite 0 0.24 0 288 (Han et al., 2014b) unknown ICP-MS Liushan 9.63 0.8 1 Porphyry Mo diorite; granodiorite 0 0.24 0 288 (Han et al., 2014b) unknown ICP-MS Liushan 10.12 0.7 1 Porphyry Mo diorite; granodiorite 0 0.24 0 288 (Han et al., 2014b) unknown ICP-MS Liushan 12.2 0.10 1 Porphyry Mo diorite; granodiorite 0 0.24 0 288 (Han et al., 2014b) unknown ICP-MS Lobash 23.47 1 Porphyry Cu-Mo 0 0.03 0.075 0 2692 (Stein et al., 2001b) unknown unknown Lobash 4.51 0.09 1 Porphyry Cu-Mo 0 0.03 0.075 0 2692 (Suzuki et al., 2000) unknown ID-ICP-MS Lobash 39.967 1 Porphyry Cu-Mo 0 0.03 0.075 0 2692 (Stein et al., 2001b) unknown unknown Lobash 7.13 0.05 1 Porphyry Cu-Mo 0 0.03 0.075 0 2692 (Suzuki et al., 2000) unknown ID-ICP-MS Lobash 22.147 1 Porphyry Cu-Mo 0 0.03 0.075 0 2692 (Stein et al., 2001b) unknown unknown Lobash 8.35 0.09 1 Porphyry Cu-Mo 0 0.03 0.075 0 2692 (Suzuki et al., 2000) unknown ID-ICP-MS Lobash 17.9 1 Porphyry Cu-Mo 0 0.03 0.075 0 2692 (Lavrov and Kuleshevich, 2010) unknown SEM Lobash 56.8 1 Porphyry Cu-Mo 0 0.03 0.075 0 2692 (Lavrov and Kuleshevich, 2010) unknown SEM Lofoten 509 1 Unknown 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Logtung 22 1 Porphyry Mo-W monzogranite 0 0.031 0 109 (Sinclair et al., 2009) various NAA Łomnica Górna 36 1 Granite Mo granite 0 0 0 327 (Mikulski and Stein, 2007) micro-drilled hand samples NTIMS Lorelei 400 300 1 Porphyry Cu-Mo 0 0 0 0 0 (McCandless et al., 1993) hand-picked grains EPMA Lornex 221 1 Porphyry Cu-Mo granitoid; granodiorite; quartz diorite 0.404 0.014 0.006 197 (Schindler, 1975) various NAA Lornex 227 1 Porphyry Cu-Mo granitoid; granodiorite; quartz diorite 0.404 0.014 0.006 197 (Schindler, 1975) various NAA Lornex 257 1 Porphyry Cu-Mo granitoid; granodiorite; quartz diorite 0.404 0.014 0.006 197 (Schindler, 1975) various NAA Lornex 345 1 Porphyry Cu-Mo granitoid; granodiorite; quartz diorite 0.404 0.014 0.006 197 (Sinclair et al., 2009) various NAA Los Pelambres 303.4 2 1 Porphyry Cu 0 0.63 0.016 0.016 11.516 (Markey et al., 2003) unknown NTIMS Los Pelambres 312.7 2 1 Porphyry Cu 0 0.63 0.016 0.016 11.516 (Markey et al., 2003) unknown NTIMS Los Pelambres 396 2 1 Porphyry Cu 0 0.63 0.016 0.016 11.516 (Markey et al., 2003) unknown NTIMS Los Pelambres 473 1 Porphyry Cu 0 0.63 0.016 0.016 11.516 (Mathur et al., 2010) hand-picked grains NTIMS Los Pelambres 600 3 450 820 Porphyry Cu 0 0.63 0.016 0.016 11.516 (Berzina et al., 2005) various various Los Pelambres 819 1 Porphyry Cu 0 0.63 0.016 0.016 11.516 (Mathur et al., 2000) hand-picked grains NTIMS Los Pelambres 835 1 Porphyry Cu 0 0.63 0.016 0.016 11.516 (Mathur et al., 2000) hand-picked grains NTIMS Lucky Ship 41 1 Porphyry Mo rhyolite 0 0.095 0 44.85 (Sinclair et al., 2009) various NAA Lufubu South 80.57 0.250 70.5535516 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Lufubu South 95.03 0.300 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Lufubu South 14.02 0.04 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Lufubu South 177.6 0.6 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Lufubu South 91.7 0.3 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Luming 37.28 1 Porphyry Mo monzogranite 0.084 177.9 (Hu et al., 2014) hand samples ICP-MS Luming 61.76 1 Porphyry Mo monzogranite 0.084 177.9 (Hu et al., 2014) hand samples ICP-MS Luming 30.2 1 Porphyry Mo monzogranite 0.084 177.9 (Hu et al., 2014) hand samples ICP-MS Luming 34.7 1 Porphyry Mo monzogranite 0.084 177.9 (Hu et al., 2014) hand samples ICP-MS Luming 21 1 Porphyry Mo monzogranite 0.084 177.9 (Hu et al., 2014) hand samples ICP-MS Luming 39.69 1 Porphyry Mo monzogranite 0.084 177.9 (Hu et al., 2014) hand samples ICP-MS Luming 38.4 1 Porphyry Mo monzogranite 0.084 177.9 (Hu et al., 2014) hand samples ICP-MS Luoboling 122 1.000 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Li and Jiang, 2017) unknown ICP-MS Luoboling 226 1.800 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Zhong et al., 2014) concentrate, unknown method unknown Luoboling 78.6 0.600 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Zhong et al., 2014) concentrate, unknown method unknown Luoboling 213 1.600 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Zhong et al., 2014) concentrate, unknown method unknown Luoboling 278 2.100 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Zhong et al., 2014) concentrate, unknown method unknown Luoboling 202 1.600 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Zhong et al., 2014) concentrate, unknown method unknown Luoboling 451 4.100 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Zhong et al., 2014) concentrate, unknown method unknown Luoboling 237 2.000 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Li and Jiang, 2017) unknown unknown Luoboling 200 2.000 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Li and Jiang, 2017) unknown unknown Luoboling 169 2.000 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Li and Jiang, 2017) unknown unknown Luoboling 223 2.000 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Li and Jiang, 2017) unknown unknown Luoboling 177 1.000 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Li and Jiang, 2017) unknown unknown Luoboling 147 1.000 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Li and Jiang, 2017) unknown unknown Luoboling 193 2.000 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Li and Jiang, 2017) unknown unknown Luoboling 117 1.000 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Li and Jiang, 2017) unknown unknown Luoboling 172 2.000 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Li and Jiang, 2017) unknown unknown Luoboling 156 1.000 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Li and Jiang, 2017) unknown unknown Luoboling 112 1.000 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Li and Jiang, 2017) unknown unknown Luoboling 173 11 112 237 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Zhong et al., 2017) various various Luoboling 241 6 78 450 Porphyry Cu-Mo granodiorite 0 0 0 105.3 (Zhong et al., 2017) various various Luokuidong 28.392 0.297 Porphyry Mo quartz syenite, granite 0 0.05 0 99.85 (Xu et al., 2016) unknown unknown Luokuidong 30.81 0.073 Porphyry Mo quartz syenite, granite 0 0.05 0 99.85 (Xu et al., 2016) unknown unknown Luokuidong 31.536 0.251 Porphyry Mo quartz syenite, granite 0 0.05 0 99.85 (Xu et al., 2016) unknown unknown Mace Head 75.74 0.36 1 Granite Mo granite 0 0 0 0 (Selby et al., 2004) concentrate, unknown method NTIMS Mace Head 75.92 0.27 1 Granite Mo granite 0 0 0 0 (Selby et al., 2004) concentrate, unknown method NTIMS Mace Head 76.14 0.36 1 Granite Mo granite 0 0 0 0 (Suzuki et al., 2001) hand-picked grains ID-ICP-MS Machangqing 30.5 1 Porphyry Cu-Mo granite; monzonite; porphyry 0.5 0.078 0.35 35.8 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Machangqing 33.6 1 Porphyry Cu-Mo granite; monzonite; porphyry 0.5 0.078 0.35 35.8 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Machangqing 66 1 Porphyry Cu-Mo granite; monzonite; porphyry 0.5 0.078 0.35 35.8 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Machangqing 84.5 1 Porphyry Cu-Mo granite; monzonite; porphyry 0.5 0.078 0.35 35.8 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Machangqing 84.7 1 Porphyry Cu-Mo granite; monzonite; porphyry 0.5 0.078 0.35 35.8 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Machangqing 89.6 1 Porphyry Cu-Mo granite; monzonite; porphyry 0.5 0.078 0.35 35.8 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Machangqing 123.3 1 Porphyry Cu-Mo granite; monzonite; porphyry 0.5 0.078 0.35 35.8 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Machangqing 125.1 1 Porphyry Cu-Mo granite; monzonite; porphyry 0.5 0.078 0.35 35.8 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Macksville 63 1 Granite Cu 0 0 0 0 0 (Riley, 1967) hand samples TIMS Mactung 4.61 0.013 1 Skarn W 0 0 0 0 97.25 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Mactung 4.678 0.015 1 Skarn W 0 0 0 0 97.25 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Mactung 11.64 0.05 1 Skarn W 0 0 0 0 97.25 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Mactung 12.48 0.04 1 Skarn W 0 0 0 0 97.25 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Mactung 16.51 0.16 1 Skarn W 0 0 0 0 97.25 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Mactung 19.2 0.3 1 Skarn W 0 0 0 0 97.25 (Selby et al., 2003) hand-picked magnetic/heavy liquids concentrate NTIMS Maggie 643 1 Porphyry Cu-Mo latite; quartz diorite; quartz monzonite 0.28 0.028 0 63 (Sinclair et al., 2009) various NAA Majdanpek 44.61 0.01 1 Porphyry, skarn Cu diorite; granodiorite 0.6 0.006 0.3 83.57 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Majdanpek 44.7 0.1 1 Porphyry, skarn Cu diorite; granodiorite 0.6 0.006 0.3 83.57 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Majdanpek 124 0.1 1 Porphyry, skarn Cu diorite; granodiorite 0.6 0.006 0.3 83.57 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Majdanpek 608.7 0.4 1 Porphyry, skarn Cu diorite; granodiorite 0.6 0.006 0.3 83.57 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Majdanpek 931 1 1 Porphyry, skarn Cu diorite; granodiorite 0.6 0.006 0.3 83.57 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Majdanpek 943 1 1 Porphyry, skarn Cu diorite; granodiorite 0.6 0.006 0.3 83.57 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Majdanpek 2770 3 2320 3550 Porphyry, skarn Cu diorite; granodiorite 0.6 0.006 0.3 83.57 (Berzina et al., 2005) various various Makari 0.23 1 Quartz vein-hosted granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Makari 0.2 Quartz vein-hosted granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Malanjkhand 138.96 0.08 1 Porphyry Cu 0 0.83 0.003 0.2 2490 (Stein et al., 2006) unknown unknown Malanjkhand 196.6 0.1 1 Porphyry Cu 0 0.83 0.003 0.2 2490 (Stein et al., 2006) unknown unknown Malanjkhand 314.9 0.3 1 Porphyry Cu 0 0.83 0.003 0.2 2490 (Stein et al., 2006) unknown unknown Malanjkhand 346.8 0.2 1 Porphyry Cu 0 0.83 0.003 0.2 2490 (Stein et al., 2006) unknown unknown Malanjkhand 432 1 Porphyry Cu 0 0.83 0.003 0.2 2490 (Stein et al., 2004) unknown unknown Malanjkhand 458 1 Porphyry Cu 0 0.83 0.003 0.2 2490 (Stein et al., 2004) unknown unknown Malanjkhand 477 1 Porphyry Cu 0 0.83 0.003 0.2 2490 (Stein et al., 2004) unknown unknown Malanjkhand 482 1 Porphyry Cu 0 0.83 0.003 0.2 2490 (Stein et al., 2004) unknown unknown Malanjkhand 490 1 Porphyry Cu 0 0.83 0.003 0.2 2490 (Stein et al., 2004) unknown unknown Malanjkhand 513 1 Porphyry Cu 0 0.83 0.003 0.2 2490 (Stein et al., 2004) unknown unknown Malanjkhand 543 1 Porphyry Cu 0 0.83 0.003 0.2 2490 (Golden et al., 2013) unknown unknown Malanjkhand 546 1 Porphyry Cu 0 0.83 0.003 0.2 2490 (Stein et al., 2004) unknown unknown Malanjkhand 623 1 Porphyry Cu 0 0.83 0.003 0.2 2490 (Stein et al., 2004) unknown unknown Maldon 85 1 Quartz vein-hosted Au granite 0 0 0 378 (Arne et al., 2001) hand-picked grains NTIMS Malmbjerg 6.086 0.003 1 Porphyry Mo 0 0 0.12 0 25.8 (Brooks et al., 2004) hand-picked grains NTIMS Malpica 98 0.1 1 Porphyry Cu granodiorite 0.5 0 0.4 54.1 (Barra et al., 2005) hand-picked grains NTIMS Manganese 0 1 Unknown 0 0 0 0 0 (Hiskey and Meloche, 1940) unknown colorimetry Maoping 0.03717 0.00034 1 Greisen W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Maoping 0.06241 0.00052 1 Greisen W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Maoping 0.07968 0.00058 1 Greisen W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Maoping 0.08293 0.00065 1 Greisen W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Maoping 0.08976 0.00088 1 Greisen W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Maoping 0.09331 0.00076 1 Greisen W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Maoping 0.1 0.0008 1 Greisen W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Maoping 0.1073 0.001 1 Greisen W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Maoping 0.1074 0.001 1 Greisen W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Maoping 0.1089 0.0009 1 Greisen W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Maoping 0.1663 0.0013 1 Greisen W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Maoping 0.2144 0.0021 1 Greisen W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Maria 0.1 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 5.47 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 8.06 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 15.87 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 16.93 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 18.26 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 20.37 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 23.33 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 24.48 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 26.09 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 28.28 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 28.62 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 29.8 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 30 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 30.57 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 46.62 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 46.86 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 49.1 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 51.61 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 56.71 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 60.98 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 61.2 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 63.82 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 64.19 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 64.79 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 66.81 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 70.71 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 73.62 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 76.97 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 77.05 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 77.72 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 82.14 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 83.27 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 87.52 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 96.47 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 98.72 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 100 100 1 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (McCandless et al., 1993) hand-picked grains EPMA Maria 104.37 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 107.02 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 113.37 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 114.17 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 116.01 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 121.16 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 126.17 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 127.09 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 134.33 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 137.11 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 137.74 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 157.34 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 160.08 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 164.16 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 173.63 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 179.18 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 199.68 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 200 100 1 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (McCandless et al., 1993) hand-picked grains EPMA Maria 205.25 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 230.73 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 232.79 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 240.01 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 245.04 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 333.12 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 342.88 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 351.74 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 316.9 0.4 1 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Barra et al., 2005) hand-picked grains NTIMS Maria 396 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 400 500 1 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (McCandless et al., 1993) hand-picked grains EPMA Maria 413.8 1 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (McCandless and Ruiz, 1993) unknown unknown Maria 445.85 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 473.62 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 487.66 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 600 1000 1 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (McCandless et al., 1993) hand-picked grains EPMA Maria 532.99 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 586.21 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 683.67 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maria 1112.14 Porphyry Cu-Mo quartz monzonite; granite 0.33 0.36 0 60.4 (Rathkopf, 2015) polished mounts EPMA Maronia 3100 1 Porphyry Cu-Mo granite; granodiorite; quartz monzodiorite 0.37 0.01 0.1 29 (Voudouris et al., 2010) hand samples EPMA Maronia 7260 58 900 28800 Porphyry Cu-Mo granite; granodiorite; quartz monzodiorite 0.37 0.01 0.1 29 (Berzina et al., 2005) various various Maronia 14200 1 Porphyry Cu-Mo granite; granodiorite; quartz monzodiorite 0.37 0.01 0.1 29 (Voudouris et al., 2010) hand samples EPMA Masjed Daghi 0.527 0.05 1 Porphyry Cu-Au monzodiorite 0.27 0.006 0.32 20.46 (Aghazadeh et al., 2015) hand-picked grains unknown Matasvaara 23.6 0.1 1 Greisen Mo-W anorthosite 0 0 0 2600 (Suzuki et al., 2000) unknown ID-ICP-MS Matasvaara 24 0.2 1 Greisen Mo-W anorthosite 0 0 0 2600 (Suzuki et al., 1993) hand samples ID-ICP-MS Matasvaara 24.5 0.1 1 Greisen Mo-W anorthosite 0 0 0 2600 (Suzuki et al., 2000) unknown ID-ICP-MS Matasvaara 24.8 0.2 1 Greisen Mo-W anorthosite 0 0 0 2600 (Suzuki et al., 2000) unknown ID-ICP-MS Matasvaara 25.1 0.2 1 Greisen Mo-W anorthosite 0 0 0 2600 (Suzuki et al., 1993) hand samples ID-ICP-MS Matasvaara 26.6 0.1 1 Greisen Mo-W anorthosite 0 0 0 2600 (Suzuki et al., 1993) hand samples ID-ICP-MS Matasvaara 27 0.2 1 Greisen Mo-W anorthosite 0 0 0 2600 (Suzuki et al., 1993) hand samples ID-ICP-MS Matasvaara 29.6 1 Greisen Mo-W anorthosite 0 0 0 2600 (Luck and Allègre, 1982) unknown ID-ion probe Matou 129.2 13 69 231.8 Porphyry Cu-Mo granodiorite 0.65 0.052 0 148 (Zhong et al., 2017) various various McGill 1030 1 Quartz vein-hosted granite 0.85 0.016 0 771 (Fleischer, 1959) flotation concentrate unknown Medet 516.3 0.1 1 Porphyry Cu-Au granodiorite 0.37 0.01 0.1 90.83 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Medet 553 0.6 1 Porphyry Cu-Au granodiorite 0.37 0.01 0.1 90.83 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Medet 827.5 0.1 1 Porphyry Cu-Au granodiorite 0.37 0.01 0.1 90.83 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Medet 905 22 565 1163 Porphyry Cu-Au granodiorite 0.37 0.01 0.1 90.83 (Berzina et al., 2005) various various Medet 1162 1 1 Porphyry Cu-Au granodiorite 0.37 0.01 0.1 90.83 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Meiling 9.159 0.070 Porphyry Cu-Mo granodiorite 0.53 0.1 0 104.5 (Xu et al., 2016) unknown unknown Meiling 25.85 0.280 Porphyry Cu-Mo granodiorite 0.53 0.1 0 104.5 (Xu et al., 2016) unknown unknown Melitena 3900 1 Porphyry Cu-Mo dacite 0.04 0.6 0.16 63.5 (Voudouris et al., 2010) hand samples EPMA Melitena 7850 51 2100 17400 Porphyry Cu-Mo dacite 0.04 0.6 0.16 63.5 (Berzina et al., 2005) various various Melitena 16500 1 Porphyry Cu-Mo dacite 0.04 0.6 0.16 63.5 (Voudouris et al., 2010) hand samples EPMA Merlin 34.963 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 59.936 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 64.931 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 119.873 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 299.681 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 402.772 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 499.259 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 546.919 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 572.724 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 594.368 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 494.42 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 615.346 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 629.331 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 661.44 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 696.751 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 713.119 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 713.242 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 725.822 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 761.323 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 763.285 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 772.246 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 783.48 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 801.648 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 809.14 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 812.294 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 816.632 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 830.367 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 850.708 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 855.281 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 863.582 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 911.781 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 916.085 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 942.254 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 950.018 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 951.488 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 966.559 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 971.665 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 998.938 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1005.887 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1007.817 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1013.116 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1029.251 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1061.89 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1073.404 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1093.837 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1138.789 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1144.665 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1146.15 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1149.366 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1164.624 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1176.249 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1178.747 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1192.304 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1198.726 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1207.015 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1209.191 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1282.546 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1304.328 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1315.002 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1317 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1407.075 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1408.503 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1410.643 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1428.685 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1490.044 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1507.397 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1514.64 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1527.376 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1536.7 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 1539.164 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 2425.421 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 2432.414 1 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Goss, 2009) drill core whole-rock analysis with all Re and Mo assumed to be in molybdenite Merlin 915.5 2.400 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 906.1 2.300 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 1010.5 2.600 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 627.3 1.600 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 496.6 1.300 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 622.9 1.600 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 1001.8 2.600 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 1107.3 2.800 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 50.1 0.100 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 122.2 0.300 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 561.6 0.090 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 493.2 0.200 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 640 0.600 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 1001.1 0.800 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 643.4 0.800 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 107.3 0.300 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Merlin 375.4 0.600 IOCG Re-Mo-Cu (Ag) 0 0.2 0.6 0 1536 (Babo et al., 2017) magnetic concentrate NTIMS Metchagoja 6.1 1 Porphyry Cu-Mo 0 0 0 0 0 (Lavrov and Kuleshevich, 2010) unknown SEM Miami 150 1 Porphyry Cu 0 0.63 0.01 0.009 61.7 (Fleischer, 1959) flotation concentrate unknown Miami 152 1 Porphyry Cu 0 0.63 0.01 0.009 61.7 (Fleischer, 1959) flotation concentrate unknown Miami 297 1 Porphyry Cu 0 0.63 0.01 0.009 61.7 (Fleischer, 1959) flotation concentrate unknown Miami 688 1 Porphyry Cu 0 0.63 0.01 0.009 61.7 (Fleischer, 1959) flotation concentrate unknown Michałowice 8.5 1 Granite Mo granite 0 0 0 316 (Mikulski and Stein, 2007) micro-drilled hand samples NTIMS Michiquillay (Cajamarca) 494 8 127 736 Porphyry Cu 0 0.72 0.022 0.16 20.02 (Voudouris et al., 2013) thin sections EPMA Middlesex 1.7 1 Quartz vein-hosted W-Sn 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Middlesex 1.8 Quartz vein-hosted W-Sn 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Mikheev 100 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 200 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 200 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 200 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 200 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 300 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 600 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 600 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 600 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 700 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 700 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 700 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 1100 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 1100 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 1300 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 1400 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 1500 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 2000 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 2000 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 2000 1 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Grabezhev and Shagalov, 2010) hand samples EPMA Mikheev 400 1.000 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Tessalina and Plotinskaya, 2017) hand-picked grains ID-TIMS Mikheev 758.9 1.800 Porphyry Cu-Mo granodiorite; quartz diorite 0.9 0.005 0 357 (Tessalina and Plotinskaya, 2017) hand-picked grains ID-TIMS Milpillas 6547 1 Porphyry Cu 0 0.85 0 0 63 (Valencia et al., 2006) concentrate, unknown method NTIMS Milpillas 8785 1 Porphyry Cu 0 0.85 0 0 63 (Valencia et al., 2006) concentrate, unknown method NTIMS Minami Ikuchi 0.04 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Minami Ikuchi 1 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Minami Ikuchi 0.6 2 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Mineral Park 100 100 1 Porphyry Cu-Mo rhyolite 0.458 0.032 0.027 73.3 (McCandless et al., 1993) hand-picked grains EPMA Mineral Park 200 200 1 Porphyry Cu-Mo rhyolite 0.458 0.032 0.027 73.3 (McCandless et al., 1993) hand-picked grains EPMA Mission 400 100 1 Porphyry Cu-Au quartz monzonite 0.67 0.015 0 58 (McCandless et al., 1993) hand-picked grains EPMA Mission 427.1 1 Porphyry Cu-Au quartz monzonite 0.67 0.015 0 58 (McCandless and Ruiz, 1993) unknown unknown Mitchell 7012 1 Porphyry Cu-Au diorite; monzonite 0.2 0.005 0.64 196 (Sinclair et al., 2009) various NAA Mitchell 8170 1 Porphyry Cu-Au diorite; monzonite 0.2 0.005 0.64 196 (Sinclair et al., 2009) various NAA Moina 0.1 1 Quartz vein-hosted W-Sn 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Moina 0.11 Quartz vein-hosted W-Sn 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Mokrsko 60.24 0.130 1 Intrusion-related granodiorite 0 0 0 351.5 (Ackerman et al., 2017) hand-picked grains ICP-MS Mokrsko 61.76 0.140 1 Intrusion-related granodiorite 0 0 0 351.5 (Ackerman et al., 2017) hand-picked grains ICP-MS Mokrsko 85 Intrusion-related granodiorite 0 0 0 351.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Mokrsko 39 Intrusion-related granodiorite 0 0 0 351.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Mokrsko 19 Intrusion-related granodiorite 0 0 0 351.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Mokrsko 65 Intrusion-related granodiorite 0 0 0 351.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Mokrsko 18 Intrusion-related granodiorite 0 0 0 351.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Mokrsko 37 Intrusion-related granodiorite 0 0 0 351.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Mokrsko 41 Intrusion-related granodiorite 0 0 0 351.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Mokrsko 67 Intrusion-related granodiorite 0 0 0 351.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Mokrsko 7 Intrusion-related granodiorite 0 0 0 351.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Mokrsko 16 Intrusion-related granodiorite 0 0 0 351.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Mokrsko 70 Intrusion-related granodiorite 0 0 0 351.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Mokrsko 64 Intrusion-related granodiorite 0 0 0 351.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Moldava 27 Granite Mo granite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Moldava 36 Granite Mo granite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Moldava 17 Granite Mo granite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Moldova Nouă 158 0.2 1 Porphyry Cu 0 0.35 0 0 72.53 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Moldova Nouă 340.2 0.4 1 Porphyry Cu 0 0.35 0 0 72.53 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Moldova Nouă 531.7 0.6 1 Porphyry Cu 0 0.35 0 0 72.53 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Moldova Nouă 1326 3 1 Porphyry Cu 0 0.35 0 0 72.53 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Molibdeno 12.5 1 unknown 0 0 0 0 0 (Hiskey and Meloche, 1940) unknown colorimetry Molybdenum Corp of Canada 24.4 1 Porphyry Mo 0 0 0 0 0 (Schindler, 1975) various NAA Montezuma 0.51 1 Unknown 0 0 0 0 60 (Luck and Allègre, 1982) unknown ID-ion probe Moonta 1.33 1 IOCG 0 0 0 0 0 (Riley, 1967) hand samples TIMS Moonta 1.49 1 IOCG 0 0 0 0 0 (Riley, 1967) hand samples TIMS Moos 0.6 1 Unknown 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Morenci 100 100 1 Porphyry Cu porphyry; quartz monzonite; granite 0.524 0.01 0.028 56.6 (McCandless et al., 1993) hand-picked grains EPMA Morenci 300 0 1 Porphyry Cu porphyry; quartz monzonite; granite 0.524 0.01 0.028 56.6 (McCandless et al., 1993) hand-picked grains EPMA Morenci 600 500 1 Porphyry Cu porphyry; quartz monzonite; granite 0.524 0.01 0.028 56.6 (McCandless et al., 1993) hand-picked grains EPMA Morenci 800 500 1 Porphyry Cu porphyry; quartz monzonite; granite 0.524 0.01 0.028 56.6 (McCandless et al., 1993) hand-picked grains EPMA Morenci 2042 1 Porphyry Cu porphyry; quartz monzonite; granite 0.524 0.01 0.028 56.6 (McCandless and Ruiz, 1993) unknown unknown Morenci 4100 3800 1 Porphyry Cu porphyry; quartz monzonite; granite 0.524 0.01 0.028 56.6 (McCandless et al., 1993) hand-picked grains EPMA Moss 8.26 1 Pegmatite Mo diorite; monzonite 0.12 0 1.6 183 (Lentz et al., 2005) unknown unknown Mount Antero 20 1 Porphyry Mo 0 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Mount Bischoff 7.1 1 Skarn W granite 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Mount Dore 493.2 2 1 IOCG Cu (Au) granite 0.66 0 0.07 1502 (Duncan et al., 2011) micro-drilled hand samples NTIMS Mount Dore 561.6 9 1 IOCG Cu (Au) granite 0.66 0 0.07 1502 (Duncan et al., 2011) micro-drilled hand samples NTIMS Mount Dore 640 6 1 IOCG Cu (Au) granite 0.66 0 0.07 1502 (Duncan et al., 2011) micro-drilled hand samples NTIMS Mount Dore 1001.1 8 1 IOCG Cu (Au) granite 0.66 0 0.07 1502 (Duncan et al., 2011) micro-drilled hand samples NTIMS Mount Elliot 283.9 5 1 IOCG Cu-Au (Fe) granite 1.1 0 0.6 1515 (Duncan et al., 2011) micro-drilled hand samples NTIMS Mount Haskin 108 1 Porphyry Mo 0 0 0.09 0 0 (Sinclair et al., 2009) various NAA Mount Korong 7.2 1 Unknown Au 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Mount Lyell 7.3 1 VMS 0 1.3 0 0.49 515.15 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Mount Lyell 7.4 VMS 0 1.3 0 0.49 515.15 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Mount Merapi 91000 1 Volcanic sublimate andesite 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount Merapi 29000 1 Volcanic sublimate andesite 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount Merapi 93000 1 Volcanic sublimate andesite 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount Merapi 43000 1 Volcanic sublimate andesite 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount Merapi 115000 1 Volcanic sublimate andesite 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount Merapi 38000 1 Volcanic sublimate andesite 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount Moliagul 6.87 1 Granodiorite Mo granite; granodiorite 0 0 0 0 (Luck and Allègre, 1982) unknown ID-ion probe Mount Moliagul 15.9 1 Granodiorite Mo granite; granodiorite 0 0 0 0 (Riley, 1967) hand samples TIMS Mount Momotombo 72000 1 Volcanic sublimate andesite 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount Momotombo 65000 1 Volcanic sublimate andesite 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount Momotombo 63000 1 Volcanic sublimate andesite 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount Momotombo 78000 1 Volcanic sublimate andesite 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount Momotombo 72000 1 Volcanic sublimate andesite 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount Momotombo 70000 1 Volcanic sublimate andesite 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount Morgan 1690 1 VMS 0 0.7 0 4.7 387.6 (Riley, 1967) hand samples TIMS Mount Mulat 70 1 Granite Mo granite 0 0 0 0 (Paganelli, 1963) unknown colorimetry Mount Mulgine 10.7 1 Granite W syenogranite 0 0.039 0 2790 (Riley, 1967) hand samples TIMS Mount Mulgine 11.9 0.5 1 Granite W syenogranite 0 0.039 0 2790 (Suzuki et al., 1993) hand samples ID-ICP-MS Mount Mulgine 14 1 Granite W syenogranite 0 0.039 0 2790 (Luck and Allègre, 1982) unknown ID-ion probe Mount Mulgine 14.1 0.1 1 Granite W syenogranite 0 0.039 0 2790 (Suzuki et al., 1993) hand samples ID-ICP-MS Mount Mulgine 14.9 1 Granite W syenogranite 0 0.039 0 2790 (Riley, 1967) hand samples TIMS Mount Mulgine 15.6 1 Granite W syenogranite 0 0.039 0 2790 (Riley, 1967) hand samples TIMS Mount Mulgine 15.8 1 Granite W syenogranite 0 0.039 0 2790 (Riley, 1967) hand samples TIMS Mount Nansen 36.91 0.83 1 Intrusion-related Au 0 0 0 11.78 52.5 (Selby and Creaser, 2001a) hand-picked magnetic/heavy liquids concentrate NTIMS Mount Perry 81 1 Granite Mo 0 0 0 0 0 (Riley, 1967) hand samples TIMS Mount Pleasant 60 1 Porphyry W-Sn 0 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Mount St. Helens 37000 1 Volcanic sublimate 0 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount St. Helens 30000 1 Volcanic sublimate 0 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount St. Helens 48000 1 Volcanic sublimate 0 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount St. Helens 30000 1 Volcanic sublimate 0 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount St. Helens 30000 1 Volcanic sublimate 0 0 0 0 0.0000505 (Bernard et al., 1990) hand samples EPMA Mount St. Helens 25000 1 Volcanic sublimate 0 0 0 0 0.0000505 (Bernard et al., 1990) condensate EPMA Mount St. Helens 31000 1 Volcanic sublimate 0 0 0 0 0.0000505 (Bernard et al., 1990) condensate EPMA Mount St. Helens 22000 1 Volcanic sublimate 0 0 0 0 0.0000505 (Bernard et al., 1990) condensate EPMA Mount St. Helens 28000 1 Volcanic sublimate 0 0 0 0 0.0000505 (Bernard et al., 1990) condensate EPMA Mount St. Helens 21000 1 Volcanic sublimate 0 0 0 0 0.0000505 (Bernard et al., 1990) condensate EPMA Mount St. Helens 25000 1 Volcanic sublimate 0 0 0 0 0.0000505 (Bernard et al., 1990) condensate EPMA Mount Stanley 19.8 1 Quartz vein-hosted 0 0 0 0 0 (Riley, 1967) hand samples TIMS Mount Washington 608 1 Porphyry Cu 0 1.07 0 3.84 0 (Sinclair et al., 2009) various NAA Mount Washington 1524 1 Porphyry Cu 0 1.07 0 3.84 0 (Sinclair et al., 2009) various NAA Mufulira 385.6 0.9 385.6 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Mujimbeji 516.7 1.3 260.195247 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Mujimbeji 182.9 0.5 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Mujimbeji 186.4 0.5 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Munka 1.315 0.001 1 Granite Mo granite 0 0.125 0 1764.5 (Stein, 2006) hand samples NTIMS Munka 1.383 0.002 1 Granite Mo granite 0 0.125 0 1764.5 (Stein, 2006) hand samples NTIMS Munka 1.977 0.002 1 Granite Mo granite 0 0.125 0 1764.5 (Stein, 2006) hand samples NTIMS Munka 2.029 0.004 1 Granite Mo granite 0 0.125 0 1764.5 (Stein, 2006) hand samples NTIMS Munka 3.676 0.001 1 Granite Mo granite 0 0.125 0 1764.5 (Stein, 2006) hand samples NTIMS Munka 4.06 0.001 1 Granite Mo granite 0 0.125 0 1764.5 (Stein, 2006) hand samples NTIMS Muratdere 198 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 460 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 251 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 704 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 557 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 243 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 184 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 230 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 72 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 236 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 213 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 233 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 257 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 606 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 319 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 716 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 140 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 179 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Muratdere 711 Porphyry Cu-Mo granodiorite 0 0 0 0 (McFall, 2016) hand samples EPMA Murvey 5.09 0.01 1 Granite Mo granite 0 0 0 0 (Selby et al., 2004) concentrate, unknown method NTIMS Murvey 5.14 0.01 1 Granite Mo granite 0 0 0 0 (Selby et al., 2004) concentrate, unknown method NTIMS Murvey 9.492 0.042 1 Granite Mo granite 0 0 0 0 (Suzuki et al., 2001) hand-picked grains ID-ICP-MS Murvey 10.95 0.084 1 Granite Mo granite 0 0 0 0 (Suzuki et al., 2001) hand-picked grains ID-ICP-MS Murvey 15.2 0.4 1 Granite Mo granite 0 0 0 0 (Suzuki et al., 2001) hand-picked grains ID-ICP-MS Myli 400 1 Porphyry Cu-Mo dacite 0 0 0.09 0 (Voudouris et al., 2010) hand samples EPMA Myli 2733 32 440 19200 Porphyry Cu-Mo dacite 0 0 0.09 0 (Voudouris et al., 2013) thin sections EPMA Myli 3300 1 Porphyry Cu-Mo dacite 0 0 0.09 0 (Voudouris et al., 2010) hand samples EPMA Nababeep Far West 1.698 0.001 1 Quartz vein-hosted W granite 0 0 0 1019 (Raith and Stein, 2000) hand-picked magnetic concentrate NTIMS Nakatatsu 25 1 Skarn Pb-Zn granitoid 0.3 0 0 0 (Terada et al., 1971) hand-picked grains NAA Nakatatsu 34 1 Skarn Pb-Zn granitoid 0.3 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Nambucca 46 1 Granite Mo granite 0 0 0 0 (Riley, 1967) hand samples TIMS Nambucca 47 1 Granite Mo granite 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Nambucca 46 Granite Mo granite 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Nannihu 22.3 0.4 1 Porphyry Mo-W granite 0 0 0 155 (Mao et al., 1999) various various Nannihu 25.33 1 Porphyry Mo-W granite 0 0 0 155 (Mao et al., 2008) hand samples ICP-MS Nannihu 34.27 0.48 1 Porphyry Mo-W granite 0 0 0 155 (Mao et al., 1999) various various Nannihu 36.68 0.92 1 Porphyry Mo-W granite 0 0 0 155 (Mao et al., 1999) various various Nannihu 53.7 1 1 Porphyry Mo-W granite 0 0 0 155 (Mao et al., 1999) various various Nannihu 131.1 0.1 1 Porphyry Mo-W granite 0 0 0 155 (Huang et al., 1994) hand samples ID-ICP-MS Nanyangshan 29.41 0.27 1 Skarn Cu-Mo granodiorite 0 0 0 139.1 (Mao et al., 2006) hand samples ICP-MS Nanyangshan 29.45 0.15 1 Skarn Cu-Mo granodiorite 0 0 0 139.1 (Mao et al., 2006) hand samples ICP-MS Nanyangshan 52.79 0.27 1 Skarn Cu-Mo granodiorite 0 0 0 139.1 (Mao et al., 2006) hand samples ICP-MS Nanyangshan 53.02 0.5 1 Skarn Cu-Mo granodiorite 0 0 0 139.1 (Mao et al., 2006) hand samples ICP-MS Nanyangshan 184.8 1 1 Skarn Cu-Mo granodiorite 0 0 0 139.1 (Mao et al., 2006) hand samples ICP-MS Nanyangshan 184.9 1.7 1 Skarn Cu-Mo granodiorite 0 0 0 139.1 (Mao et al., 2006) hand samples ICP-MS Narrap 2.17 0.004 1 Quartz vein-hosted W granite 0 0 0 1019 (Raith and Stein, 2000) hand-picked magnetic concentrate NTIMS Narrap 2.318 0.003 1 Quartz vein-hosted W granite 0 0 0 1019 (Raith and Stein, 2000) hand-picked magnetic concentrate NTIMS Naruo 2321.2 31.000 Porphyry Cu-Au granodiorite 0 0 0 119.5 (J. Sun et al., 2017) concentrate, unknown method ICP-MS Naruo 2014.63 30.000 Porphyry Cu-Au granodiorite 0 0 0 119.5 (J. Sun et al., 2017) concentrate, unknown method ICP-MS Naruo 1635.58 19.000 Porphyry Cu-Au granodiorite 0 0 0 119.5 (J. Sun et al., 2017) concentrate, unknown method ICP-MS Naruo 3491.72 36.000 Porphyry Cu-Au granodiorite 0 0 0 119.5 (J. Sun et al., 2017) concentrate, unknown method ICP-MS Nianzigou 18.082 0.151 1 Porphyry Mo 0 0 0 0 154.3 (Zhang et al., 2009) hand samples ICP-MS Nianzigou 21.705 0.167 1 Porphyry Mo 0 0 0 0 154.3 (Zhang et al., 2009) hand samples ICP-MS Nianzigou 21.907 0.173 1 Porphyry Mo 0 0 0 0 154.3 (Zhang et al., 2009) hand samples ICP-MS Nianzigou 23.751 0.211 1 Porphyry Mo 0 0 0 0 154.3 (Zhang et al., 2009) hand samples ICP-MS Nianzigou 25.525 0.267 1 Porphyry Mo 0 0 0 0 154.3 (Zhang et al., 2009) hand samples ICP-MS Nianzigou 25.934 0.196 1 Porphyry Mo 0 0 0 0 154.3 (Zhang et al., 2009) hand samples ICP-MS Nianzigou 27.426 0.2 1 Porphyry Mo 0 0 0 0 154.3 (Zhang et al., 2009) hand samples ICP-MS Nippo 5.6 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Nisshin 4.2 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Nisshin 4.6 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Nithi Mountain 120 1 Porphyry Mo 0 0 0 0 0 (Sinclair et al., 2009) various NAA Niuling 0.02909 1 Quartz vein-hosted W 0 0 0 0 0 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Niuling 0.02909 0.00023 1 Quartz vein-hosted W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Niuling 0.04876 0.0004 1 Quartz vein-hosted W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Niuling 0.3326 0.0025 1 Quartz vein-hosted W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Niuling 0.637 0.0053 1 Quartz vein-hosted W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Niuling 13.106 1 Quartz vein-hosted W 0 0 0 0 0 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Niuling 13.106 0.102 1 Quartz vein-hosted W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Niuling 103.965 2.002 1 Quartz vein-hosted W 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Now Chun 200.5 2.1 1 Porphyry Cu granodiorite 0.23 0.025 0 13.71 (Aghazadeh et al., 2015) hand-picked grains unknown Nucleus 12.54 0.03 1 Skarn, epithermal Au granite; granitoid 0.24 0 0.86 76 (Bineli Betsi et al., 2013) hand samples ID-MS Nucleus 14.42 0.05 1 Skarn, epithermal Au granite; granitoid 0.24 0 0.86 76 (Bineli Betsi et al., 2013) hand samples ID-MS Nucleus 26.05 0.06 1 Skarn, epithermal Au granite; granitoid 0.24 0 0.86 76 (Bineli Betsi et al., 2013) hand samples ID-MS Nummedalen 811 1 Unknown 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Obayashi 25 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Obri Dul 14.57 0.040 1 Skarn 0 0 0 0 312.5 (Ackerman et al., 2017) hand-picked grains ICP-MS Obri Dul 2.4 Skarn 0 0 0 0 312.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Obri Dul 2.1 Skarn 0 0 0 0 312.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Obri Dul 8.8 Skarn 0 0 0 0 312.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Obri Dul 1.3 Skarn 0 0 0 0 312.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Obri Dul 2.4 Skarn 0 0 0 0 312.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Ogonja (Onganja) 499 1 Metamorphic Cu-Au 0 2.2 0 1.2 521 (Moore, 2010) hand samples NTIMS Ogonja (Onganja) 1465 1 Metamorphic Cu-Au 0 2.2 0 1.2 521 (Moore, 2010) hand samples NTIMS Ogonja (Onganja) 1826 1 Metamorphic Cu-Au 0 2.2 0 1.2 521 (Moore, 2010) hand samples NTIMS OK 746 1 Porphyry Cu diorite; granitoid; granodiorite; quartz monzonite 0.24 0.009 0 28 (Sinclair et al., 2009) various NAA Okawame 287.1 1.7 Skarn Mo granite 0 0 0 122.8 (Suzuki et al., 1996) hand samples ID-ICP-MS Okawame 302.4 1.6 Skarn Mo granite 0 0 0 122.8 (Suzuki et al., 1996) hand samples ID-ICP-MS Okawame 245 4 210 280 Skarn Mo granite 0 0 0 122.8 (Terada et al., 1971) hand-picked grains NAA Okawame 355 4 Skarn Mo granite 0 0 0 122.8 (Ishihara, 1988) various NAA/spectrophotometry Old Fort 159 1 Porphyry Cu 0 0.21 0.024 0 0 (Sinclair et al., 2009) various NAA Omey 150.46 0.55 1 Granite Mo granite 0 0 0 422.5 (Feely et al., 2010) magnetic concentrate NTIMS Oraviţa 5.882 0.009 1 Skarn Cu-Mo-Pb-Zn 0 0 0 0 74.355 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Oraviţa 19.77 0.04 1 Skarn Cu-Mo-Pb-Zn 0 0 0 0 74.355 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Oraviţa 918 3 1 Skarn Cu-Mo-Pb-Zn 0 0 0 0 74.355 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Ørsdalen 1.1 1 Granite Mo granite; granitoid 0 0 0 977 (Bingen and Stein, 2003) hand samples NTIMS Ørsdalen 9.8 1 Granite Mo granite; granitoid 0 0 0 977 (Bingen and Stein, 2003) hand samples NTIMS Ørsdalen 12 1 Granite Mo granite; granitoid 0 0 0 977 (Bingen and Stein, 2003) hand samples NTIMS Ørsdalen 13 1 Granite Mo granite; granitoid 0 0 0 977 (Bingen and Stein, 2003) hand samples NTIMS Ørsdalen 22 1 Granite Mo granite; granitoid 0 0 0 977 (Golden et al., 2013) unknown unknown Osa 4.1 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Osa 48 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Osa 37.8 5 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Otjozonjati 3606 1 Quartz vein-hosted 0 0 0 0 521 (Golden et al., 2013) unknown unknown Otome 4 1 Quartz vein-hosted W granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Otome 5.6 1 Quartz vein-hosted W granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Otome 50.83 0.13 1 Quartz vein-hosted W granite 0 0 0 0 (Suzuki et al., 1996) hand samples ID-ICP-MS Otome 92.95 0.33 1 Quartz vein-hosted W granite 0 0 0 0 (Suzuki et al., 1996) hand samples ID-ICP-MS Otomi 37 1 Quartz vein-hosted W granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Otomi 83 1 Quartz vein-hosted W granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Owashe 2.273 0.043 1 Quartz vein-hosted 0 0 0 0 42.9 (Suzuki et al., 1996) hand samples ID-ICP-MS Owashe 2.68 0.017 1 Quartz vein-hosted 0 0 0 0 42.9 (Suzuki et al., 1996) hand samples ID-ICP-MS Owashi 14 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Päävaara 5.44 1 Porphyry Mo 0 0 0 0 0 (Lavrov and Kuleshevich, 2010) unknown SEM Padrt 542 2.000 1 Quartz vein-hosted 0 0 0 0 343 (Ackerman et al., 2017) hand-picked grains ICP-MS Padrt 602.4 1.300 1 Quartz vein-hosted 0 0 0 0 343 (Ackerman et al., 2017) hand-picked grains ICP-MS Pagoni Rachi 4600 1 Porphyry Cu-Mo granodiorite; tonalite 0.4 0.01 0.57 30 (Voudouris et al., 2009) hand samples EPMA Pagoni Rachi 7600 1 Porphyry Cu-Mo granodiorite; tonalite 0.4 0.01 0.57 30 (Voudouris et al., 2010) hand samples EPMA Pagoni Rachi 8400 1 Porphyry Cu-Mo granodiorite; tonalite 0.4 0.01 0.57 30 (Voudouris et al., 2009) hand samples EPMA Pagoni Rachi 12600 1 Porphyry Cu-Mo granodiorite; tonalite 0.4 0.01 0.57 30 (Voudouris et al., 2009) hand samples EPMA Pagoni Rachi 16318 175 379 46900 Porphyry Cu-Mo granodiorite; tonalite 0.4 0.01 0.57 30 (Voudouris et al., 2013) thin sections EPMA Pagoni Rachi 19800 53 4500 42100 Porphyry Cu-Mo granodiorite; tonalite 0.4 0.01 0.57 30 (Berzina et al., 2005) various various Pagoni Rachi 28800 1 Porphyry Cu-Mo granodiorite; tonalite 0.4 0.01 0.57 30 (Voudouris et al., 2009) hand samples EPMA Pagoni Rachi 34300 1 Porphyry Cu-Mo granodiorite; tonalite 0.4 0.01 0.57 30 (Voudouris et al., 2009) hand samples EPMA Pagoni Rachi 37500 1 Porphyry Cu-Mo granodiorite; tonalite 0.4 0.01 0.57 30 (Voudouris et al., 2010) hand samples EPMA Pagoni Rachi 45900 1 Porphyry Cu-Mo granodiorite; tonalite 0.4 0.01 0.57 30 (Voudouris et al., 2009) hand samples EPMA Panantza 585.2 4 Porphyry Cu-Mo granodiorite; monzodiorite 0.82 0.007 0.1 154 (Chiaradia et al., 2009) hand samples NTIMS Paszowice 0.54 1 Granite Mo granite 0 0 0 310 (Mikulski and Stein, 2007) micro-drilled hand samples NTIMS Paszowice 0.68 1 Granite Mo granite 0 0 0 310 (Mikulski and Stein, 2007) micro-drilled hand samples NTIMS Paszowice 0.93 1 Granite Mo granite 0 0 0 310 (Mikulski and Stein, 2007) micro-drilled hand samples NTIMS Pattison 4.83 0.031 1 Porphyry Cu-Mo alkali-granite; quartz monzonite 0.01 0.015 0 65 (Selby and Creaser, 2001a) hand-picked magnetic/heavy liquids concentrate NTIMS Pattison 23.18 0.01 1 Porphyry Cu-Mo alkali-granite; quartz monzonite 0.01 0.015 0 65 (Selby and Creaser, 2001a) hand-picked magnetic/heavy liquids concentrate NTIMS Pax Mine 234 1 Unknown syenite 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Pax Mine 24 1 Unknown syenite 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Pax Mine 74 1 Unknown syenite 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Petráčkova hora 19.5 0.04 3 19.33 19.81 Intrusion-related Au granodiorite 0 0 1.08 344 (Zachariáš et al., 2001) hand samples NTIMS Petráčkova hora 43 0.08 1 Intrusion-related Au granodiorite 0 0 1.08 344 (Zachariáš et al., 2001) hand samples NTIMS Pine Creek 35 1 Skarn W 0 0 0.823 0 92 (Giles and Schilling, 1972) hand samples colorimetry Pine Creek 36 1 Skarn W 0 0 0.823 0 92 (Giles and Schilling, 1972) hand samples colorimetry Pine Creek 43 1 Skarn W 0 0 0.823 0 92 (Giles and Schilling, 1972) hand samples colorimetry Pine Creek 67 1 Skarn W 0 0 0.823 0 92 (Giles and Schilling, 1972) hand samples colorimetry Pine Creek 88 1 Skarn W 0 0 0.823 0 92 (Giles and Schilling, 1972) hand samples colorimetry Pine Creek 178 1 Skarn W 0 0 0.823 0 92 (Giles and Schilling, 1972) hand samples colorimetry Pingdi 13.9 6 4.1 44 Porphyry Mo granite 0 0.23 0 102.9 (Zhong et al., 2017) various various Plumas 90 1 Porphyry Cu diorite 0.4119 0 0.05 101 (Giles and Schilling, 1972) hand samples colorimetry Plumas 94 1 Porphyry Cu diorite 0.4119 0 0.05 101 (Giles and Schilling, 1972) hand samples colorimetry Plumas 108 1 Porphyry Cu diorite 0.4119 0 0.05 101 (Giles and Schilling, 1972) hand samples colorimetry Plumas 113 1 Porphyry Cu diorite 0.4119 0 0.05 101 (Giles and Schilling, 1972) hand samples colorimetry Plumas 115 1 Porphyry Cu diorite 0.4119 0 0.05 101 (Giles and Schilling, 1972) hand samples colorimetry Plumas 131 1 Porphyry Cu diorite 0.4119 0 0.05 101 (Giles and Schilling, 1972) hand samples colorimetry Pogo 0.197 0.002 1 Intrusion-related Au granite 0 0 16.12 100 (Selby et al., 2002) unknown NTIMS Pogo 1.753 0.014 1 Intrusion-related Au granite 0 0 16.12 100 (Selby et al., 2002) unknown NTIMS Pogo 4.209 0.005 1 Intrusion-related Au granite 0 0 16.12 100 (Selby et al., 2002) unknown NTIMS Pohled 3.114 0.009 1 Granite Mo granite 0 0 0 325 (Ackerman et al., 2017) hand-picked grains ICP-MS Porcupine 0.48 1 Orogenic Au syenogranite 0.2 0 1.31 1937 (Lawley et al., 2013) hand-picked magnetic/heavy liquids concentrate NTIMS Porcupine 1.72 1 Orogenic Au syenogranite 0.2 0 1.31 1937 (Lawley et al., 2013) hand-picked magnetic/heavy liquids/HF concentrate NTIMS Porcupine 1.73 1 Orogenic Au syenogranite 0.2 0 1.31 1937 (Lawley et al., 2013) hand-picked magnetic/heavy liquids concentrate NTIMS Porcupine 1.92 1 Orogenic Au syenogranite 0.2 0 1.31 1937 (Lawley et al., 2013) hand-picked magnetic/heavy liquids concentrate NTIMS Porcupine 1.96 1 Orogenic Au syenogranite 0.2 0 1.31 1937 (Lawley et al., 2013) hand-picked magnetic/heavy liquids/HF concentrate NTIMS Porcupine 3.35 1 Orogenic Au syenogranite 0.2 0 1.31 1937 (Lawley et al., 2013) hand-picked magnetic/heavy liquids/HF concentrate NTIMS Porcupine 3.37 1 Orogenic Au syenogranite 0.2 0 1.31 1937 (Lawley et al., 2013) hand-picked magnetic/heavy liquids concentrate NTIMS Porcupine 7.56 1 Orogenic Au syenogranite 0.2 0 1.31 1937 (Lawley et al., 2013) hand-picked magnetic/heavy liquids concentrate NTIMS Porcupine 10.29 1 Orogenic Au syenogranite 0.2 0 1.31 1937 (Lawley et al., 2013) hand-picked magnetic/heavy liquids/HF concentrate NTIMS Porcupine 10.79 1 Orogenic Au syenogranite 0.2 0 1.31 1937 (Lawley et al., 2013) hand-picked magnetic/heavy liquids concentrate NTIMS Preissac-Lacorne 21.3 1 Granite Mo monzogranite 0 0.186 0 2680 (Luck and Allègre, 1982) unknown ID-ion probe Preissac-Lacorne 22.2 1 Granite Mo monzogranite 0 0.186 0 2680 (Luck and Allègre, 1982) unknown ID-ion probe Preissac-Lacorne 26.2 1 Granite Mo monzogranite 0 0.186 0 2680 (Schindler, 1975) various NAA Preissac-Lacorne 28 1 Granite Mo monzogranite 0 0.186 0 2680 (Schindler, 1975) various NAA Preissac-Lacorne 29 1 Granite Mo monzogranite 0 0.186 0 2680 (Giles and Schilling, 1972) hand samples colorimetry Preissac-Lacorne 29.7 0.1 1 Granite Mo monzogranite 0 0.186 0 2680 (Suzuki et al., 1993) hand samples ID-ICP-MS Preissac-Lacorne 30.2 0.3 1 Granite Mo monzogranite 0 0.186 0 2680 (Suzuki et al., 1993) hand samples ID-ICP-MS Preissac-Lacorne 30.2 0.2 1 Granite Mo monzogranite 0 0.186 0 2680 (Suzuki et al., 1993) hand samples ID-ICP-MS Preissac-Lacorne 37 1 Granite Mo monzogranite 0 0.186 0 2680 (Giles and Schilling, 1972) hand samples colorimetry Premier 0.38 1 Granite Mo 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Pribram 26.09 0.080 1 Granite Mo granite 0 0 0 346.5 (Ackerman et al., 2017) hand-picked grains ICP-MS Pridhams 5.15 1 IOCG 0 1 0 0 1599 (Skirrow et al., 2007) unknown NTIMS Pt. Hedland 25.5 1 Unknown 0 0 0 0 0 (Riley, 1967) hand samples TIMS Punta de Salvia 40 1 Granite Mo granite 0 0 0 0 (Paganelli, 1963) unknown colorimetry Qarachilar 288.46 0.930 Porphyry Cu-Mo granodiorite 0 0 0 27.59 (Simmonds and Moazzen, 2015) hand-picked grains ICP-MS Qarachilar 462.82 2.350 Porphyry Cu-Mo granodiorite 0 0 0 27.59 (Simmonds and Moazzen, 2015) hand-picked grains ICP-MS Qarachilar 244.71 1.240 Porphyry Cu-Mo granodiorite 0 0 0 27.59 (Simmonds and Moazzen, 2015) hand-picked grains ICP-MS Qarachilar 202.76 0.960 Porphyry Cu-Mo granodiorite 0 0 0 27.59 (Simmonds and Moazzen, 2015) hand-picked grains ICP-MS Qarachilar 112.67 0.500 Porphyry Cu-Mo granodiorite 0 0 0 27.59 (Simmonds and Moazzen, 2015) hand-picked grains ICP-MS Qarachilar 277.36 2.120 Porphyry Cu-Mo granodiorite 0 0 0 27.59 (Simmonds and Moazzen, 2015) hand-picked grains ICP-MS Qianjiawan 334.9 2.7 1 Skarn Cu-Au diorite; granodiorite 0 0 0 0 (Xie et al., 2007) hand-picked magnetic concentrate ICP-MS Qiaoxiahala 1599.687 11.780 IOCG diorite 0.95166667 0 3.035 375.2 (Q. Li et al., 2014) hand-picked magnetic/heavy liquids concentrate ICP-MS Qiaoxiahala 699.966 5.370 IOCG diorite 0.95166667 0 3.035 375.2 (Q. Li et al., 2014) hand-picked magnetic/heavy liquids concentrate ICP-MS Qiaoxiahala 383.134 3.250 IOCG diorite 0.95166667 0 3.035 375.2 (Q. Li et al., 2014) hand-picked magnetic/heavy liquids concentrate ICP-MS Qiaoxiahala 1927.654 17.060 IOCG diorite 0.95166667 0 3.035 375.2 (Q. Li et al., 2014) hand-picked magnetic/heavy liquids concentrate ICP-MS Qiaoxiahala 4007.627 42.230 IOCG diorite 0.95166667 0 3.035 375.2 (Q. Li et al., 2014) hand-picked magnetic/heavy liquids concentrate ICP-MS Qiaoxiahala 4769.652 65.680 IOCG diorite 0.95166667 0 3.035 375.2 (Q. Li et al., 2014) hand-picked magnetic/heavy liquids concentrate ICP-MS Qiaoxiahala 4181.766 67.070 IOCG diorite 0.95166667 0 3.035 375.2 (Q. Li et al., 2014) hand-picked magnetic/heavy liquids concentrate ICP-MS Qiaoxiahala 3117.242 33.600 IOCG diorite 0.95166667 0 3.035 375.2 (Q. Li et al., 2014) hand-picked magnetic/heavy liquids concentrate ICP-MS Qiushuwan 112.7 1 Skarn Mo granodiorite 0.8 0.12 0 146.8 (Mao et al., 2008) hand samples ICP-MS Qiushuwan 127.7 1 Porphyry Cu-Mo granodiorite 0.8 0.12 0 146.8 (Mao et al., 2008) hand samples ICP-MS Qiushuwan 157.4 1 Porphyry Cu-Mo granodiorite 0.8 0.12 0 146.8 (Mao et al., 2008) hand samples ICP-MS Qiushuwan 161.5 1 Skarn Mo granodiorite 0.8 0.12 0 146.8 (Mao et al., 2008) hand samples ICP-MS Qiushuwan 171.5 1 Skarn Mo granodiorite 0.8 0.12 0 146.8 (Mao et al., 2008) hand samples ICP-MS Qiushuwan 180 1 Porphyry Cu-Mo granodiorite 0.8 0.12 0 146.8 (Mao et al., 2008) hand samples ICP-MS Queensgate 33 1 Quartz vein-hosted Mo 0 0 0 0 0 (Riley, 1967) hand samples TIMS Questa 7.3 1 Porphyry Mo diorite 0 0.144 0 24.5 (Hiskey and Meloche, 1940) unknown colorimetry Questa 7.5 1 Porphyry Mo diorite 0 0.144 0 24.5 (Fleischer, 1959) flotation concentrate unknown Questa 7.5 1 Porphyry Mo diorite 0 0.144 0 24.5 (Fleischer, 1959) flotation concentrate unknown Questa 7.5 1 Porphyry Mo diorite 0 0.144 0 24.5 (Fleischer, 1959) flotation concentrate unknown Questa 7.5 1 Porphyry Mo diorite 0 0.144 0 24.5 (Hiskey and Meloche, 1940) unknown colorimetry Questa 7.5 1 Porphyry Mo diorite 0 0.144 0 24.5 (Hiskey and Meloche, 1940) unknown colorimetry Questa 9 1 Porphyry Mo diorite 0 0.144 0 24.5 (Fleischer, 1959) flotation concentrate unknown Questa 9 1 Porphyry Mo diorite 0 0.144 0 24.5 (Hiskey and Meloche, 1940) unknown colorimetry Questa 12.5 1 Porphyry Mo diorite 0 0.144 0 24.5 (Fleischer, 1959) flotation concentrate unknown Questa 12.5 1 Porphyry Mo diorite 0 0.144 0 24.5 (Hiskey and Meloche, 1940) unknown colorimetry Questa 14 1 Porphyry Mo diorite 0 0.144 0 24.5 (Terada et al., 1971) hand-picked grains NAA Questa 10 1 Porphyry Mo diorite 0 0.144 0 24.5 (Terada et al., 1971) hand-picked grains NAA Questa 29 1 Porphyry Mo diorite 0 0.144 0 24.5 (Terada et al., 1971) hand-picked grains NAA Questa 200 100 1 Porphyry Mo diorite 0 0.144 0 24.5 (McCandless et al., 1993) hand-picked grains EPMA Qulong 16.4 0.1 1 Porphyry Cu-Mo granodiorite, monzogranite, quartz diorite 0.52 0.032 0 15.75 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Qulong 41.6 0.6 1 Porphyry Cu-Mo granodiorite, monzogranite, quartz diorite 0.52 0.032 0 15.75 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Qulong 136.7 3.1 1 Porphyry Cu-Mo granodiorite, monzogranite, quartz diorite 0.52 0.032 0 15.75 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Qulong 303.1 3.1 1 Porphyry Cu-Mo granodiorite, monzogranite, quartz diorite 0.52 0.032 0 15.75 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Qulong 143.32 1.080 Porphyry Cu-Mo granodiorite, monzogranite, quartz diorite 0.52 0.032 0 15.75 (Y. Li et al., 2017) hand-picked grains NTIMS Qulong 64.44 1.940 Porphyry Cu-Mo granodiorite, monzogranite, quartz diorite 0.52 0.032 0 15.75 (Y. Li et al., 2017) hand-picked grains NTIMS Qulong 104.16 1.320 Porphyry Cu-Mo granodiorite, monzogranite, quartz diorite 0.52 0.032 0 15.75 (Y. Li et al., 2017) hand-picked grains NTIMS Qulong 224.51 1.550 Porphyry Cu-Mo granodiorite, monzogranite, quartz diorite 0.52 0.032 0 15.75 (Y. Li et al., 2017) hand-picked grains NTIMS Qulong 221.57 1.180 Porphyry Cu-Mo granodiorite, monzogranite, quartz diorite 0.52 0.032 0 15.75 (Y. Li et al., 2017) hand-picked grains NTIMS Qulong 323.6 2.270 Porphyry Cu-Mo granodiorite, monzogranite, quartz diorite 0.52 0.032 0 15.75 (Y. Li et al., 2017) hand-picked grains NTIMS Qulong 615.4 Porphyry Cu-Mo granodiorite, monzogranite, quartz diorite 0.52 0.032 0 15.75 (Wang et al., 2016) hand samples MC-ICP-MS Ragunda 0.1921 0.000 Granite Mo granite 0 0 0 0 (Selby et al., 2007) various various Ray 600 400 1 Porphyry Cu-Mo quartz monzonite 0.681 0.01 0.004 66 (McCandless et al., 1993) hand-picked grains EPMA Red Bird 43 1 Porphyry Mo quartz monzonite 0.07 0.071 0 46 (Sinclair et al., 2009) various NAA Red Bird 6 1 Porphyry Mo quartz monzonite 0.07 0.071 0 46 (Sinclair et al., 2009) various NAA Red Hills 234 0.27 1 Porphyry Cu-Mo quartz monzonite 0.1 0 0 234.1 (Gilmer et al., 2003) hand samples unknown Red Mountain (Yukon) 32 2 56 73 Porphyry Mo granodiorite; quartz diorite 0 0.167 0 87.3 (Sinclair et al., 2009) various NAA Relin 29.5 1 Porphyry Cu-Mo monzogranite 0.049 83 (Gao et al., 2017) hand-picked grains ICP-MS Relin 29.4 1 Porphyry Cu-Mo monzogranite 0.049 83 (Gao et al., 2017) hand-picked grains ICP-MS Relin 6.8 1 Porphyry Cu-Mo monzogranite 0.049 83 (Gao et al., 2017) hand-picked grains ICP-MS Relin 12.7 1 Porphyry Cu-Mo monzogranite 0.049 83 (Gao et al., 2017) hand-picked grains ICP-MS Renfrew 1 1 Skarn W 0 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Revenue 15.02 0.04 1 Porphyry Cu-Au granodiorite; porphyry; quartz monzonite 0.12 0.03 0 78.05 (Bineli Betsi et al., 2013) hand samples ID-MS Revenue 15.09 0.04 1 Porphyry Cu-Au granodiorite; porphyry; quartz monzonite 0.12 0.03 0 78.05 (Bineli Betsi et al., 2013) hand samples ID-MS Roundy Creek 59 1 Porphyry Mo quartz monzonite 0 0.066 0 44.85 (Sinclair et al., 2009) various NAA Rozna 513.7 1.500 1 Pegmatite 0 0 0 0 0 (Ackerman et al., 2017) hand-picked grains ICP-MS Ruanjiawan 24.8 0.2 1 Skarn Cu granodiorite 0 0 0 0 (Xie et al., 2007) hand-picked magnetic concentrate ICP-MS Ruanjiawan 113.8 6 75.4 177 Skarn Cu granodiorite 0 0 0 0 (Zhong et al., 2017) various various S'Abba Gana 45 1 Granite Mo granite 0 0 0 0 (Paganelli, 1963) unknown colorimetry Sadisdorf 0.0898 0.000 1 Greisen Sn-W granite 0 0 0 323.5 (Ackerman et al., 2017) hand-picked grains ICP-MS Sadisdorf 0.04 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Sadisdorf 0.14 Greisen Sn-W granite 0 0 0 323.5 (Pasava et al., 2016) polished mounts LA-ICP-MS Salmijarvi 45.9 8.9 1 Porphyry Cu quartz monzodiorite 0.19 0.003 0.09 0 (Nigatu, 2011) micro-drilled hand samples ICP-MS Salmijarvi 59.9 5.8 1 Porphyry Cu quartz monzodiorite 0.19 0.003 0.09 0 (Nigatu, 2011) micro-drilled hand samples ICP-MS Salmijarvi 63.3 2.9 1 Porphyry Cu quartz monzodiorite 0.19 0.003 0.09 0 (Nigatu, 2011) micro-drilled hand samples ICP-MS Salmijarvi 91.9 5.3 1 Porphyry Cu quartz monzodiorite 0.19 0.003 0.09 0 (Nigatu, 2011) micro-drilled hand samples ICP-MS Salmijarvi 148 1.6 1 Porphyry Cu quartz monzodiorite 0.19 0.003 0.09 0 (Nigatu, 2011) micro-drilled hand samples ICP-MS Salmijarvi 223.4 3.4 1 Porphyry Cu quartz monzodiorite 0.19 0.003 0.09 0 (Nigatu, 2011) micro-drilled hand samples ICP-MS Salmijarvi 466.6 52.9 1 Porphyry Cu quartz monzodiorite 0.19 0.003 0.09 0 (Nigatu, 2011) micro-drilled hand samples ICP-MS Salmijarvi 1468.5 10.9 1 Porphyry Cu quartz monzodiorite 0.19 0.003 0.09 0 (Nigatu, 2011) micro-drilled hand samples ICP-MS Salmijarvi 1587.3 24.9 1 Porphyry Cu quartz monzodiorite 0.19 0.003 0.09 0 (Nigatu, 2011) micro-drilled hand samples ICP-MS Salobo 81.8 3 IOCG Cu-Au-Ag (Fe-Mo-U-Co-Ni) granite 1.31 0.02 0.66 2576 (Requia et al., 2003) micro-drilled hand samples NTIMS Salobo 198.9 2 IOCG Cu-Au-Ag (Fe-Mo-U-Co-Ni) granite 1.31 0.02 0.66 2576 (Requia et al., 2003) micro-drilled hand samples NTIMS San Antonio 519 1 Skarn Cu andesite; dacite; intrusive igneous rock 0.976 0.011 0.77 36.5 (Fleischer, 1959) flotation concentrate unknown San Carlos 743.5 5 Porphyry Cu-Mo granodiorite; monzodiorite 0.5 0.007 0 155.5 (Chiaradia et al., 2009) hand samples NTIMS San Carlos 831.6 9 Porphyry Cu-Mo granodiorite; monzodiorite 0.5 0.007 0 155.5 (Chiaradia et al., 2009) hand samples NTIMS San Manuel 300 200 1 Porphyry Cu-Mo diorite 0.6 0.011 0.017 61 (McCandless et al., 1993) hand-picked grains EPMA San Manuel 700 400 1 Porphyry Cu-Mo diorite 0.6 0.011 0.017 61 (McCandless et al., 1993) hand-picked grains EPMA San Manuel 800 200 1 Porphyry Cu-Mo diorite 0.6 0.011 0.017 61 (McCandless et al., 1993) hand-picked grains EPMA San Manuel 1200 1500 1 Porphyry Cu-Mo diorite 0.6 0.011 0.017 61 (McCandless et al., 1993) hand-picked grains EPMA San Martin 100 100 1 Skarn Cu 0 1 0 0 0 (McCandless et al., 1993) hand-picked grains EPMA Sanaeda 110 1 Porphyry Mo granodiorite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Sanaeda 120 1 Porphyry Mo granodiorite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Sandaozhuang 15.48 1 Skarn Mo-W granite 0 0 0 143.85 (Mao et al., 2008) hand samples ICP-MS Sandaozhuang 25.51 1 Porphyry Mo-W granite 0 0 0 143.85 (Mao et al., 2008) hand samples ICP-MS Sandaozhuang 27.92 1 Skarn Mo-W granite 0 0 0 143.85 (Mao et al., 2008) hand samples ICP-MS Santa Rita 500 400 1 Porphyry Cu 0 0.6203 0.008 0.056 55.5 (McCandless et al., 1993) hand-picked grains EPMA Santa Rita 1100 1000 1 Porphyry Cu 0 0.6203 0.008 0.056 55.5 (McCandless et al., 1993) hand-picked grains EPMA Santo Thomas II 10183 6 700 15400 Porphyry Cu-Au diorite; quartz diorite; tonalite; andesite 0.38 0.001 0.64 1.5 (Voudouris et al., 2013) thin sections EPMA Sanzhishu 20.3 6 15.7 25.7 Porphyry Mo monzogranite 0 0.06 0 111 (Zhong et al., 2017) various various Sar Cheshmeh 10.85 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 21.3 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 245 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 70.3 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 91.6 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 100.5 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 112 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 119 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 123 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 123.5 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 127.5 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 364 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 373 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 418 3.5 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aghazadeh et al., 2015) hand-picked grains unknown Sar Cheshmeh 426 3.4 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aghazadeh et al., 2015) hand-picked grains unknown Sar Cheshmeh 474 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 517 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) hand-picked grains ICP-MS Sar Cheshmeh 552 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) flotation concentrate ICP-MS Sar Cheshmeh 575 5 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aghazadeh et al., 2015) hand-picked grains unknown Sar Cheshmeh 580 4.2 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aghazadeh et al., 2015) hand-picked grains unknown Sar Cheshmeh 590 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) flotation concentrate ICP-MS Sar Cheshmeh 597 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) flotation concentrate ICP-MS Sar Cheshmeh 613 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) flotation concentrate ICP-MS Sar Cheshmeh 631 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aminzadeh et al., 2011) flotation concentrate ICP-MS Sar Cheshmeh 659 5.5 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aghazadeh et al., 2015) hand-picked grains unknown Sar Cheshmeh 888 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Mathur et al., 2000) hand-picked grains NTIMS Sar Cheshmeh 987 9.6 1 Porphyry Cu-Au granodiorite 1.2 0.03 0.27 13.29 (Aghazadeh et al., 2015) hand-picked grains unknown Sar Kuh 164.6 1.6 1 Porphyry Cu granodiorite 0.26 0.004 0 14.88 (Aghazadeh et al., 2015) hand-picked grains unknown Sar Kuh 452.1 6.4 1 Porphyry Cu granodiorite 0.26 0.004 0 14.88 (Aghazadeh et al., 2015) hand-picked grains unknown Sar Kuh 807.9 8.6 1 Porphyry Cu granodiorite 0.26 0.004 0 14.88 (Aghazadeh et al., 2015) hand-picked grains unknown Sar Kuh 1904 43 1 Porphyry Cu granodiorite 0.26 0.004 0 14.88 (Aghazadeh et al., 2015) hand-picked grains unknown Sardes 3785 7 1100 5200 Porphyry Cu-Mo quartz monzonite 0 0 0 0 (Voudouris et al., 2013) thin sections EPMA Sardes 3800 1 Porphyry Cu-Mo quartz monzonite 0 0 0 0 (Voudouris et al., 2010) hand samples EPMA Sardes 5200 1 Porphyry Cu-Mo quartz monzonite 0 0 0 0 (Voudouris et al., 2010) hand samples EPMA Sary-Cheku 600 12 320 960 Porphyry Cu-Mo 0 0.5 0 0.1 0 (Berzina et al., 2005) various various Sase 60 1 Quartz vein-hosted Mo granodiorite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Sase 100 1 Quartz vein-hosted Mo granodiorite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Sase 91 2 Quartz vein-hosted Mo granodiorite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Săvărsin 438.4 0.5 1 Quartz vein-hosted Mo 0 0 0 0 159.8 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Schaft Creek 590 1 Porphyry Cu-Mo breccia; granodiorite; quartz diorite; quartz monzonite 0.298 0.017 0.14 222 (Sinclair et al., 2009) various NAA Seikyu 81.4 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1967) unknown NAA Seikyu 82.8 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1967) unknown NAA Seikyu 85.2 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1967) unknown NAA Seikyu 73 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu 86.2 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1967) unknown NAA Seikyu 165.7 1.4 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Suzuki et al., 1996) hand samples ID-ICP-MS Seikyu 169.5 2.1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Suzuki et al., 1996) hand samples ID-ICP-MS Seikyu 79 10 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Ishihara, 1988) various NAA/spectrophotometry Seikyu 92.2 5 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Ishihara, 1988) various NAA/spectrophotometry Seikyu 133.3 3 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Ishihara, 1988) various NAA/spectrophotometry Seikyu—Chinka-Onobe 17 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Chukan-hi 97 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Chukan-hi 170 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Kamitani 23 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Kamitani 100 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Kamitani 85 3 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Ishihara, 1988) various NAA/spectrophotometry Seikyu—Minami 94 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Minami 120 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Minami 137.1 1.1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Suzuki et al., 1996) hand samples ID-ICP-MS Seikyu—Minami 138.2 0.66 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Suzuki et al., 1996) hand samples ID-ICP-MS Seikyu—Namera 62 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Namera 100 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Namera 103 3 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Ishihara, 1988) various NAA/spectrophotometry Seikyu—Ogashi-shin 130 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Ogashi-shin 120 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Onobe-shin 110 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Shin-i-go 26 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Shinsei-hi 33 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Shinsei-hi 69 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Uwa-hi 19 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Uwa-hi 140 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Ziri-hi 32 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Seikyu—Ziri-hi 41 1 Quartz vein-hosted granite; granodiorite 0 0 0 57.1 (Terada et al., 1971) hand-picked grains NAA Sekigane 1.6 1 Greisen Mo granite 0 0 0 66.5 (Terada et al., 1971) hand-picked grains NAA Sekigane 3.7 1 Greisen Mo granite 0 0 0 66.5 (Terada et al., 1971) hand-picked grains NAA Sekigane 4.979 0.02 1 Greisen Mo granite 0 0 0 66.5 (Suzuki et al., 1996) hand samples ID-ICP-MS Sekigane 5.108 0.022 1 Greisen Mo granite 0 0 0 66.5 (Suzuki et al., 1996) hand samples ID-ICP-MS Sekigane 2.4 3 Greisen Mo granite 0 0 0 66.5 (Ishihara, 1988) various NAA/spectrophotometry Sennai 1.5 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Sentinel 286.2 0.7 286.2 Sediment-hosted Cu 0 0 0 0 507.25 (Sillitoe et al., 2017) magnetic concentrate NTIMS Seriphos 200 1 Porphyry Mo-W alkali-granite 0 0 0 0 (Voudouris et al., 2010) hand samples EPMA Seriphos 345 11 10 1030 Porphyry Mo-W alkali-granite 0 0 0 0 (Voudouris et al., 2013) thin sections EPMA Seriphos 1000 1 Porphyry Mo-W alkali-granite 0 0 0 0 (Voudouris et al., 2010) hand samples EPMA Serra Verde 45.28 1 IOCG alkali-granite 0 0 0 2609 (Marschik et al., 2005) hand-picked grains NTIMS Serra Verde 11 1 IOCG alkali-granite 0 0 0 2609 (Mathur et al., 2010) hand-picked grains NTIMS Setting Net Lake 9.878 0.015 1 Porphyry Mo quartz monzonite 0 0.054 0 2643 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS Setting Net Lake 9.87 0.021 1 Porphyry Mo quartz monzonite 0 0.054 0 2643 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS Setting Net Lake 9.921 0.014 1 Porphyry Mo quartz monzonite 0 0.054 0 2643 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS Shakhtama 9 1 Porphyry Cu-Mo granite; granodiorite 0.26 0.06 0.09 152.5 (Berzina et al., 2005) various various Shakhtama 16 1 Porphyry Cu-Mo granite; granodiorite 0.26 0.06 0.09 152.5 (Berzina et al., 2005) various various Shakhtama 18 1 Porphyry Cu-Mo granite; granodiorite 0.26 0.06 0.09 152.5 (Berzina et al., 2005) various various Shakhtama 24 1 Porphyry Cu-Mo granite; granodiorite 0.26 0.06 0.09 152.5 (Berzina et al., 2005) various various Shalgiya 32 4 22 39 Porphyry Mo 0 0 0.11 0 0 (Berzina et al., 2005) various various Shalgiya 32 1 Porphyry Mo 0 0 0.11 0 0 (Fleischer, 1960) unknown colorimetry Shameika 2.17 1 1 Porphyry Mo alkali-granite 0 0.08 0 278 (Mao et al., 2003) hand samples ICP-MS Shameika 5.95 4 1 Porphyry Mo alkali-granite 0 0.08 0 278 (Mao et al., 2003) hand samples ICP-MS Shameika 8.42 8 1 Porphyry Mo alkali-granite 0 0.08 0 278 (Mao et al., 2003) hand samples ICP-MS Shameika 8.76 3 1 Porphyry Mo alkali-granite 0 0.08 0 278 (Mao et al., 2003) hand samples ICP-MS Shameika 9.08 2 1 Porphyry Mo alkali-granite 0 0.08 0 278 (Mao et al., 2003) hand samples ICP-MS Shameika 9.92 3 1 Porphyry Mo alkali-granite 0 0.08 0 278 (Mao et al., 2003) hand samples ICP-MS Shameika 11.59 7 1 Porphyry Mo alkali-granite 0 0.08 0 278 (Mao et al., 2003) hand samples ICP-MS Shameika 12.72 9 1 Porphyry Mo alkali-granite 0 0.08 0 278 (Mao et al., 2003) hand samples ICP-MS Shameika 13.9 8 1 Porphyry Mo alkali-granite 0 0.08 0 278 (Mao et al., 2003) hand samples ICP-MS Shameika 16.59 5 1 Porphyry Mo alkali-granite 0 0.08 0 278 (Mao et al., 2003) hand samples ICP-MS Shameika 36.94 2 1 Porphyry Mo alkali-granite 0 0.08 0 278 (Mao et al., 2003) hand samples ICP-MS Shand 531 1 Porphyry Cu-Mo granodiorite 1.01 0.02 0.6 241.5 (Watanabe and Stein, 2000) concentrate, unknown method NTIMS Shand 539 1 Porphyry Cu-Mo granodiorite 1.01 0.02 0.6 241.5 (Watanabe and Stein, 2000) concentrate, unknown method NTIMS Shangfanggou 19.58 1 Skarn Mo-W granite 0 0 0 142.35 (Mao et al., 2008) hand samples ICP-MS Shangfanggou 20.46 1 Skarn Mo-W granite 0 0 0 142.35 (Mao et al., 2008) hand samples ICP-MS Shankou 41.6 6 31.1 58.5 Porphyry Mo granite 0 0.14 0 165.3 (Zhong et al., 2017) various various Sharang 16.91 0.14 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 17.17 0.14 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 17.18 0.16 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 22.62 0.2 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 30.68 0.28 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 30.94 0.26 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 40.41 0.32 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 56.55 0.48 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 66.8 0.71 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 72.46 0.72 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 77.46 0.63 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 79.11 0.72 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 84.68 0.65 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 100.36 0.8 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 120.12 1.03 1 Porphyry Mo granite 0 0 0 52.3 (Zhao et al., 2014) hand samples ICP-MS Sharang 74.23 Porphyry Mo granite 0 0 0 52.3 (Wang et al., 2016) hand samples MC-ICP-MS Sharang 67.95 Porphyry Mo granite 0 0 0 52.3 (Wang et al., 2016) hand samples MC-ICP-MS Sharang 56.81 Porphyry Mo granite 0 0 0 52.3 (Wang et al., 2016) hand samples MC-ICP-MS Shatanjiao 174.2 1.6 1 Skarn Cu-Mo granodiorite 0 0 0 140 (Mao et al., 2006) hand samples ICP-MS Shatanjiao 674.2 6.1 1 Skarn Cu-Mo granodiorite 0 0 0 140 (Mao et al., 2006) hand samples ICP-MS Shatanjiao 674.5 3.5 1 Skarn Cu-Mo granodiorite 0 0 0 140 (Mao et al., 2006) hand samples ICP-MS Shatanjiao 1163 6 1 Skarn Cu-Mo granodiorite 0 0 0 140 (Mao et al., 2006) hand samples ICP-MS Shatanjiao 1169 12 1 Skarn Cu-Mo granodiorite 0 0 0 140 (Mao et al., 2006) hand samples ICP-MS Shedong 119.6 5 10.4 359.2 Porphyry W-Mo granodiorite 0 0.23 0 437.8 (Zhong et al., 2017) various various Shigushan 0.5773 1 Quartz vein-hosted W 0 0 0 0 154.2 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Shigushan 1.495 1 Quartz vein-hosted W 0 0 0 0 154.2 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Shijiawan 19 1 Porphyry Mo granite 0 0 0 140.65 (Mao et al., 2008) hand samples ICP-MS Shijiawan 19.32 1 Porphyry Mo granite 0 0 0 140.65 (Mao et al., 2008) hand samples ICP-MS Shimenshan 1.3899 0.006 Porphyry Mo monzogranite, granite 0 0.17 0 79.1 (Xu et al., 2016) unknown unknown Shimenshan 1.1068 0.007 Porphyry Mo monzogranite, granite 0 0.17 0 79.1 (Xu et al., 2016) unknown unknown Shimenshan 1.045 0.003 Porphyry Mo monzogranite, granite 0 0.17 0 79.1 (Xu et al., 2016) unknown unknown Shimenshan 1.673 0.006 Porphyry Mo monzogranite, granite 0 0.17 0 79.1 (Xu et al., 2016) unknown unknown Shimizu 5 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Shimizu 5.9 1 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Shino-machi (Shinomachi) 0.45 1 Quartz vein-hosted granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Shino-machi (Shinomachi) 0.5 1 Quartz vein-hosted granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Shipingchuan 15.1 Quartz vein-hosted Mo syenogranite 0 0.3 0 102.5 (Zhong et al., 2017) various various Shipingchuan 37.7 Quartz vein-hosted Mo syenogranite 0 0.3 0 102.5 (Zhong et al., 2017) various various Shirakawa 9.6 1 Skarn W granite 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Shiratori 0.01 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Shiratori 3.5 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Shiratori 1.5 3 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Shirenzhang 0.4843 1 Quartz vein-hosted W 0 0 0 0 159.1 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Shirenzhang 5.039 1 Quartz vein-hosted W 0 0 0 0 159.1 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Shiro 1.7 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Shiro 1.9 1 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Shizhuyuan 0.104 1 Skarn W 0 0 0 0 144 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Shizhuyuan 0.134 1 Skarn W 0 0 0 0 144 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Shizhuyuan 1.04 N/A 1 Skarn W 0 0 0 0 144 (Mao et al., 1999) various various Shizhuyuan 1.16 N/A 1 Skarn W 0 0 0 0 144 (Mao et al., 1999) various various Shizhuyuan 1.22 N/A 1 Skarn W 0 0 0 0 144 (Mao et al., 1999) various various Shizhuyuan 1.22 N/A 1 Skarn W 0 0 0 0 144 (Mao et al., 1999) various various Shizhuyuan 1.3 1 Skarn W 0 0 0 0 144 (Zhang et al., 2005) hand samples ICP-MS Shizhuyuan 1.32 N/A 1 Skarn W 0 0 0 0 144 (Mao et al., 1999) various various Shizhuyuan 1.34 N/A 1 Skarn W 0 0 0 0 144 (Mao et al., 1999) various various Shizhuyuan 1.2 6 1 1.3 Skarn W 0 0 0 0 144 (Zhong et al., 2017) various various Shizitou 148 6 71.1 197 Porphyry Mo granite 0 0.08 0 162.3 (Zhong et al., 2017) various various Shouwangfei 10.51 0.18 1 Porphyry, skarn Cu-Mo granodiorite 0.72 0.31 0 150 (Mao et al., 1999) various various Shuikoushan 1638 13.000 Granodiorite Pb-Zn granodiorite 0 0 0 157.8 (Huang et al., 2015) hand-picked grains ICP-MS Shuikoushan 1841 22.000 Granodiorite Pb-Zn granodiorite 0 0 0 157.8 (Huang et al., 2015) hand-picked grains ICP-MS Shuikoushan 1757 22.000 Granodiorite Pb-Zn granodiorite 0 0 0 157.8 (Huang et al., 2015) hand-picked grains ICP-MS Shuikoushan 1319 18.000 Granodiorite Pb-Zn granodiorite 0 0 0 157.8 (Huang et al., 2015) hand-picked grains ICP-MS Shuikoushan 419.9 3.700 Granodiorite Pb-Zn granodiorite 0 0 0 157.8 (Huang et al., 2015) hand-picked grains ICP-MS Shuikoushan 948.9 9.900 Granodiorite Pb-Zn granodiorite 0 0 0 157.8 (Huang et al., 2015) hand-picked grains ICP-MS Shuikoushan 705.4 5.600 Granodiorite Pb-Zn granodiorite 0 0 0 157.8 (Huang et al., 2015) hand-picked grains ICP-MS Siah-Kamar 25.681 0.208 Porphyry Mo monzonite, quartz monzonite 0 0.25 0 41.9 (Nabatian et al., 2017) hand-picked magnetic concentrate unknown Siah-Kamar 28.537 0.194 Porphyry Mo monzonite, quartz monzonite 0 0.25 0 41.9 (Nabatian et al., 2017) hand-picked magnetic concentrate unknown Siah-Kamar 31.66 0.236 Porphyry Mo monzonite, quartz monzonite 0 0.25 0 41.9 (Nabatian et al., 2017) hand-picked magnetic concentrate unknown Siah-Kamar 49.513 0.448 Porphyry Mo monzonite, quartz monzonite 0 0.25 0 41.9 (Nabatian et al., 2017) hand-picked magnetic concentrate unknown Siedlimowice 6 1 Granite Mo monzogranite 0 0 0 258 (Mikulski and Stein, 2007) micro-drilled hand samples NTIMS Siedlimowice 10 1 Granite Mo monzogranite 0 0 0 258 (Mikulski and Stein, 2007) micro-drilled hand samples NTIMS Sierrita 187 1 Porphyry Cu-Mo granite; granodiorite; quartz monzonite 0.26 0.023 0.003 57.75 (Jensen, 1998) hand samples NTIMS Sierrita 200 1 Porphyry Cu-Mo granite; granodiorite; quartz monzonite 0.26 0.023 0.003 57.75 (Jensen, 1998) hand samples NTIMS Sierrita 200 100 1 Porphyry Cu-Mo granite; granodiorite; quartz monzonite 0.26 0.023 0.003 57.75 (McCandless et al., 1993) hand-picked grains EPMA Sierrita 238.2 1 Porphyry Cu-Mo granite; granodiorite; quartz monzonite 0.26 0.023 0.003 57.75 (McCandless and Ruiz, 1993) unknown unknown Sierrita 243 1 Porphyry Cu-Mo granite; granodiorite; quartz monzonite 0.26 0.023 0.003 57.75 (Jensen, 1998) hand samples NTIMS Sierrita 258 1 Porphyry Cu-Mo granite; granodiorite; quartz monzonite 0.26 0.023 0.003 57.75 (Jensen, 1998) hand samples NTIMS Sileurian Cheiftain 38 Porphyry Cu-Mo 0 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Sileurian Cheiftain 41 1 Porphyry Cu-Mo 0 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Silver Bell 200 200 1 Porphyry Cu 0 0.66 0.013 0.026 63.2 (McCandless et al., 1993) hand-picked grains EPMA Silver Bell 300 200 1 Porphyry Cu 0 0.66 0.013 0.026 63.2 (McCandless et al., 1993) hand-picked grains EPMA Silver Bell 530.5 0.4 1 Porphyry Cu 0 0.66 0.013 0.026 63.2 (Barra et al., 2005) hand-picked grains NTIMS Silver Bell 400 100 1 Porphyry Cu 0 0.66 0.013 0.026 63.2 (McCandless et al., 1993) hand-picked grains EPMA Silver Bell 1300 200 1 Porphyry Cu 0 0.66 0.013 0.026 63.2 (McCandless et al., 1993) hand-picked grains EPMA Sipalay 1700 1 Porphyry Cu diorite 0.47 0.014 0.05 30 (Terada et al., 1971) hand-picked grains NAA Sira 3.783 0.003 1 Granite Mo 0 0 0 0 942 (Bingen et al., 2006) micro-drilled hand samples NTIMS Sira 6.843 0.004 1 Granite Mo 0 0 0 0 942 (Bingen et al., 2006) micro-drilled hand samples NTIMS Sira 11.28 0.01 1 Granite Mo 0 0 0 0 942 (Bingen et al., 2006) micro-drilled hand samples NTIMS Sira 22.98 0.01 1 Granite Mo 0 0 0 0 942 (Bingen et al., 2006) micro-drilled hand samples NTIMS Sira 27.83 0.02 1 Granite Mo 0 0 0 0 942 (Bingen et al., 2006) micro-drilled hand samples NTIMS Sira 27.88 0.04 1 Granite Mo 0 0 0 0 942 (Bingen et al., 2006) micro-drilled hand samples NTIMS Skalsko 133.5 0.300 1 Pegmatite 0 0 0 0 354 (Ackerman et al., 2017) hand-picked grains ICP-MS Skalsko 78 Pegmatite 0 0 0 0 354 (Pasava et al., 2016) polished mounts LA-ICP-MS Skalsko 59 Pegmatite 0 0 0 0 354 (Pasava et al., 2016) polished mounts LA-ICP-MS Skalsko 33 Pegmatite 0 0 0 0 354 (Pasava et al., 2016) polished mounts LA-ICP-MS Skalsko 19 Pegmatite 0 0 0 0 354 (Pasava et al., 2016) polished mounts LA-ICP-MS Skalsko 4.9 Pegmatite 0 0 0 0 354 (Pasava et al., 2016) polished mounts LA-ICP-MS Skalsko 10 Pegmatite 0 0 0 0 354 (Pasava et al., 2016) polished mounts LA-ICP-MS Skouries 900 4 800 1000 Porphyry Cu-Au diorite; syenite 0.35 0 0.47 18.5 (Berzina et al., 2005) various various Skutec 205.1 0.700 1 Granite Mo granite 0 0 0 0 (Ackerman et al., 2017) hand-picked grains ICP-MS Sodagawa 21 1 Granite Mo 0 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Sonoma Pass 38 1 Pegmatite 0 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Sora 6 1 Porphyry Cu-Mo alkali-granite; diorite; granite; monzogabbro; monzonite; monzodiorite; quartz monzodiorite; syenite 0.17 0.058 0.017 396.5 (Berzina et al., 2005) various various Sora 9 1 Porphyry Cu-Mo alkali-granite; diorite; granite; monzogabbro; monzonite; monzodiorite; quartz monzodiorite; syenite 0.17 0.058 0.017 396.5 (Berzina et al., 2005) various various Sora 11 1 Porphyry Cu-Mo alkali-granite; diorite; granite; monzogabbro; monzonite; monzodiorite; quartz monzodiorite; syenite 0.17 0.058 0.017 396.5 (Berzina et al., 2005) various various Sora 13 1 Porphyry Cu-Mo alkali-granite; diorite; granite; monzogabbro; monzonite; monzodiorite; quartz monzodiorite; syenite 0.17 0.058 0.017 396.5 (Berzina et al., 2005) various various Sora 15 1 Porphyry Cu-Mo alkali-granite; diorite; granite; monzogabbro; monzonite; monzodiorite; quartz monzodiorite; syenite 0.17 0.058 0.017 396.5 (Berzina et al., 2005) various various Sora 16 1 Porphyry Cu-Mo alkali-granite; diorite; granite; monzogabbro; monzonite; monzodiorite; quartz monzodiorite; syenite 0.17 0.058 0.017 396.5 (Berzina et al., 2005) various various Sora 17 1 Porphyry Cu-Mo alkali-granite; diorite; granite; monzogabbro; monzonite; monzodiorite; quartz monzodiorite; syenite 0.17 0.058 0.017 396.5 (Berzina et al., 2005) various various Sora 17 1 Porphyry Cu-Mo alkali-granite; diorite; granite; monzogabbro; monzonite; monzodiorite; quartz monzodiorite; syenite 0.17 0.058 0.017 396.5 (Berzina et al., 2005) various various Sora 18 1 Porphyry Cu-Mo alkali-granite; diorite; granite; monzogabbro; monzonite; monzodiorite; quartz monzodiorite; syenite 0.17 0.058 0.017 396.5 (Berzina et al., 2005) various various South Mountain Batholith 0.26 0.003 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 0.336 0.002 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 0.348 0.003 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 0.365 0.002 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 0.381 0.006 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 0.393 0.003 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 0.413 0.003 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 0.438 0.002 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 0.447 0.003 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 0.465 0.003 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 0.466 0.003 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 0.494 0.004 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 0.497 0.002 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 0.521 0.003 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 1.479 0.006 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 1.496 0.005 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 1.496 0.006 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 4.14 0.015 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 4.213 0.021 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 4.233 0.021 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 4.209 0.015 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 4.248 0.015 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 4.272 0.014 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS South Mountain Batholith 4.227 0.014 1 Granite Sn-W 0 0 0 0 0 (Selby and Creaser, 2004) hand-picked magnetic/heavy liquids concentrate LA-ICP-MS and NTIMS Squaw Peak 200 100 1 Porphyry Cu-Au quartz diorite 0.4 0 0 60.65 (McCandless et al., 1993) hand-picked grains EPMA St. Helens 2.3 1 Unknown 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA St. Helens 1.9 Unknown 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Stachlovice 3.37 0.010 1 Granodiorite Mo granodiorite 0 0 0 296 (Ackerman et al., 2017) hand-picked grains ICP-MS Star 100 100 1 Skarn W-Mo 0 0 0 0 0 (McCandless et al., 1993) hand-picked grains EPMA Stare Ransko 1.8 VMS gabbro; peridotite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Stare Ransko 1.2 VMS gabbro; peridotite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Stare Ransko 1.6 VMS gabbro; peridotite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Stare Ransko 3 VMS gabbro; peridotite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Stare Ransko 1.1 VMS gabbro; peridotite 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Starra 4.52 1 1 IOCG Au-Cu (Co-W-W) granite 1.9 0.004 3.8 1582.5 (Duncan et al., 2011) micro-drilled hand samples NTIMS Starra 5.273 4 1 IOCG Au-Cu (Co-W-W) granite 1.9 0.004 3.8 1582.5 (Duncan et al., 2011) micro-drilled hand samples NTIMS Starra 245.3 6 1 IOCG Au-Cu (Co-W-W) granite 1.9 0.004 3.8 1582.5 (Duncan et al., 2011) micro-drilled hand samples NTIMS Stavanger 3035 1 Unknown 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Stavanger 3130 1 Unknown 0 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Storie Moly 23 1 Porphyry Mo quartz monzonite 0 0.078 0 82.55 (Sinclair et al., 2009) various NAA Storie Moly 15 1 Porphyry Mo quartz monzonite 0 0.078 0 82.55 (Sinclair et al., 2009) various NAA Storie Moly 22 1 Porphyry Mo quartz monzonite 0 0.078 0 82.55 (Sinclair et al., 2009) various NAA Stypsi 1400 1 Porphyry Cu dacite 0 0 0.1 0 (Voudouris et al., 2010) hand samples EPMA Stypsi 6400 1 Porphyry Cu dacite 0 0 0.1 0 (Voudouris et al., 2010) hand samples EPMA Stypsi 10600 1 Porphyry Cu dacite 0 0 0.1 0 (Voudouris et al., 2010) hand samples EPMA Stypsi 2460 10 300 10600 Porphyry Cu dacite 0 0 0.1 0 (Voudouris et al., 2013) thin sections EPMA Su Seinargiu 0.345 0.0005 1 Granite Mo 0 0 0 0 290 (Boni et al., 2003) hand samples unknown Suaqui Verde 164.8 0.1 1 Porphyry Cu diorite; andesite 0.43 0 0 56.9 (Barra et al., 2005) hand-picked grains NTIMS Suaqui Verde 189.9 0.2 1 Porphyry Cu diorite; andesite 0.43 0 0 56.9 (Barra et al., 2005) hand-picked grains NTIMS Sundown 1.5 1 Quartz vein-hosted Cu 0 0 0 0 0 (Riley, 1967) hand samples TIMS Suoerkuduke 232.2 2.2 1 Skarn Cu-Mo 0 0 0 0 310 (Wan et al., 2014) hand-picked magnetic concentrate ICP-MS Suoerkuduke 232.7 1.7 1 Skarn Cu-Mo 0 0 0 0 310 (Wan et al., 2014) hand-picked magnetic concentrate ICP-MS Suoerkuduke 261.9 2.7 1 Skarn Cu-Mo 0 0 0 0 310 (Wan et al., 2014) hand-picked magnetic concentrate ICP-MS Suoerkuduke 265.8 2.2 1 Skarn Cu-Mo 0 0 0 0 310 (Wan et al., 2014) hand-picked magnetic concentrate ICP-MS Suoerkuduke 597.4 7.1 1 Skarn Cu-Mo 0 0 0 0 310 (Wan et al., 2014) hand-picked magnetic concentrate ICP-MS Suoerkuduke 813.2 8.4 1 Skarn Cu-Mo 0 0 0 0 310 (Wan et al., 2014) hand-picked magnetic concentrate ICP-MS Suoerkuduke 818.3 7.5 1 Skarn Cu-Mo 0 0 0 0 310 (Wan et al., 2014) hand-picked magnetic concentrate ICP-MS Suoerkuduke 892.2 11 1 Skarn Cu-Mo 0 0 0 0 310 (Wan et al., 2014) hand-picked magnetic concentrate ICP-MS Suoerkuduke 901.5 11 1 Skarn Cu-Mo 0 0 0 0 310 (Wan et al., 2014) hand-picked magnetic concentrate ICP-MS Susap 130 1 Porphyry Cu-Mo granodiorite, quartz monzonite, monzonite, syenite, diorite 0.155 0.045 0 172.55 (Sinclair et al., 2009) various NAA Sutsu 1061.9 7 Porphyry Cu-Mo granodiorite; monzodiorite 0.5 0.007 0 155 (Chiaradia et al., 2009) hand samples NTIMS Suyunhe 78.91 0.73 1 Quartz vein-hosted 0 0 0 0 301.15 (Shen et al., 2013) unknown ICP-MS Suyunhe 89.53 0.95 1 Quartz vein-hosted 0 0 0 0 301.15 (Shen et al., 2013) unknown ICP-MS Suyunhe 95.77 0.92 1 Quartz vein-hosted 0 0 0 0 301.15 (Shen et al., 2013) unknown ICP-MS Suyunhe 105.3 0.9 1 Quartz vein-hosted 0 0 0 0 301.15 (Shen et al., 2013) unknown ICP-MS Suyunhe 180.9 2 1 Quartz vein-hosted 0 0 0 0 301.15 (Shen et al., 2013) unknown ICP-MS SWAN 177.5 2 1 IOCG Cu-Au (Fe) granite 0.5 0 0.3 1515 (Duncan et al., 2011) micro-drilled hand samples NTIMS Taiyangshan 38.43 0.380 Porphyry Cu-Mo quartz diorite, monzonite, quartz monzonite, granite 0.54 0.12 0 208 (Qiu et al., 2016b) hand-picked grains ICP-MS Taiyangshan 35.33 0.320 Porphyry Cu-Mo quartz diorite, monzonite, quartz monzonite, granite 0.54 0.12 0 208 (Qiu et al., 2016b) hand-picked grains ICP-MS Taiyangshan 29.28 0.240 Porphyry Cu-Mo quartz diorite, monzonite, quartz monzonite, granite 0.54 0.12 0 208 (Qiu et al., 2016b) hand-picked grains ICP-MS Taiyangshan 32.81 0.270 Porphyry Cu-Mo quartz diorite, monzonite, quartz monzonite, granite 0.54 0.12 0 208 (Qiu et al., 2016b) hand-picked grains ICP-MS Taiyangshan 32.67 0.260 Porphyry Cu-Mo quartz diorite, monzonite, quartz monzonite, granite 0.54 0.12 0 208 (Qiu et al., 2016b) hand-picked grains ICP-MS Taiyangshan 27.7 0.240 Porphyry Cu-Mo quartz diorite, monzonite, quartz monzonite, granite 0.54 0.12 0 208 (Qiu et al., 2016b) hand-picked grains ICP-MS Takagi 95 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Takagi 150 1 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Takagigawa 37.376 0.087 1 Unknown Mo 0 0 0 0 0 (Suzuki et al., 1996) hand samples ID-ICP-MS Takagigawa 43.77 0.1 1 Unknown Mo 0 0 0 0 0 (Suzuki et al., 1996) hand samples ID-ICP-MS Takashiro 98 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Takashiro 130 1 Quartz vein-hosted Mo granite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Takashiro 155 3 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Takatori 57.9 1.8 Greisen Sn-W 0 0 0 0 11 (Suzuki et al., 1996) hand samples ID-ICP-MS Takatori 69.01 0.45 1 Greisen Sn-W 0 0 0 0 11 (Suzuki et al., 1996) hand samples ID-ICP-MS Talitsa 27.3 0.060 Porphyry Cu-Mo granodiorite, quartz monzonite, granite 0.28 0.19 0 299.1 (Tessalina and Plotinskaya, 2017) hand-picked grains ID-TIMS Talnakh 38000 1 Magmatic Ni-Cu-PGE gabbrodolerite; gabbro; quartz diorite 0 0 0 251.5 (Kovalenker et al., 1974) unknown EPMA Talnakh 28000 1 Magmatic Ni-Cu-PGE gabbrodolerite; gabbro; quartz diorite 0 0 0 251.5 (Kovalenker et al., 1974) unknown EPMA Talnakh 6000 Magmatic Ni-Cu-PGE gabbrodolerite; gabbro; quartz diorite 0 0 0 251.5 (Kovalenker et al., 1974) unknown EPMA Tamatsukuri 70 3 Quartz vein-hosted Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Tameapa 71 0.1 1 Porphyry Cu-Mo dacite; granite; granodiorite; tonalite 0.4 0.68 0 53.7 (Barra et al., 2005) hand-picked grains NTIMS Tameapa 76.1 0.1 1 Porphyry Cu-Mo dacite; granite; granodiorite; tonalite 0.4 0.68 0 53.7 (Barra et al., 2005) hand-picked grains NTIMS Tameapa 85.5 0.1 1 Porphyry Cu-Mo dacite; granite; granodiorite; tonalite 0.4 0.68 0 53.7 (Barra et al., 2005) hand-picked grains NTIMS Tameapa 93.2 0.1 1 Porphyry Cu-Mo dacite; granite; granodiorite; tonalite 0.4 0.68 0 53.7 (Barra et al., 2005) hand-picked grains NTIMS Tameapa 173.1 0.2 1 Porphyry Cu-Mo dacite; granite; granodiorite; tonalite 0.4 0.68 0 53.7 (Barra et al., 2005) hand-picked grains NTIMS Tameapa 181.8 0.1 1 Porphyry Cu-Mo dacite; granite; granodiorite; tonalite 0.4 0.68 0 53.7 (Barra et al., 2005) hand-picked grains NTIMS Tameapa 198.8 0.2 1 Porphyry Cu-Mo dacite; granite; granodiorite; tonalite 0.4 0.68 0 53.7 (Barra et al., 2005) hand-picked grains NTIMS Tameapa 199 0.2 1 Porphyry Cu-Mo dacite; granite; granodiorite; tonalite 0.4 0.68 0 53.7 (Barra et al., 2005) hand-picked grains NTIMS Tameapa 610.4 0.5 1 Porphyry Cu-Mo dacite; granite; granodiorite; tonalite 0.4 0.68 0 53.7 (Barra et al., 2005) hand-picked grains NTIMS Tameapa 618.8 0.5 1 Porphyry Cu-Mo dacite; granite; granodiorite; tonalite 0.4 0.68 0 53.7 (Barra et al., 2005) hand-picked grains NTIMS Tameapa 740.7 0.6 1 Porphyry Cu-Mo dacite; granite; granodiorite; tonalite 0.4 0.68 0 53.7 (Barra et al., 2005) hand-picked grains NTIMS Tangjiaping 3.955 1 Porphyry Mo granite 0 0.09 0 115.4 (Mao et al., 2008) hand samples ICP-MS Tangjiaping 4.041 1 Porphyry Mo granite 0 0.09 0 115.4 (Mao et al., 2008) hand samples ICP-MS Tangjiaping 4.451 1 Porphyry Mo granite 0 0.09 0 115.4 (Mao et al., 2008) hand samples ICP-MS Tangjiaping 5.96 1 Porphyry Mo granite 0 0.09 0 115.4 (Mao et al., 2008) hand samples ICP-MS Tangjiaping 6.562 1 Porphyry Mo granite 0 0.09 0 115.4 (Mao et al., 2008) hand samples ICP-MS Tangjiaping 10.81 1 Porphyry Mo granite 0 0.09 0 115.4 (Mao et al., 2008) hand samples ICP-MS Tangjiaping 11.94 1 Porphyry Mo granite 0 0.09 0 115.4 (Mao et al., 2008) hand samples ICP-MS Taohuazui 371.3 3.2 1 Skarn Au-Cu quartz diorite 2.2 0 3.6 138 (Xie et al., 2011) hand-picked grains ICP-MS Taohuazui 1009 9 1 Skarn Au-Cu quartz diorite 2.2 0 3.6 138 (Xie et al., 2011) hand-picked grains ICP-MS Taoxikeng 4.851 1 Quartz vein-hosted W 0 0 0 0 154.4 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Taoxikeng 7.486 1 Quartz vein-hosted W 0 0 0 0 154.4 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Taoxikeng 7.711 1 Quartz vein-hosted W 0 0 0 0 154.4 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Taoxikeng 10.35 1 Quartz vein-hosted W 0 0 0 0 154.4 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Taoxikeng 13.03 1 Quartz vein-hosted W 0 0 0 0 154.4 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Taseko 154 1 Porphyry Cu-Au granodiorite; quartz diorite; quartz monzonite 0.53 0.012 0.53 85.9 (Sinclair et al., 2009) various NAA Telemark 21 1 Granite Mo granite; quartz diorite 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Telimbela 312.8 3 1 Porphyry Cu granodiorite; quartz diorite 0 0 0 15 (Schütte et al., 2012) concentrate, unknown method NTIMS Tempiute 44 1 Skarn W granite 0 0 0 338.65 (Giles and Schilling, 1972) hand samples colorimetry Tenabo 49 1 Porphyry Cu-Au granite 0 0 0 0 (Giles and Schilling, 1972) hand samples colorimetry Tepasto 7.55 1 Granite Mo granite 0 0 0 1590 (Luck and Allègre, 1982) unknown ID-ion probe Tepasto 11.1 1 Granite Mo granite 0 0 0 1590 (Luck and Allègre, 1982) unknown ID-ion probe Tepasto 4.31 0.010 Granite Mo granite 0 0 0 1590 (Selby et al., 2007) various various Thrudvang 54.02 33.950 Quartz vein-hosted Mo-W 0 0 0 0 2749 (Rosa and Ulrich, 2015) concentrate, unknown method NTIMS Tianmugou 13.01 1 Porphyry Mo granite 0 0.6 0 121.6 (Mao et al., 2008) hand samples ICP-MS Tianmugou 25.08 1 Porphyry Mo granite 122 (Y. Yang et al., 2017) hand-picked magnetic concentrate ICP-MS Tianmugou 26.41 1 Porphyry Mo granite 122 (Y. Yang et al., 2017) hand-picked magnetic concentrate ICP-MS Tianmugou 31.62 1 Porphyry Mo granite 122 (Y. Yang et al., 2017) hand-picked magnetic concentrate ICP-MS Tianmugou 29.15 1 Porphyry Mo granite 122 (Y. Yang et al., 2017) hand-picked magnetic concentrate ICP-MS Tianmugou 27.94 1 Porphyry Mo granite 122 (Y. Yang et al., 2017) hand-picked magnetic concentrate ICP-MS Tianmugou 23.21 1 Porphyry Mo granite 122 (Y. Yang et al., 2017) hand-picked magnetic concentrate ICP-MS Tianmugou 31.64 1 Porphyry Mo granite 122 (Y. Yang et al., 2017) hand-picked magnetic concentrate ICP-MS Tidewater 109 1 Porphyry Mo 0 0 0.06 0 86 (Sinclair et al., 2009) various NAA Tidewater 13 1 Porphyry Mo 0 0 0.06 0 86 (Sinclair et al., 2009) various NAA Tincova 82.2 0.1 1 Skarn Fe-Pb-Zn 0 0 0 0 76.555 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Tincova 86.6 0.1 1 Skarn Fe-Pb-Zn 0 0 0 0 76.555 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Tinggong 255.7 2.5 1 Porphyry Cu-Mo 0 0.5 0 0 15.4 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Tinggong 259.4 3.2 1 Porphyry Cu-Mo 0 0.5 0 0 15.4 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Tinggong 330.5 3.2 1 Porphyry Cu-Mo 0 0.5 0 0 15.4 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Tinggong 406.3 3.7 1 Porphyry Cu-Mo 0 0.5 0 0 15.4 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Tinggong 510.9 4.8 1 Porphyry Cu-Mo 0 0.5 0 0 15.4 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Tinggong 708.8 7.5 1 Porphyry Cu-Mo 0 0.5 0 0 15.4 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Tinggong 992.7 11 1 Porphyry Cu-Mo 0 0.5 0 0 15.4 (Hou et al., 2009) hand-picked heavy liquid concentrate unknown Tintaya 547 1 Porphyry Cu-Au monzonite 1.7804 0 0 33 (Mathur et al., 2000) hand-picked grains NTIMS Tintaya 550 1 Porphyry Cu-Au monzonite 1.7804 0 0 33 (Berzina et al., 2005) various various Tominskoe 1080 1 Porphyry Cu 0 0.58 0 0.12 347 (Voudouris et al., 2013) thin sections EPMA Tongchang 13.32 0.1 1 Porphyry Cu-Mo diabase; diorite; gabbro; granodiorite; intrusive igneous rock; pyroxenite 0.459 0.016 0.12 173 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Tongchang 21.84 0.18 1 Porphyry Cu-Mo diabase; diorite; gabbro; granodiorite; intrusive igneous rock; pyroxenite 0.459 0.016 0.12 173 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Tongchang 29.77 0.24 1 Porphyry Cu-Mo diabase; diorite; gabbro; granodiorite; intrusive igneous rock; pyroxenite 0.459 0.016 0.12 173 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Tongchang 33.83 0.25 1 Porphyry Cu-Mo diabase; diorite; gabbro; granodiorite; intrusive igneous rock; pyroxenite 0.459 0.016 0.12 173 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Tongchang 74.39 0.59 1 Porphyry Cu-Mo diabase; diorite; gabbro; granodiorite; intrusive igneous rock; pyroxenite 0.459 0.016 0.12 173 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Tongchang 76.87 0.65 1 Porphyry Cu-Mo diabase; diorite; gabbro; granodiorite; intrusive igneous rock; pyroxenite 0.459 0.016 0.12 173 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Tongchang 107.3 1 1 Porphyry Cu-Mo diabase; diorite; gabbro; granodiorite; intrusive igneous rock; pyroxenite 0.459 0.016 0.12 173 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Tongchang 134.7 1.1 1 Porphyry Cu-Mo diabase; diorite; gabbro; granodiorite; intrusive igneous rock; pyroxenite 0.459 0.016 0.12 173 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Tongchang 157.1 1.1 1 Porphyry Cu-Mo diabase; diorite; gabbro; granodiorite; intrusive igneous rock; pyroxenite 0.459 0.016 0.12 173 (Xu et al., 2012) hand-picked heavy liquid concentrate ICP-MS Tongchanggou 101.8 1 Porphyry Mo-Cu granodiorite 0.8 0.3 86 (Yang et al., 2017) hand-picked grains ICP-MS Tongchanggou 50.1 1 Skarn Mo granodiorite 0.8 0.3 86 (Yang et al., 2017) hand-picked grains ICP-MS Tongchanggou 21.4 1 Porphyry Mo-Cu granodiorite 0.8 0.3 86 (Yang et al., 2017) hand-picked grains ICP-MS Tongchanggou 18.2 1 Porphyry Mo-Cu granodiorite 0.8 0.3 86 (Yang et al., 2017) hand-picked grains ICP-MS Tongcun 68 3 18.5 94.8 Porphyry, skarn Mo granite 0 0.01 0 161.8 (Zhong et al., 2017) various various Tongcun 85.4 6 36.6 121.7 Porphyry, skarn Mo granite 0 0.01 0 161.8 (Zhong et al., 2017) various various Tongkengzhang 1.3 6 1.1 1.3 Porphyry Mo granite 0 0.12 0 133.7 (Zhong et al., 2017) various various Tongkuangli 53.52 0.49 1 Skarn Mo granite 0 0 0 141.1 (Mao et al., 2006) hand samples ICP-MS Tongkuangli 53.71 0.28 1 Skarn Mo granite 0 0 0 141.1 (Mao et al., 2006) hand samples ICP-MS Tongkuangli 54.46 0.28 1 Skarn Mo granite 0 0 0 141.1 (Mao et al., 2006) hand samples ICP-MS Tongkuangli 54.5 0.52 1 Skarn Mo granite 0 0 0 141.1 (Mao et al., 2006) hand samples ICP-MS Tongkuangyu 171.6 3 1 Porphyry Cu 0 0.69 0.003 0 2092.5 (Mao et al., 1999) various various Tongkuangyu 1240 40 1 Porphyry Cu 0 0.69 0.003 0 2092.5 (Mao et al., 1999) various various Tongkuangyu 1280 20 1 Porphyry Cu 0 0.69 0.003 0 2092.5 (Mao et al., 1999) various various Tonglushan 261.4 2.2 1 Skarn Au-Cu granodiorite 1.15 0 1.15 137 (Xie et al., 2011) hand-picked grains ICP-MS Tonglushan 263.7 2.2 1 Skarn Au-Cu granodiorite 1.15 0 1.15 137 (Xie et al., 2011) hand-picked grains ICP-MS Tonglushan 305.7 2.5 1 Skarn Au-Cu granodiorite 1.15 0 1.15 137 (Xie et al., 2007) hand-picked magnetic concentrate ICP-MS Tonglushan 305.7 2.5 1 Skarn Au-Cu granodiorite 1.15 0 1.15 137 (Xie et al., 2011) hand-picked grains ICP-MS Tonglushan 432.5 3.7 1 Skarn Au-Cu granodiorite 1.15 0 1.15 137 (Xie et al., 2011) hand-picked grains ICP-MS Tonglushan 665.4 5.2 1 Skarn Au-Cu granodiorite 1.15 0 1.15 137 (Xie et al., 2007) hand-picked magnetic concentrate ICP-MS Tonglushan 665.4 5.2 1 Skarn Au-Cu granodiorite 1.15 0 1.15 137 (Xie et al., 2011) hand-picked grains ICP-MS Tongniujing 76.95 0.73 1 Quartz vein-hosted Cu-Au granite 0 0 0 138.2 (Mao et al., 2006) hand samples ICP-MS Tongniujing 77.32 0.4 1 Quartz vein-hosted Cu-Au granite 0 0 0 138.2 (Mao et al., 2006) hand samples ICP-MS Tongniujing 78.56 0.41 1 Quartz vein-hosted Cu-Au granite 0 0 0 138.2 (Mao et al., 2006) hand samples ICP-MS Tongniujing 78.61 0.88 1 Quartz vein-hosted Cu-Au granite 0 0 0 138.2 (Mao et al., 2006) hand samples ICP-MS Tongshankou 75.4 0.6 1 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Li et al., 2008) hand-picked grains ID-iCP-MS Tongshankou 84.6 0.6 1 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Li et al., 2008) hand-picked grains ID-iCP-MS Tongshankou 99.5 0.8 1 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Li et al., 2008) hand-picked grains ID-iCP-MS Tongshankou 110.6 0.8 1 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Li et al., 2008) hand-picked grains ID-iCP-MS Tongshankou 135.4 1 1 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Li et al., 2008) hand-picked grains ID-iCP-MS Tongshankou 175.7 1.4 1 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Xie et al., 2007) hand-picked magnetic concentrate ICP-MS Tongshankou 177 1.6 1 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Li et al., 2008) hand-picked grains ID-iCP-MS Tongshankou 178.3 1.6 1 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Xie et al., 2007) hand-picked magnetic concentrate ICP-MS Tongshankou 203.6 1.7 1 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Xie et al., 2007) hand-picked magnetic concentrate ICP-MS Tongshankou 224.3 1.7 1 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Xie et al., 2007) hand-picked magnetic concentrate ICP-MS Tongshankou 232.3 1.9 1 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Xie et al., 2007) hand-picked magnetic concentrate ICP-MS Tongshankou 235.2 1.8 1 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Xie et al., 2007) hand-picked magnetic concentrate ICP-MS Tongshankou 203.6 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Zhong et al., 2017) various various Tongshankou 224.3 Porphyry, skarn Cu-Mo diorite; granodiorite; quartz diorite 0.94 0.04 0 143.8 (Zhong et al., 2017) various various Topland 2.18 1 Unknown 0 0 0 0 0 (Schindler, 1975) various NAA Toquepala 387 1 Porphyry Cu 0 0.95 0.04 0 54.5 (Mathur et al., 2000) hand-picked grains NTIMS Toquepala 790 3 387 1496 Porphyry Cu 0 0.95 0.04 0 54.5 (Berzina et al., 2005) various various Toquepala 1495 1 Porphyry Cu 0 0.95 0.04 0 54.5 (Mathur et al., 2000) hand-picked grains NTIMS Travore 0.4088 0.0051 1 Quartz vein-hosted Mo granite 0 0 0 464 (Suzuki et al., 2001) hand-picked grains ID-ICP-MS Travore 0.467 0.026 1 Quartz vein-hosted Mo granite 0 0 0 464 (Suzuki et al., 2001) hand-picked grains ID-ICP-MS Tres Chorreras 35.29 3 1 Breccia pipe 0 0 0 3.4 19 (Schütte et al., 2012) concentrate, unknown method NTIMS Tres Chorreras 641 5 1 Breccia pipe 0 0 0 3.4 19 (Schütte et al., 2012) concentrate, unknown method NTIMS Trout Lake (Max) 49.89 0.19 1 Porphyry Mo granodiorite; tonalite 0 0.138 1.4 76 (Lawley and Selby, 2012) Mo powder NTIMS Trout Lake (Max) 54.67 0.26 1 Porphyry Mo granodiorite; tonalite 0 0.138 1.4 76 (Lawley and Selby, 2012) Mo powder NTIMS Trout Lake (Max) 56.26 0.21 1 Porphyry Mo granodiorite; tonalite 0 0.138 1.4 76 (Lawley and Selby, 2012) Mo powder NTIMS Trout Lake (Max) 56 Porphyry Mo granodiorite; tonalite 0 0.138 1.4 76 (Sinclair et al., 2009) various NAA Trout Lake (Max) 73 1 Porphyry Mo granodiorite; tonalite 0 0.138 1.4 76 (Sinclair et al., 2009) various NAA Tsagaan Suvarga 80 1 Porphyry Cu-Mo porphyry 0.53 0.018 0.084 370.4 (Watanabe and Stein, 2000) concentrate, unknown method NTIMS Tsagaan Suvarga 156 1 Porphyry Cu-Mo porphyry 0.53 0.018 0.084 370.4 (Watanabe and Stein, 2000) concentrate, unknown method NTIMS Tumen 0.0634 0.0002 1 Intrusion-related Mo 0 0 0.175 0 905.55 (Deng et al., 2013b) hand-picked magnetic concentrate ICP-MS Tumen 0.5482 0.0036 1 Intrusion-related Mo 0 0 0.175 0 905.55 (Deng et al., 2013b) hand-picked magnetic concentrate ICP-MS Tumen 0.66 0.0043 1 Intrusion-related Mo 0 0 0.175 0 905.55 (Deng et al., 2013b) hand-picked magnetic concentrate ICP-MS Tumen 22.615 0.2528 1 Intrusion-related Mo 0 0 0.175 0 905.55 (Deng et al., 2013b) hand-picked magnetic concentrate ICP-MS Tumen 23.6497 0.1822 1 Intrusion-related Mo 0 0 0.175 0 905.55 (Deng et al., 2013b) hand-picked magnetic concentrate ICP-MS Tumen 29.1473 0.2538 1 Intrusion-related Mo 0 0 0.175 0 905.55 (Deng et al., 2013b) hand-picked magnetic concentrate ICP-MS Tumen 30.9085 0.248 1 Intrusion-related Mo 0 0 0.175 0 905.55 (Deng et al., 2013b) hand-picked magnetic concentrate ICP-MS Tweedam 7.22 0.01 1 Quartz vein-hosted W granite 0 0 0 1019 (Raith and Stein, 2000) hand-picked magnetic concentrate NTIMS Tweedam 7.26 0.01 1 Quartz vein-hosted W granite 0 0 0 1019 (Raith and Stein, 2000) hand-picked magnetic concentrate NTIMS Tyrny-Auz 2 1 Skarn W-Mo 0 0 0 0 248 (Fleischer, 1959) flotation concentrate unknown Tyrny-Auz 3.2 1 Skarn W-Mo 0 0 0 0 248 (Fleischer, 1960) unknown colorimetry Tyrny-Auz 4 1 Skarn W-Mo 0 0 0 0 248 (Fleischer, 1959) flotation concentrate unknown Tyrny-Auz 10 1 Skarn W-Mo 0 0 0 0 248 (Fleischer, 1959) flotation concentrate unknown Uchitomi 0.1 1 Quartz vein-hosted granodiorite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Umal'ta 5 1 Quartz vein-hosted Mo granite 0 0 0 0 (Fleischer, 1959) flotation concentrate unknown Unkurtash 30 3 26 32 Porphyry Mo 0 0 0 0 0 (Berzina et al., 2005) various various Valeă Capişoara 29.03 0.04 1 Porphyry Cu 0 0 0 0 74.68 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Valley 288 1 Porphyry Cu diorite; granodiorite; quartz diorite 0.48 0.006 0.006 196 (Schindler, 1975) various NAA Valley 294 1 Porphyry Cu diorite; granodiorite; quartz diorite 0.48 0.006 0.006 196 (Sinclair et al., 2009) various NAA Valley 297 1 Porphyry Cu diorite; granodiorite; quartz diorite 0.48 0.006 0.006 196 (Schindler, 1975) various NAA Vårdal 25.11 0.02 1 Granite Mo 0 0 0 0 978 (Bingen et al., 2006) micro-drilled hand samples NTIMS Vårdal 35.2 0.03 1 Granite Mo 0 0 0 0 978 (Bingen et al., 2006) micro-drilled hand samples NTIMS Vardenis 16600 3 12200 18800 Porphyry Cu 0 0 0 0 0 (Berzina et al., 2005) various various Veliki Krivelj 301.8 0.8 1 Porphyry Cu-Mo 0 0.64 0.002 0.24 87.88 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Vidly 12 Intrusion-related Mo 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Vidly 17 Intrusion-related Mo 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Vidly 13 Intrusion-related Mo 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Vidly 12 Intrusion-related Mo 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Vidly 19 Intrusion-related Mo 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Vidly 17 Intrusion-related Mo 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Vidly 12 Intrusion-related Mo 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Vidly 20 Intrusion-related Mo 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Vidly 19 Intrusion-related Mo 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Vidly 15 Intrusion-related Mo 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Vidly 12 Intrusion-related Mo 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Vidly 13 Intrusion-related Mo 0 0 0 0 0 (Pasava et al., 2016) polished mounts LA-ICP-MS Vlaykov Vruh 161 0.3 1 Porphyry Cu granodiorite 0.46 0 0 87.235 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Vlaykov Vruh 341.9 0.4 1 Porphyry Cu granodiorite 0.46 0 0 87.235 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Vlaykov Vruh 1674.9 0.3 1 Porphyry Cu granodiorite 0.46 0 0 87.235 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Vlaykov Vruh 2055.2 0.6 1 Porphyry Cu granodiorite 0.46 0 0 87.235 (Zimmerman et al., 2008) micro-drilled hand samples TIMS Vrancice 13.5 0.040 1 Granite Mo granite 0 0 0 346.5 (Ackerman et al., 2017) hand-picked grains ICP-MS Vsestary 52 0.150 1 Quartz vein-hosted 0 0 0 0 0 (Ackerman et al., 2017) hand-picked grains ICP-MS Vulcan 11.032 0.035 1 IOCG breccia 0 0 0 1586 (Reid et al., 2013) micro-drilled hand samples NTIMS Vulcan 243 1.9 1 IOCG breccia 0 0 0 1586 (Reid et al., 2013) micro-drilled hand samples NTIMS Vulcan 279.1 1 1 IOCG breccia 0 0 0 1586 (Reid et al., 2013) micro-drilled hand samples NTIMS Vulcan 530.6 2.1 1 IOCG breccia 0 0 0 1586 (Reid et al., 2013) micro-drilled hand samples NTIMS Vulcan 653.3 2.5 1 IOCG breccia 0 0 0 1586 (Reid et al., 2013) micro-drilled hand samples NTIMS Wallaroo 17.5 1 IOCG Cu-Au (U-Mo) 0 0 0 0 255.7 (Riley, 1967) hand samples TIMS Wangdian 208.9 2.100 Porphyry Cu granodiorite 0.6 0.106 0 443.05 (Qiu et al., 2016a) concentrate, unknown method ICP-MS Wangdian 213.2 1.800 Porphyry Cu granodiorite 0.6 0.106 0 443.05 (Qiu et al., 2016a) concentrate, unknown method ICP-MS Wasadagawa 21 1 Granite Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Westonia 152 1 Orogenic Au tonalite 0 0 0 0 (Riley, 1967) hand samples TIMS Whiting Creek 13 1 Porphyry Cu-Mo granitoid; granodiorite 0.06 0.02 0 80.25 (Sinclair et al., 2009) various NAA Whiting Creek 92 2 Porphyry Cu-Mo granitoid; granodiorite 0.06 0.02 0 80.25 (Sinclair et al., 2009) various NAA Whiting Creek 172 1 Porphyry Cu-Mo granitoid; granodiorite 0.06 0.02 0 80.25 (Sinclair et al., 2009) various NAA Wilson's Downfall 10.2 1 Granite Sn-W granite 0 0 0 0 (Riley, 1967) hand samples TIMS Windhoek 1273 1 Unknown 0 0 0 0 521 (Golden et al., 2013) unknown unknown Wolfram Camp 0.24 1 Breccia pipe Mo-W-Bi granite 0 0 0 0 (Riley, 1967) hand samples TIMS Wolfram Camp 0.25 1 Breccia pipe Mo-W-Bi granite 0 0 0 0 (Riley, 1967) hand samples TIMS Wonbah 161 1 Breccia pipe Mo 0 0 0 0 0 (Riley, 1967) hand samples TIMS Wunugetushan 50.9 0.4 1 Porphyry Cu-Mo andesite; dacite; diorite; granite; monzogranite; quartz monzonite; rhyolite 0.45 0.085 0 163.5 (Mao et al., 1999) various various Wunugetushan 141.98 1 Porphyry Cu-Mo andesite; dacite; diorite; granite; monzogranite; quartz monzonite; rhyolite 0.45 0.085 0 163.5 (Chen et al., 2011) hand samples ICP-MS Wunugetushan 148.15 1 Porphyry Cu-Mo andesite; dacite; diorite; granite; monzogranite; quartz monzonite; rhyolite 0.45 0.085 0 163.5 (Chen et al., 2011) hand samples ICP-MS Wunugetushan 175.76 1 Porphyry Cu-Mo andesite; dacite; diorite; granite; monzogranite; quartz monzonite; rhyolite 0.45 0.085 0 163.5 (Chen et al., 2011) hand samples ICP-MS Wunugetushan 182.48 1 Porphyry Cu-Mo andesite; dacite; diorite; granite; monzogranite; quartz monzonite; rhyolite 0.45 0.085 0 163.5 (Chen et al., 2011) hand samples ICP-MS Wunugetushan 185.26 1 Porphyry Cu-Mo andesite; dacite; diorite; granite; monzogranite; quartz monzonite; rhyolite 0.45 0.085 0 163.5 (Chen et al., 2011) hand samples ICP-MS Wunugetushan 188.87 1 Porphyry Cu-Mo andesite; dacite; diorite; granite; monzogranite; quartz monzonite; rhyolite 0.45 0.085 0 163.5 (Chen et al., 2011) hand samples ICP-MS Wunugetushan 368.79 1 Porphyry Cu-Mo andesite; dacite; diorite; granite; monzogranite; quartz monzonite; rhyolite 0.45 0.085 0 163.5 (Chen et al., 2011) hand samples ICP-MS Wunugetushan 230.1 1 Porphyry Cu-Mo granite, monzogranite 0.46 0.053 180.5 (Wang et al., 2015) hand-picked magnetic concentrate ID-ICP-MS Wunugetushan 203.5 1 Porphyry Cu-Mo granite, monzogranite 0.46 0.053 180.5 (Wang et al., 2015) hand-picked magnetic concentrate ID-ICP-MS Wunugetushan 118.9 1 Porphyry Cu-Mo granite, monzogranite 0.46 0.053 180.5 (Wang et al., 2015) hand-picked magnetic concentrate ID-ICP-MS Wunugetushan 301.5 1 Porphyry Cu-Mo granite, monzogranite 0.46 0.053 180.5 (Wang et al., 2015) hand-picked magnetic concentrate ID-ICP-MS Wunugetushan 141.7 1 Porphyry Cu-Mo granite, monzogranite 0.46 0.053 180.5 (Wang et al., 2015) hand-picked magnetic concentrate ID-ICP-MS Wunugetushan 139.1 1 Porphyry Cu-Mo granite, monzogranite 0.46 0.053 180.5 (Wang et al., 2015) hand-picked magnetic concentrate ID-ICP-MS Xamchab 700 400 1 Pegmatite Mo granite; leucogranite 0 0 0 0 (McCandless et al., 1993) hand-picked grains EPMA Xamchab 1400 600 1 Pegmatite Mo granite; leucogranite 0 0 0 0 (McCandless et al., 1993) hand-picked grains EPMA Xamchab 1600 400 1 Pegmatite Mo granite; leucogranite 0 0 0 0 (McCandless et al., 1993) hand-picked grains EPMA Xamchab 1800 700 1 Pegmatite Mo granite; leucogranite 0 0 0 0 (McCandless et al., 1993) hand-picked grains EPMA Xiaobaishitou 57.97 0.430 Skarn W granite 0 0 0 241 (Deng et al., 2017) hand-picked magnetic concentrate ICP-MS Xiaobaishitou 44.12 0.330 Skarn W granite 0 0 0 241 (Deng et al., 2017) hand-picked magnetic concentrate ICP-MS Xiaobaishitou 40.33 0.310 Skarn W granite 0 0 0 241 (Deng et al., 2017) hand-picked magnetic concentrate ICP-MS Xiaobaishitou 41.77 0.330 Skarn W granite 0 0 0 241 (Deng et al., 2017) hand-picked magnetic concentrate ICP-MS Xiaobaishitou 55.39 0.450 Skarn W granite 0 0 0 241 (Deng et al., 2017) hand-picked magnetic concentrate ICP-MS Xiaobaishitou 64.67 0.510 Skarn W granite 0 0 0 241 (Deng et al., 2017) hand-picked magnetic concentrate ICP-MS Xiaobaishitou 55.66 0.460 Skarn W granite 0 0 0 241 (Deng et al., 2017) hand-picked magnetic concentrate ICP-MS Xiaodonggou 4.558 0.049 1 Porphyry Mo granite 0 0 0 138.1 (Zeng et al., 2010) unknown ICP-MS Xiaodonggou 6.005 0.063 1 Porphyry Mo granite 0 0 0 138.1 (Zeng et al., 2010) unknown ICP-MS Xiaodonggou 7.528 0.068 1 Porphyry Mo granite 0 0 0 138.1 (Zeng et al., 2010) unknown ICP-MS Xiaodonggou 7.635 0.06 1 Porphyry Mo granite 0 0 0 138.1 (Zeng et al., 2010) unknown ICP-MS Xiaodonggou 8.382 0.066 1 Porphyry Mo granite 0 0 0 138.1 (Zeng et al., 2010) unknown ICP-MS Xiaodonggou 8.418 0.084 1 Porphyry Mo granite 0 0 0 138.1 (Zeng et al., 2010) unknown ICP-MS Xiaojiayingzi 21.75 0.26 1 Skarn Mo 0 0 0 0 0 (Dai et al., 2009) hand-picked magnetic concentrate ICP-MS Xiaojiayingzi 37.08 0.38 1 Skarn Mo 0 0 0 0 0 (Dai et al., 2009) hand-picked magnetic concentrate ICP-MS Xiaojiayingzi 37.92 0.62 1 Skarn Mo 0 0 0 0 0 (Dai et al., 2009) hand-picked magnetic concentrate ICP-MS Xiaojiayingzi 42.39 0.5 1 Skarn Mo 0 0 0 0 0 (Dai et al., 2009) hand-picked magnetic concentrate ICP-MS Xiaojiayingzi 83.74 1.1 1 Skarn Mo 0 0 0 0 0 (Dai et al., 2009) hand-picked magnetic concentrate ICP-MS Xiaojiayingzi 163 2.1 1 Skarn Mo 0 0 0 0 0 (Dai et al., 2009) hand-picked magnetic concentrate ICP-MS Xiaoliugou 0.76 0.3 1 Skarn W granodiorite 0 0 0 465.2 (Mao et al., 1999) various various Xiaoliugou 1.68 0.02 1 Skarn W granodiorite 0 0 0 465.2 (Mao et al., 1999) various various Xiaoliugou 2.27 0.02 1 Quartz vein-hosted W granodiorite 0 0 0 465.2 (Mao et al., 1999) various various Xiaoliugou 4.97 0.04 1 Quartz vein-hosted W granodiorite 0 0 0 465.2 (Mao et al., 1999) various various Xiaoliugou 8.74 0.27 1 Quartz vein-hosted W granodiorite 0 0 0 465.2 (Mao et al., 1999) various various Xiaoshigou 37.14 0.5 1 Porphyry, skarn Mo granite 0 0 0 135.5 (Mao et al., 1999) various various Xifanping 9.4 1 Porphyry Cu-Mo quartz monzonite 0.28 0 0.31 32.1 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Xifanping 88.4 1 Porphyry Cu-Mo quartz monzonite 0.28 0 0.31 32.1 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Xifanping 117.3 1 Porphyry Cu-Mo quartz monzonite 0.28 0 0.31 32.1 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Xifanping 220.8 1 Porphyry Cu-Mo quartz monzonite 0.28 0 0.31 32.1 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Xifanping 380.5 1 Porphyry Cu-Mo quartz monzonite 0.28 0 0.31 32.1 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Xin'an 11 6 3.6 17.6 Porphyry Mo granite 0 0.1 0 168.3 (Zhong et al., 2017) various various Xincun 31.15 0.120 Porphyry Mo rhyolite porphyry, monzogranite, granite 0 0.09 0 97.7 (Xu et al., 2016) unknown unknown Xincun 27.25 0.170 Porphyry Mo rhyolite porphyry, monzogranite, granite 0 0.09 0 97.7 (Xu et al., 2016) unknown unknown Xincun 14.56 0.070 Porphyry Mo rhyolite porphyry, monzogranite, granite 0 0.09 0 97.7 (Xu et al., 2016) unknown unknown Xincun 99.67 0.690 Porphyry Mo rhyolite porphyry, monzogranite, granite 0 0.09 0 97.7 (Xu et al., 2016) unknown unknown Xincun 13.41 0.060 Porphyry Mo rhyolite porphyry, monzogranite, granite 0 0.09 0 97.7 (Xu et al., 2016) unknown unknown Xincun 5.49 0.020 Porphyry Mo rhyolite porphyry, monzogranite, granite 0 0.09 0 97.7 (Xu et al., 2016) unknown unknown Xingluokeng 3.9 5 2.9 4.3 Porphyry Mo-W granite 0 0.023 0 156.3 (Zhong et al., 2017) various various Xingshan 20.026 1 Porphyry Mo monzogranite, granodiorite 0.116 167.3 (Zhou et al., 2013) hand-picked magnetic concentrate ICP-MS Xingshan 20.363 1 Porphyry Mo monzogranite, granodiorite 0.116 167.3 (Zhou et al., 2013) hand-picked magnetic concentrate ICP-MS Xiongcun 7656.5 Porphyry Cu-Au quartz diorite 0.4 0 0.4 161.5 (Lang et al., 2014) hand samples NTIMS - ICP-MS Xiongcun 3191.1 Porphyry Cu-Au quartz diorite 0.4 0 0.4 161.5 (Lang et al., 2014) hand samples NTIMS - ICP-MS Xiongcun 3316.6 Porphyry Cu-Au quartz diorite 0.4 0 0.4 161.5 (Lang et al., 2014) hand samples NTIMS - ICP-MS Xiongcun 6135 Porphyry Cu-Au quartz diorite 0.4 0 0.4 161.5 (Lang et al., 2014) hand samples NTIMS - ICP-MS Xiongcun 1048.4 Porphyry Cu-Au quartz diorite 0.4 0 0.4 161.5 (Lang et al., 2014) hand samples NTIMS - ICP-MS Xiongcun 1014.8 Porphyry Cu-Au quartz diorite 0.4 0 0.4 161.5 (Lang et al., 2014) hand samples NTIMS - ICP-MS Xiongcun 1029 Porphyry Cu-Au quartz diorite 0.4 0 0.4 161.5 (Lang et al., 2014) hand samples NTIMS - ICP-MS Xiongcun 1346.6 Porphyry Cu-Au quartz diorite 0.4 0 0.4 161.5 (Lang et al., 2014) hand samples NTIMS - ICP-MS Xiongcun 1268.7 Porphyry Cu-Au quartz diorite 0.4 0 0.4 161.5 (Lang et al., 2014) hand samples NTIMS - ICP-MS Xiongcun 1354.1 Porphyry Cu-Au quartz diorite 0.4 0 0.4 161.5 (Lang et al., 2014) hand samples NTIMS - ICP-MS Xiongcun 1293.4 Porphyry Cu-Au quartz diorite 0.4 0 0.4 161.5 (Lang et al., 2014) hand samples NTIMS - ICP-MS Xiongjiashan 0.4 5 0.2 0.6 Quartz vein-hosted Mo granite 0 0.14 0 152 (Zhong et al., 2017) various various Xitian 8.67401 0.023 Skarn Sn-W granite 0 0 0 150.3 (Liang et al., 2016) hand-picked grains ICP-MS Xitian 18.5982 0.056 Skarn Sn-W granite 0 0 0 150.3 (Liang et al., 2016) hand-picked grains ICP-MS Xitian 41.9488 0.174 Skarn Sn-W granite 0 0 0 150.3 (Liang et al., 2016) hand-picked grains ICP-MS Xitian 43.9859 0.224 Skarn Sn-W granite 0 0 0 150.3 (Liang et al., 2016) hand-picked grains ICP-MS Xitian 39.1277 0.121 Skarn Sn-W granite 0 0 0 150.3 (Liang et al., 2016) hand-picked grains ICP-MS Yakuoji 210 1 Quartz vein-hosted Cu granodiorite 0 0 0 0 (Terada et al., 1971) hand-picked grains NAA Yamasa 200 1 Quartz vein-hosted granite 0 0 0 60.6 (Terada et al., 1971) hand-picked grains NAA Yamasa 162.4 1.4 Quartz vein-hosted granite 0 0 0 60.6 (Suzuki et al., 1996) hand samples ID-ICP-MS Yamasa 163.9 1.2 Quartz vein-hosted granite 0 0 0 60.6 (Suzuki et al., 1996) hand samples ID-ICP-MS Yamasa 167.5 1.8 Quartz vein-hosted granite 0 0 0 60.6 (Suzuki et al., 1996) hand samples ID-ICP-MS Yamasa 110 4 100 200 Quartz vein-hosted granite 0 0 0 60.6 (Terada et al., 1971) hand-picked grains NAA Yamasa 198 5 Quartz vein-hosted granite 0 0 0 60.6 (Ishihara, 1988) various NAA/spectrophotometry Yamato 89 1 Skarn Cu quartz diorite; dacite 0 0 0 14.181 (Terada et al., 1971) hand-picked grains NAA Yamato 140 1 Skarn Cu quartz diorite; dacite 0 0 0 14.181 (Ishihara, 1988) various NAA/spectrophotometry Yamatsuri 1 1 Granite Mo granite 0 0 0 0 (Ishihara, 1988) various NAA/spectrophotometry Yangakly 1800 3 1600 2000 Porphyry Cu 0 0 0 0 0 (Berzina et al., 2005) various various Yaochong 42.5 1 Porphyry Mo monzogranite 0 0.088 0 133 (Chen et al., 2015) hand-picked magnetic concentrate ICP-MS Yaochong 43.8 1 Porphyry Mo monzogranite 0 0.088 0 133 (Chen et al., 2015) hand-picked magnetic concentrate ICP-MS Yaochong 74.8 1 Porphyry Mo monzogranite 0 0.088 0 133 (Chen et al., 2015) hand-picked magnetic concentrate ICP-MS Yaochong 35.5 1 Porphyry Mo monzogranite 0 0.088 0 133 (Chen et al., 2015) hand-picked magnetic concentrate ICP-MS Yaochong 21.8 1 Porphyry Mo monzogranite 0 0.088 0 133 (Chen et al., 2015) hand-picked magnetic concentrate ICP-MS Yaogangxian 0.01016 1 Quartz vein-hosted W granite 0 0 0 154.9 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Yaogangxian 0.05436 0.00068 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 0.059 0.0012 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 0.09887 0.00093 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 0.1003 0.0012 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 0.1311 0.0016 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 0.3919 0.0037 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 0.4073 0.0049 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 0.4507 0.004 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 0.4895 0.0048 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 0.9025 0.008 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 1 0.008 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 1.056 0.01 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 1.306 0.013 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 1.632 0.015 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 4.334 1 Quartz vein-hosted W granite 0 0 0 154.9 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Yaogangxian 4.334 0.044 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 4.909 0.056 1 Quartz vein-hosted W granite 0 0 0 154.9 (Wang et al., 2008) hand-picked heavy liquid concentrate ICP-MS Yaogangxian 0.01016 0.002 1 Quartz vein-hosted W granite 0 0 0 154.9 (Peng et al., 2006) hand-picked magnetic concentrate ICP-MS Yaogangxian 0.03838 0.0099 1 Quartz vein-hosted W granite 0 0 0 154.9 (Peng et al., 2006) hand-picked magnetic concentrate ICP-MS Yaogangxian 0.05948 0.0105 1 Quartz vein-hosted W granite 0 0 0 154.9 (Peng et al., 2006) hand-picked magnetic concentrate ICP-MS Yaogangxian 0.06903 0.0294 1 Quartz vein-hosted W granite 0 0 0 154.9 (Peng et al., 2006) hand-picked magnetic concentrate ICP-MS Yaogangxian 0.561 0.0151 1 Quartz vein-hosted W granite 0 0 0 154.9 (Peng et al., 2006) hand-picked magnetic concentrate ICP-MS Yaogangxian 0.7678 0.0186 1 Quartz vein-hosted W granite 0 0 0 154.9 (Peng et al., 2006) hand-picked magnetic concentrate ICP-MS Yaogangxian 1.665 0.06 1 Quartz vein-hosted W granite 0 0 0 154.9 (Peng et al., 2006) hand-picked magnetic concentrate ICP-MS Yaogangxian 2.618 0.057 1 Quartz vein-hosted W granite 0 0 0 154.9 (Peng et al., 2006) hand-picked magnetic concentrate ICP-MS Yaolanzai 0.02967 0.00032 1 Greisen W-Sn 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Yaolanzai 0.02967 1 Greisen W-Sn 0 0 0 0 0 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Yaolanzai 0.05078 0.00046 1 Greisen W-Sn 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Yaolanzai 0.06224 0.00046 1 Greisen W-Sn 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Yaolanzai 0.07875 0.00066 1 Greisen W-Sn 0 0 0 0 0 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Yaolanzai 0.07875 1 Greisen W-Sn 0 0 0 0 0 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Yea 695 1 Granite Mo-W 0 0 0 0 0 (Riley, 1967) hand samples TIMS Yetholme 60.7 1 Skarn Mo-W 0 0 0 0 0 (Schindler, 1975) various NAA Yetholme 61.1 1 Skarn Mo-W 0 0 0 0 0 (Schindler, 1975) various NAA Yetholme 61.7 1 Skarn Mo-W 0 0 0 0 0 (Schindler, 1975) various NAA Yetholme 65 1 Skarn Mo-W 0 0 0 0 0 (Riley, 1967) hand samples TIMS Yetholme 66 1 Skarn Mo-W 0 0 0 0 0 (Riley, 1967) hand samples TIMS Yetholme 66.3 1 Skarn Mo-W 0 0 0 0 0 (Schindler, 1975) various NAA Yetholme 66.5 1 Skarn Mo-W 0 0 0 0 0 (Schindler, 1975) various NAA Yetholme 71 1 Skarn Mo-W 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Yetholme 129 1 Skarn Mo-W 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Yetholme 128 Skarn Mo-W 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Yetholme 63 Skarn Mo-W 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Yetholme 65 Skarn Mo-W 0 0 0 0 0 (Morgan et al., 1968) hand-picked heavy liquid concentrate NAA Yinachang 5.71 0.02 1 IOCG 0 0 0 0 730.95 (Zhao et al., 2013) hand-picked magnetic/heavy liquids concentrate ID-NTIMS Yinachang 71.9 0.24 1 IOCG 0 0 0 0 730.95 (Zhao et al., 2013) hand-picked magnetic/heavy liquids concentrate ID-NTIMS Yinachang 79.1 0.32 1 IOCG 0 0 0 0 730.95 (Zhao et al., 2013) hand-picked magnetic/heavy liquids concentrate ID-NTIMS Yinachang 91.4 0.46 1 IOCG 0 0 0 0 730.95 (Zhao et al., 2013) hand-picked magnetic/heavy liquids concentrate ID-NTIMS Yinachang 93.2 0.45 1 IOCG 0 0 0 0 730.95 (Zhao et al., 2013) hand-picked magnetic/heavy liquids concentrate ID-NTIMS Yinyan 0.1324 0.001 Porphyry Sn granite, monzogranite 0 0 0 78.8 (Zheng et al., 2015) hand samples ICP-MS Yinyan 0.9694 0.008 Porphyry Sn granite, monzogranite 0 0 0 78.8 (Zheng et al., 2015) hand samples ICP-MS Yinyan 1.273 0.004 Porphyry Sn granite, monzogranite 0 0 0 78.8 (Zheng et al., 2015) hand samples ICP-MS Yinyan 0.5782 0.002 Porphyry Sn granite, monzogranite 0 0 0 78.8 (Zheng et al., 2015) hand samples ICP-MS Ylitornio 61.7 1 Sui generis 0 0 0 0 1770 (Luck and Allègre, 1982) unknown ID-ion probe Yuanzhuding 92 11 2.7 449.4 Porphyry Cu-Mo monzogranite 0.18 0.045 0 155.6 (Zhong et al., 2017) various various Yulong 290.5 1 Porphyry Cu-Mo granite; monzogranite 0.94 0.022 0.35 41.3 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Yulong 387 1 Porphyry Cu-Mo granite; monzogranite 0.94 0.022 0.35 41.3 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Yulong 433 1 Porphyry Cu-Mo granite; monzogranite 0.94 0.022 0.35 41.3 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Yulong 664.5 1 Porphyry Cu-Mo granite; monzogranite 0.94 0.022 0.35 41.3 (Hou et al., 2006) hand-picked heavy liquid concentrate ICP-MS Zappa-Koffee 287.8 2.8 1 Porphyry Cu-Mo 0 0 0 0 0 (Selby and Creaser, 2001a) hand-picked magnetic/heavy liquids concentrate NTIMS Zappa-Koffee 765.2 35.3 1 Porphyry Cu-Mo 0 0 0 0 0 (Selby and Creaser, 2001a) hand-picked magnetic/heavy liquids concentrate NTIMS Zhaiwa 1.047 0.019 1 Porphyry Cu-Mo granite 0 0 0 1761 (Deng et al., 2013a) hand-picked magnetic concentrate ICP-MS Zhaiwa 1.945 0.013 1 Porphyry Cu-Mo granite 0 0 0 1761 (Deng et al., 2013a) hand-picked magnetic concentrate ICP-MS Zhaiwa 3.686 0.086 1 Porphyry Cu-Mo granite 0 0 0 1761 (Deng et al., 2013a) hand-picked magnetic concentrate ICP-MS Zhaiwa 6.76 0.113 1 Porphyry Cu-Mo granite 0 0 0 1761 (Deng et al., 2013a) hand-picked magnetic concentrate ICP-MS Zhaiwa 31.567 0.515 1 Porphyry Cu-Mo granite 0 0 0 1761 (Deng et al., 2013a) hand-picked magnetic concentrate ICP-MS Zhaiwa 42.993 0.725 1 Porphyry Cu-Mo granite 0 0 0 1761 (Deng et al., 2013a) hand-picked magnetic concentrate ICP-MS Zhanet 9.099 0.076 1 Greisen 0 0 0 0 294.95 (Chen et al., 2010) hand samples ICP-MS Zhanet 9.664 0.128 1 Greisen 0 0 0 0 294.95 (Chen et al., 2010) hand samples ICP-MS Zhanet 15.25 0.14 1 Greisen 0 0 0 0 294.95 (Chen et al., 2010) hand samples ICP-MS Zhangdou 0.2078 0.0017 1 Quartz vein-hosted W 0 0 0 0 149.1 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Zhangdou 0.2078 1 Quartz vein-hosted W 0 0 0 0 149.1 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Zhangdou 0.2518 0.0019 1 Quartz vein-hosted W 0 0 0 0 149.1 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Zhangdou 0.3713 0.0028 1 Quartz vein-hosted W 0 0 0 0 149.1 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Zhangdou 0.372 0.0029 1 Quartz vein-hosted W 0 0 0 0 149.1 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Zhangdou 0.4263 0.0035 1 Quartz vein-hosted W 0 0 0 0 149.1 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Zhangdou 0.5232 1 Quartz vein-hosted W 0 0 0 0 149.1 (Guo et al., 2011) hand-picked magnetic concentrate ICP-MS Zhangdou 0.5232 0.004 1 Quartz vein-hosted W 0 0 0 0 149.1 (Feng et al., 2011) hand-picked magnetic concentrate ICP-MS Zhifang 25.85 0.120 Quartz vein-hosted Mo 0 0 0 0 246 (Deng et al., 2015) hand-picked magnetic concentrate ICP-MS Zhifang 3.984 0.024 Quartz vein-hosted Mo 0 0 0 0 246 (Deng et al., 2015) hand-picked magnetic concentrate ICP-MS Zhifang 3.984 0.026 Quartz vein-hosted Mo 0 0 0 0 246 (Deng et al., 2015) hand-picked magnetic concentrate ICP-MS Zhifang 29.85 0.170 Quartz vein-hosted Mo 0 0 0 0 246 (Deng et al., 2015) hand-picked magnetic concentrate ICP-MS Zhifang 8.18 0.022 Quartz vein-hosted Mo 0 0 0 0 246 (Deng et al., 2015) hand-picked magnetic concentrate ICP-MS Zhilingtou 27.5 5 14.5 58.6 Porphyry Mo granite 0 0.07 0 110.1 (Zhong et al., 2017) various various Zhireken 12 1 Porphyry Cu-Mo diorite; granite; granodiorite 0.1 0.099 0.03 157.5 (Berzina et al., 2005) various various Zhireken 17 1 Porphyry Cu-Mo diorite; granite; granodiorite 0.1 0.099 0.03 157.5 (Berzina et al., 2005) various various Zhireken 20 1 Porphyry Cu-Mo diorite; granite; granodiorite 0.1 0.099 0.03 157.5 (Berzina et al., 2005) various various Zhireken 21 1 Porphyry Cu-Mo diorite; granite; granodiorite 0.1 0.099 0.03 157.5 (Berzina et al., 2005) various various Zhireken 35 1 Porphyry Cu-Mo diorite; granite; granodiorite 0.1 0.099 0.03 157.5 (Berzina et al., 2005) various various Zhireken 39 1 Porphyry Cu-Mo diorite; granite; granodiorite 0.1 0.099 0.03 157.5 (Berzina et al., 2005) various various Zhireken 57 1 Porphyry Cu-Mo diorite; granite; granodiorite 0.1 0.099 0.03 157.5 (Berzina et al., 2005) various various Zhuonuo 227.15 Porphyry Mo monzogranite 0 0 0 13.17 (Wang et al., 2016) hand samples MC-ICP-MS Zhuonuo 312.11 Porphyry Mo monzogranite 0 0 0 13.17 (Wang et al., 2016) hand samples MC-ICP-MS Zhuonuo 292.99 Porphyry Mo monzogranite 0 0 0 13.17 (Wang et al., 2016) hand samples MC-ICP-MS Zhuxi 889.9 1 Skarn W-Cu granite 0.8 0 0 150 (Pan et al., 2017) hand-picked heavy liquid concentrate ICP-MS Zhuxi 107.3 1 Skarn W-Cu granite 0.8 0 0 150 (Pan et al., 2017) hand-picked heavy liquid concentrate ICP-MS Zhuxi 47.35 1 Skarn W-Cu granite 0.8 0 0 150 (Pan et al., 2017) hand-picked heavy liquid concentrate ICP-MS Zhuxi 109.1 1 Skarn W-Cu granite 0.8 0 0 150 (Pan et al., 2017) hand-picked heavy liquid concentrate ICP-MS Zhuxi 103.5 1 Skarn W-Cu granite 0.8 0 0 150 (Pan et al., 2017) hand-picked heavy liquid concentrate ICP-MS Appendix B

Citation Reference (Ackerman et al., 2017) Ackerman, L., Haluzova, E., Creaser, R., Pasava, J., Veselovsky, F., Breiter, K., Erban, V., and Drabek, M., 2017, Temporal evolution of mineralization events in the Boheman Massif inferred from the Re-Os geochronology of molybdenite. Mineralium Deposita 52: 651-662. (Aghazadeh et al., 2015) Aghazadeh, M., Hou, Z.Q., Badrzadeh, Z., and Zhou, L., 2015, Temporal–spatial distribution and tectonic setting of porphyry copper deposits in Iran: Constraints from zircon U–Pb and molybdenite Re–Os geochronology: Ore Geology Reviews, v. 70, p. 385–406. (Ahmed et al., 2009) Ahmed, A.H. and Arai, S., and Ikenne, M., 2009, Mineralogy and paragenesis of the Co-Ni arsenide ores of Bou Azzer, Anti-Atlas, Morocco: Economic Geology, v. 104, p. 249–266. (Aminzadeh et al., 2011) Aminzadeh, B. and Shahabpour, J., and Maghami, M., 2011, Variation of rhenium contents in molybdenites from the Sar Cheshmeh porphyry Cu–Mo deposit in Iran: Resource Geology, v. 61, p. 290–295. (Arancibia and Clark, 1996) Arancibia, O.N. and Clark, A.H., 1996, Early magnetite–amphibole–plagioclase alteration-mineralization in the Island copper porphyry copper–gold–molybdenum deposit, British Columbia: Economic Geology, v. 91, p. 402–438. (Arne et al., 1998) Arne, D.C., Bierlein, F.P,, McNaughton, N.J., Wilson, C.J.L., and Morand, V.J., 1998, Timing of gold mineralisation in western and central Victoria, Australia: New constraints from SHRIMP II analysis of zircon grains from felsic intrusive rocks: Ore Geology Reviews, v. 13, p. 251–273. (Arne et al., 2001) Arne, D.C., Bierlin, F.P., Morgan, J.W., and Stein, H.J., 2001, Re–Os dating of sulfides associated with gold mineralization in central Victoria, Australia: Economic Geology, v. 96, p. 1455–1459. (Babo et al., 2017) Babo, J., Spandler, C., Oliver, N., Brown, M., Rubenach, M., and Creaser, R., 2017, The high-grade Mo-Re Merlin deposit, Cloncurry district, Australia: Paragenesis and geochronology of hydrothermal alteration and ore formation. Economic Geology 112: 397-422. (Barra et al., 2003) Barra, F., Ruiz, J., Mathur, R.D., and Titley, S.R., 2003, A Re–Os study of sulfide minerals from the Bagdad porphyry Cu–Mo deposit, northern Arizona, USA: Minerallium Deposita, v. 38, p. 585–596. (Barra et al., 2005) Barra, F., Ruiz, J., Valencia, V.A., Ochoa-Landín, L., Chesley, J.T., and Zürcher, L., 2005, Laramide porphyry Cu–Mo mineralization in northern Mexico: Age constraints from Re–Os geochronology in molybdenite: Economic Geology, 100th Anniversary Volume, p. 1605–1616. (Barra, 2005) Barra, F., 2005, Applications of the Re–Os isotopic system in the study of mineral deposits: geochronology and source of metals: Unpublished Ph.D. Dissertation, University of Arizona, Tucson, 211 p. (Basitova, 1950) Basitova, S.M., 1950, Geochemistry of rhenium: Ph.D. dissertation, Vernadskii Institue of Geochemistry and Analytical Chemistry, Moscow. (Berger et al., 2010) Berger, B.R., Mars, J.L., Denning, P.D., Philips, J.D., Hammarstrom, J.M., , et al., 2010, Global mineral resource assessment: porphyry copper assessment of Western Central Asia: U.S. Geological Survey Scientific Investigations Report 2010-5090-N, 219 p. (Bernard et al., 1990) Bernard, A. and Symonds, R.B., and Rose, W.I.J., 1990, Volatile transport and deposition of Mo, W, Re in high temperature magmatic fluids: Applied Geochemistry, v. 5, p. 317–326. (Berzina et al., 2005) Berzina, A.N., Sotnikov, V.I., Economou-Eliopoulos, M., and Eliopoulos, D.G., 2005, Distribution of rhenium in molybdenite from porphyry Cu–Mo and Mo–Cu deposits of Russia (Siberia) and Mongolia: Ore Geology Reviews, v. 26, p. 91–113. (Bineli Betsi et al., 2013) Bineli Betsi, T., Lentz, D.R., Chiaradia, M., Kyser, K., and Creaser, R.A., 2013, Genesis of the Au–Bi–Cu–As, Cu–Mo±W, and base-metal Au–Ag mineralization at the Mountain Freegold (Yukon, Canada): constraints from Ar–Ar and Re–Os geochronology and Pb and stable isotope compositions: Minerallium Deposita, v. 48, p. 991–1017. (Bingen and Stein, 2002) Bingen, B., and Stein, H., 2002, 1.05-1.1 Ga Sveconorwegian metamorphism and deformation of the supracrustal sequence and Saesvatn, South Norway: Re-Os dating of Cu-Mo mineral occurrences. GSL Special Publication 204: 319-335. (Bingen and Stein, 2003) Bingen, B. and Stein, H.J., 2003, Molybdenite Re–Os dating of biotite dehydration melting in the Rogaland high-temperature granulites, S Norway: Earth and Planetary Science Letters, v. 208, p. 181–195. (Bingen et al., 2006) Bingen, B., Stein, H.J., Bogaerts, M., Bolle, O., and Mansfeld, J., 2006, Molybdenite Re–Os dating constrains gravitational collapse of the Sveconorwegian orogen, SW Scandinavia: Lithos, v. 87, p. 328–346. (Boliden AB, 2015) Boliden AB, 2015, Annual Report 2014, 122 p., http://investors.boliden.com/files/press/boliden/Boliden_ar14_2015-03-10_ENG.pdf (Boni et al., 2003) Boni, M., Stein, H.J., Zimmerman, A., and Villa, I.M., 2003, Re-Os age for molybdenite from SW Sardinia (Italy): a comparison with 40Ar/39Ar dating of Variscan granitoids, in Eliopoulos et al., ed., Mineral exploration and sustainable development: Millpress, p. 247–250. (Boni et al., 2003) Boni, M., Stein, H., Zimmerman, A., and Villa, I., 2003. Re-Os age for molybdenite from SW Sardinia (Italy): A comparison with 40Ar/39Ar dating of Variscan granitoids. Mineral Exploration and Sustainable Development , 247-250. (Brooks et al., 2004) Brooks, C.K., Tegner, C., Stein, H.J., and Thomassen, B., 2004, Re–Os and 40Ar/39Ar ages of porphyry molybdenum deposits in the East Greenland volcanic-rifted margin: Economic Geology, v. 99, p. 1215–1222. (Brown et al., 2002) Brown, S.M., Fletcher, I.R., Stein, H.J., Snee, L.W., and Groves, D.I., 2002, Geochronological constraints on pre-, syn-, and postmineralization events at the world-class Cleo gold deposit, eastern Goldfields Province, Western Australia: Economic Geology, v. 97, p. 541–559. (Bucci et al., 2004) Bucci, L.A., McNaughton, N.J., Fletcher, I.R., Groves, D.I., Kositcin, N., Stein, H.J., et al., 2004, Timing and duration of high-temperature gold mineralization and spatially associated granitoid magmatism at Chalice, Yilgarn Craton, Western Australia: Economic Geology, v. 99, p. 1123–1144. (C. Leng et al., 2015) Leng, C., Zhang, X., Huang, Z., Huang, Q, Wang, S., Ma, D., Luo, T., Li, C., and Li, W., 2015, Geology, Re-Os ages, sulfur and lead isotopes of the Diyanqinamu porphyry Mo deposit, Inner Mongolia, NE China. Economic Geology 110: 557-574. (Chen and Zhou, 2012) Chen, W.T. and Zhou, M.F., 2012, Paragenesis, stable isotopes, and molybdenite Re–Os isotope age of the Lala iron-copper deposit, Southwest China: Economic Geology, v. 107, p. 459–480. (Chen et al., 2010) Chen, X.H., Qu, W.J., Han, S.Q., Eleonora, S., Yang, N., Chen, Z.L., et al., 2010, Re–Os geochronology of Cu and W–Mo deposits in the Balkhash metallogenic belt, Kazakhstan and its geological significance: Geoscience Frontiers, v. 1, p. 115–124. (Chen et al., 2011) Chen, Z.G., Zhang, L.C., Wan, B., Wu, H.Y., and Cleven, N., 2011, Geochronology and geochemistry of the Wunugetushan porphyry Cu–Mo deposit in NE china, and their geological significance: Ore Geology Reviews, v. 43, p. 92–105. (Chen et al., 2015) Chen, W., Xu, Z., Qiu, W., Li, C., Yu, Y., Wang, H., and Su, Y., 2015, Petrogenesis of the Yaochong granite and Mo deposit, Western Dabie orogen, eastern-central China: Constraints from zircon U-Pb and molybdenite Re-Os ages, whole-rock geochemistry and Sr-Nd-Pb-Hf isotopes. Journal of Asian Earth Sciences 103: 198-211. (Cheng et al., 2012) Cheng, Y.B., Mao, J.W., Rusk, B., and Yang, Z., 2012, Geology and genesis of Kafang Cu–Sn deposit, Gejiu district, SW China: Ore Geology Reviews, v. 48, p. 180–196. (Chiaradia et al., 2009) Chiaradia, M., Vallance, J., Fontboté, L., Stein, H.J., Schaltegger, U., Coder, J., et al., 2009, U–Pb, Re–Os, and 40Ar/39Ar geochronology of the Nambija Au–skarn and Pangui porphyry Cu deposits, Ecuador: implications for the Jurassic metallogenic belt of the northern Andes: Minerallium Deposita, v. 44, p. 371–387. (Ciobanu et al., 2002) Ciobanu, C.L. and Cook, N.J., and Stein, H.J., 2002, Regional setting and geochronology of the Late Cretaceous Banatitic Magmatic and Metallogenetic Belt: Minerallium Deposita, v. 37, p. 541–567. (Ciobanu et al., 2013) Ciobanu, C.L., Cook, N.J., Kelson, C.R., Guerin, R., Kalleske, N., and Danyushevsky, L., 2013, Trace element heterogeneity in molybdenite fingerprints stages of mineralization: Chemical Geology, v. 347, p. 175–189. (Cline, 2001) Cline, J.S., 2001, Timing of gold and arsenic sulfide mineral deposition at the Getchell carlin-type gold deposit, north-central Nevada: Economic Geology, v. 96, p. 75–89. (Conliffe et al., 2010) Conliffe, J., Selby, D., Porter, S.J., and Feely, M., 2010, Re–Os molybdenite dates from the Ballachulish and Kilmelford Igneous Complexes (Scottish Highlands): age constraints for late Caledonian magmatism: Journal of the Geological Society, v. 167, p. 297–302. (Corriveau, 2007) Corriveau, L., 2007, Iron oxide copper-gold deposits: A Canadian perspective, in Goodfellow, W.D., ed., Mineral deposits of Canada: A synthesis of major deposit-types, district metallogeny, the evolution of geological provinces, and exploration methods: Geological Association of Canada, Mineral Deposits Division Special Publication 5, p. 307–328. (Dai et al., 2009) Dai, J.Z., Mao, J.W., Zhao, C.S., Xie, G.Q., Yang, F.Q., and Wang, Y.T., 2009, New U–Pb and Re–Os age data and the geodynamic setting of the Xiaojiayingzi Mo (Fe) deposit, western Liaoning province, northeastern China: Ore Geology Reviews, v. 35, p. 235–244. (Delibaş and Genç, 2012) Delibaş, O. and Genç, Y., 2012, Re–Os molybdenite ages of granitoid-hosted Mo–Cu occurrences from central Anatolia (Turkey): Ore Geology Reviews, v. 44, p. 39–48. (Deng et al., 2013a) Deng, X.H., Chen, Y.J., Santosh, M., Zhao, G.C., and Yao, J.M., 2013a, Metallogeny during continental outgrowth in the Columbia supercontinent: Isotopic characterization of the Zhaiwa Mo–Cu system in the North China Craton: Ore Geology Reviews, v. 51, p. 43–56. (Deng et al., 2013b) Deng, X.H., Chen, Y.J., Santosh, M., and Yao, J.M., 2013b, Re–Os geochronology, fluid inclusions and genesis of the 0.85 Ga Tumen molybdenite–fluorite deposit in eastern Qinling, China: implications for pre-Mesozoic Mo enrichment and tectonic setting: New type of Mo mineralization: Geological Journal, v. 48, p. 484–497. (Deng et al., 2015) Deng, X., Chen, Y., Santosh, M., Yao, J., and Sun, Y., 2015, Re-Os and Sr-Nd-Pb isotope constraints on source of fluids in the Zhifang Mo deposit, Qinling Orogen, China. Gondwana Research 30: 132-143. (Deng et al., 2017) Deng, X., Chen, Y., Santosh, M., Wang, J., Li, C., Yue, S., Zheng, Z., Chen, H., Tang, H., Dong, L., and Qu, X., 2017, U-Pb zircon, Re-Os molybdenite geochronology and Rb-Sr geochemistry from the Xiaobaishitou W (-Mo) deposit: Implications for Triassic tectonic setting in eastern Tianshan, NW China. Ore Geology Reviews 80:332-351. (Doebrich et al., 2004) Doebrich, J.L., Zahony, S.G., Leavitt, J.D., Portacio, J.S., Siddiqui, A.A., Wooden, J.L., et al., 2004, Ad Duwayhi, Saudi Arabia: geology and geochronology of a Neoproterozoic intrusion-related gold system in the Arabian Shield: Economic Geology, v. 99, p. 713–741. (Dong et al., 2013) Dong, G.C., Santosh, M., Li, S.R., Shen, J.F., Mo, X.X., Scott, S., et al., 2013, Mesozoic magmatism and metallogenesis associated with the destruction of the North China Craton: Evidence from U–Pb geochronology and stable isotope geochemistry of the Mujicun porphyry Cu–Mo deposit: Ore Geology Reviews, v. 53, p. 434–445. (Du et al., 1995) Du, A.D., He, H.L., Yin, N.W., Zou, X.Q., Sun, Y.L., Sun, D.Z., et al., 1995, A study of the rhenium–osmium geochronomoetry of molybdenites: Acta Geologica Sinica (English Edition), v. 8, p. 171–181. (Du et al., 2004) Du, A.D., Wu, S.Q., Sun, D.Z., Wang, S.X., Markey, R.J., Stein, H.J., et al., 2004, Preparation and Certification of Re-Os Dating Reference Materials: Molybdenites HLP and JDC: Geostandards and Geoanalytical Research, v. 28, p. 41–52. (Dubé et al., 2007) Dubé, B., Gosselin, P., Mercier-Langevin, P., Hannington, M., and Galley, A., 2007, Gold-rich volcanogenic massive sulphide deposits, in Goodfellow, W.D., ed., Mineral deposits of Canada: A synthesis of major deposit-types, district metallogeny, the evolution of geological provinces, and exploration methods: Geological Association of Canada, Mineral Deposits Division Special Publication 5, p. 75–94. (Duncan et al., 2011) Duncan, R.J., Stein, H.J., Evans, K.A., Hitzman, M.W., Nelson, E.P., and Kirwin, D.J., 2011, A new geochronological framework for mineraization and alteration in the Selwyn-Mount Dore Corridor, Eastern Fold Belt, Mount Isa Inlier, Australia: Genetic implications for iron-oxide copper–gold deposits: Economic Geology, v. 106, p. 169–192. (Duuring et al., 2007) Duuring, P. and Cassidy, K.F., and Hagemann, S.G., 2007, Granitoid-associated orogenic, intrusion-related, and porphyry style metal deposits in the Archean Yilgarn Craton, Western Australia: Ore Geology Reviews, v. 32, p. 157–186. (Duuring et al., 2009) Duuring, P., Rowins, S.M., McKinley, B.S.M., Dickinson, J.M., Diakow, L.J., Kim, Y.S., et al., 2009, Magmatic and structural controls on porphyry-style Cu–Au–Mo mineralization at Kemess South, Toodoggone District of British Columbia, Canada: Minerallium Deposita, v. 44, p. 435–462. (Easton, 1986) Easton, R.M., 1986, Geochronology of the Grenville Province, in Moore, J.M. , Davidson, A., and Baer, A.J., eds., The Grenville Province: Geological Association of Canada Special Paper 31, p. 271–280. (Eckstrand and Hulbert, 2007) Eckstrand, O.R. and Hulbert, L.J., 2007, Magmatic nickel-copper-platinum group element deposits, in Goodfellow, W.D., ed., Mineral deposits of Canada: A synthesis of major deposit-types, district metallogeny, the evolution of geological provinces, and exploration methods: Geological Association of Canada, Mineral Deposits Division Special Publication 5, p. 205–222. (Febbo et al., 2015) Febbo, G.E., Kennedy, L.A., Savell, M., Creaser, R.A., and Friedman, R.M., 2015, Geology of the Mitchell Au-Cu-Ag-Mo porphyry deposit, northwestern British Columbia, Canada, in Geological Fieldwork 2014: British Columbia Ministry of Energy and Mines, British Columbia Geological Survey Paper 2015-1, p. 59–86. (Feely et al., 2007) Feely, M., Selby, D., Conliffe, J., and Judge, M., 2007, Re–Os geochronology and fluid inclusion microthermo-metry of molybdenite mineralization in late-Caledonian Omey Granite, western Ireland: Applied Earth Science, v. 116, p. 143–149. (Feely et al., 2010) Feely, M., Selby, D., Hunt, J., and Conliffe, J., 2010, Long-lived granite-related molybdenite mineralization at Connemara, western Irish Caledonides: Geological Magazine, v. 147, p. 886–894. (Feng et al., 2011) Feng, C.Y., Zeng, Z.L., Zhang, D.Q., Qu, W.J., Du, A.D., Li, D.X., et al., 2011, SHRIMP zircon U–Pb and molybdenite Re–Os isotopic dating of the tungsten deposits in the Tianmenshan-Hongtaoling W–Sn orefield, southern Jiangxi Province, China, and geological implications: Ore Geology Reviews, v. 43, p. 8–25. (Fleischer, 1959) Fleischer, M., 1959, The geochemistry of rhenium, with special reference to its occurrence in molybdenite: Economic Geology, v. 54, p. 1406–1413. (Fleischer, 1960) Fleischer, M., 1960, The geochemistry of rhenium—addendum: Economic Geology, v. 55, p. 607–609. (Fornadel et al., 2012) Fornadel, A.P., Voudouris, P.C., Spry, P.G., and Melfos, V., 2012, Mineralogical, stable isotope, and fluid inclusion studies of spatially related porphyry Cu and epithermal Au–Te mineralization, Fakos Peninsula, Limnos Island, Greece: Mineralogy and Petrology, v. 105, p. 85–111. (Frei et al., 1998) Frei, R., Nägler, T.F., Schönberg, R., and Kramers, J.D., 1998, Re–Os, Sm–Nd, U–Pb, and stepwise lead leaching isotope systematics in shear-zone hosted gold mineralization: Genetic tracing and age constraints of crustal hydrothermal activity: Geochimica et Cosmochimica Acta, v. 62, p. 1925–1936. (Freydier et al., 1997) Freydier, C., Ruiz, J., Chesley, J.T., McCandless, T.E., and Munizaga, F., 1997, Re–Os isotope systematics of sulfides from felsic igneous rocks: Application to base metal porphyry mineralization in Chile: Geology, v. 25, p. 775–778. (G. Wang et al., 2017) Wang, G., Wu, G., Xu, L., Li, X., Zhang, T., Quan, Z., Wu, H., Liu, J., and Chen, Y., 2017, Molybdenite Re-Os age, H-O-C-S-Pb isotopes, and fluid inclusion study of the Caosiyao porphyry Mo deposit in Inner Mongolia, China. Ore Geology Reviews 81: 728-744. (Gallagher et al., 1992) Gallagher, V., Feely, M., Högelsberger, H., Jenkin, G.R.T., and Fallick, A.E., 1992, Geological, fluid inclusion and stable isotope studies of Mo mineralization, Galway Granite, Ireland: Minerallium Deposita, v. 27, p. 314–325. (Gao et al., 2017) Gao, Z., Yang, L., Meng, J., and Zhang, L., 2017, Zircon U-Pb, molybdenite Re-Os geochronology and Sr-Nd-Pb-Hf-O-S isotopic constraints on the genesis of Relin Cu-Mo deposit in Zhongdian, Northwest Yunnan, China. Ore Geology REviews 91: 945-962. (Garrido et al., 2008) Garrido, M., Barra, F., Domínguez, E., Ruiz, J., and Valencia, V.A., 2008, Late Carboniferous porphyry copper mineralization at La Voluntad, Neuquén, Argentina: Constraints from Re–Os molybdenite dating: Minerallium Deposita, v. 43, p. 591–597. (Giles and Schilling, 1972) Giles, D.L. and Schilling, J.H., 1972, Variation in rhenium content of molybdenite: International Geological Congress, 24th, Montréal, 1972, Proceedings, v. 10, p. 145–152. (Gilmer et al., 2003) Gilmer, A.K., Kyle, J.R., Connelly, J.N., Mathur, R.D., and Henry, C.D., 2003, Extension of Laramide magmatism in southwestern North America into Trans-Pecos Texas: Geology, v. 31, p. 447–450. (Golden et al., 2013) Golden, J., McMillan, M., Downs, R.T., Hystad, G., Goldstein, I., Stein, H.J., et al., 2013, Rhenium variationsin molybdenite (MoS2): Evidence for progressive subsurface oxidation: Earth and Planetary Science Letters, v. 366, p. 1–5. (Goss, 2009) Goss, B.J., 2009, Market Release, High-grade molybdenum and rhenium intercepts drilled on Ivanhoe Australia's Merlin Project (http://www.ivanhoe-mines.com/i/pdf/2009-03-24_IAL_NR.pdf). (Grabezhev and Shagalov, 2010) Grabezhev, A.I. and Shagalov, E.S., 2010, Rhenium distribution in molybdenite: Results of microprobe scanning (Copper Porphyry Deposits, the Urals): Doklady Earth Sciences, v. 431, p. 351–355. (Grabezhev and Voudouris, 2014) Grabezhev, A.I. and Voudouris, P.C., 2014, Rhenium distribution in molybdenite from the Vosnesensk porphyry Cu (Mo,Au) deposit (southern Urals, Russia): The Canadian Mineralogist, v. 52, p. 671–686. (Guo et al., 2011) Guo, C.L., Mao, J.W., Bierlein, F., Chen, Z.H., Chen, Y.C., Li, C.B., et al., 2011, SHRIMP U–Pb (zircon), Ar–Ar (muscovite) and Re–Os (molybdenite) isotopic dating of the Taoxikeng tungsten deposit, South China Block: Ore Geology Reviews, v. 43, p. 26–39. (Guo et al., 2012) Guo, S., Zhao, Y.Y., Qu, H.C., Wu, D.X., Xu, H., Li, C., et al., 2012, Geological Characteristics and Ore-forming Time of the Dexing Porphyry Copper Ore Mine in Jiangxi Province: Acta Geologica Sinica (English Edition), v. 86, p. 691–699. (Guo et al., 2018) Guo, W., Zeng, Q., Zhang, B., and Hu, Y., 2018, Genesis of the Jurassic Dongfengbeishan porphyry Mo deposit in Eastern Yanbian, NE China inferred from molybdenite Re-Os and zircon U-Pb ages, and whole-rock elemental and zircon Hf isotopic compositions. Journal of Asian Earth Sciences 15: 245-269. (H. Sun et al., 2017) Sun, H., Li, H., Danisik, M., Xia, Q., Jiang, C., Wu, P., Yang, H., Fan, Q., and Zhu, D., 2017, U-Pb and Re-Os geochronology and geochemistry of the Donggebi Mo deposit, Eastern Tianshan, NW China: Insights into mineralization and tectonic setting. Ore Geology Reviews 86: 584-599. (Hamasaki, 2002) Hamasaki, S., 2002, Volcanic-related alteration and geochemistry of Iwodake volcano, Satsuma-Iwojima, Kyushu SW Japan: Earth and Planetary Science Letters, v. 54, p. 217–229. (Hammarstrom et al., 2014) Hammarstrom, J.M., Bookstrom, A.A., DeMarr, M.W., Dicken, C.L., Ludington, S., Robinson, G.R., Jr., et al., 2014, Porphyry copper assessment of East and Southeast Asia—Philippines, Taiwan (Republic of China), Republic of Korea (South Korea), and Japan: U.S. Geological Survey Scientific Investigations Report 2010–5090–P, 241 p. (Han et al., 2009) Han, C.M., Xiao, W.J., Zhao, G.C., Sun, M., Qu, W.J., and Du, A.D., 2009, A Re–Os study of molybdenites from the Lanjiagou Mo deposit of North China Craton and its geological significance: Gondwana Research, v. 16, p. 264–271. (Han et al., 2013) Han, YG., Zhang, S.H., Pirajno, F., Zhou, X.W., Zhao, G.C., Qü, W.J., et al., 2013, U–Pb and Re–Os isotopic systematics and zircon Ce4+/Ce3+ ratios in the Shiyaogou Mo deposit in eastern Qinling, central China: Insights into the oxidation state of granitoids and Mo (Au) mineralization: Ore Geology Reviews, v. 55, p. 29–47. (Han et al., 2014a) Han, YG., Xiao, W.J., Zhao, G.C., Sun, M., Qü, W.J., and Du, A.D., 2014a, Re–Os geochronology on molybdenites from the Donggebi Mo Deposit in the Eastern Tianshan of the Central Asia Orogenic Belt and its geological significance: Resource Geology, v. 64, p. 136–148. (Han et al., 2014b) Han, C.M., Xiao, W.J., Zhao, G.C., Su, B.X., Ao, S.J., Zhang, J., et al., 2014b, Tectonic implications of Re-Os dating of molybdenum deposits in the Tianshan–Xingmeng Orogenic Belt, Central Asia: International Geology Review, v. 56, p. 985–1006. (Han et al., 2014c) Han, C., Xiao, W., Windley, B., Zhao, G., Su, B., Ao, S., Zhang, J., Zhang, Z., Wan, B., Cui, B., Qu, W., and Du, A., 2014, Re-Os age of molybdenite from the Daheishan Mo deposit in the Eastern Central Asian Orogenic Belt, NE China. Resource Geology 64.4: 379-386. (Hannah et al., 2007) Hannah, J.L., Stein, H.J., Wieser, M.E., De Laeter, J.R., and Varner, M.D., 2007, Molybdenum isotope variations in molybdenite: Vapor transport and Rayleigh fractionation of Mo: Geology, v. 35, p. 703–706. (Hirt et al., 1963) Hirt, B. and Herr, W., and Hoffmeister, W., 1963, Age determinations by the rhenium-osmium method, Radiometric dating: International Atomic Energy Agency, Vienna, 1963, p. 35–43. (Hiskey and Meloche, 1940) Hiskey, C.F. and Meloche, V.W., 1940, Determination of rhenium in molybdenite minerals: Industrial & Engineering Chemistry Analytical Edition, v. 12, p. 503–506. (Holiday et al., 2002) Holiday, J.R., Wilson, A.J., Belvin, P.L., Tedder, I.J., Dunhan, P.D., and Pfitzner, M., 2002, Porphyry gold–copper mineralisation in the Cadia district, eastern Lachlan Fold Belt, New South Wales, and its relationship to shoshonitic magmatism: Minerallium Deposita, v. 37, p. 100–116. (Holwell et al., 2012) Holwell, D.A., Selby, D., Boyce, A.J., Gilbertson, J.A., and Abraham-James, T., 2012, An Re–Os date for molybdenite-bearing quartz vein mineralization within the Kangerlussuaq alkaline complex, east Greenland: Implications for the timing of regional metallogenesis: Economic Geology, v. 107, p. 713–722. (Hou et al., 2006) Hou, Z.Q., Zeng, P.S., Gao, Y.F., Du, A.D., and Fu, D.M., 2006, Himalayan Cu–Mo–Au mineralization in the eastern Indo-Asian collision zone: constraints from Re–Os dating of molybdenite: Minerallium Deposita, v. 41, p. 33–45. (Hou et al., 2009) Hou, Z.Q., Yang, Z.M., Qu, X.M., Meng, X.J., Li, Z.Q., Beaudoin, G., et al., 2009, The Miocene Gangdese porphyry copper belt generated during post-collisional extension in the Tibetan Orogen: Ore Geology Reviews, v. 36, p. 25–51. (Hu et al., 2014) Hu, X., Ding, Z., He, M., Yao, S., Zhu, B., Shen, J., and Chen, B., 2014. A porphyry-skarn metallogenic system in the Lesser Xing'an Range, NE China: Implications from U-Pb and Re-Os geochronology and Sr-Nd-Hf isotopes of the Luming Mo and Xulaojiugou Pb-Zn deposits. Journal of Asian Earth Sciences 90: 88-100. (Huang et al., 1994) Huang, D., Wu, C., Du, A., and He, H., 1994, Re-Os isotope ages of molybdenum deposits and their significance. Chinese Journal of Geochemistry 14.4: 313-322. (Huang et al., 2015) Huang, J., Peng, J., Yang, J., Zhang, B., and Xu, C., 2015, Precise zircon U-Pb and molybdenite Re-Os dating of the Shuikoushan granodiorite-related Pb-Zn mineralization, southern Hunan, South China. Ore Geology Reviews 71: 305-317. (Hutton et al., 2012) Hutton, L.J., Denaro, T.J, Dhnaram, C., and Derrick, G.M., 2012, Mineral systems in the Mount Isa inlier: Journal of International Geoscience, v. 35, p. 120–130. (Ishihara, 1988) Ishihara, S., 1988, Rhenium contents of molybdenites in granitoid-series rocks in Japan: Economic Geology, v. 83, p. 1047–1051. (J. Sun et al., 2017) Sun, J., Mao, J., Beaudoin, G., Duan, X., Yao, F., Ouyang, H., Wu, Y., Li, Y., and Meng, X., 2017, Geochronology and geochemistry of porphyritic intrusions in the Duolong porphyry and epithermal Cu-Au district, central Tibet: Implications for the genesis and exploration of porphyry copper deposits. Ore Geology Reviews 80: 1004-1019. (J.W. Li et al., 2014) Li, J.W., Vasconcelos, P.M., Zhou, M.F., Deng, X.D., Cohen, B., Bi, S.J., et al., 2014, Longevity of magmatic-hydrothermal systems in the Daye Cu–Fe–Au District, eastern China with implications for mineral exploration: Ore Geology Reviews, v. 57, p. 375–392. (Jensen, 1998) Jensen, P.W., 1998, A structural and geochemical study of the Sierrita porphyry copper system, Pima County, Arizona: Unpublished Ph.D. Dissertation, University of Arizona, Tucson, 136 p. (John and Bliss, 1994) John, D.A. and Bliss, J.D., 1994, Grade and tonnage model of tungsten skarn deposits, Nevada: U.S. Geological Survey Open-File Report 94-005, 35 p. (Kirkham and Sinclair, 1995) Kirkham, R.V. and Sinclair, W.D., 1995, Porphyry copper, gold, molybdenum, tungsten, tin, silver, in Eckstrand, O.R., Sinclair, W.D., and Thorpe, R.I., eds., Geology of Canadian Mineral Deposit Types: Geological Survey of Canada Geology of Canada no. 8, p. 421–446. (Kohút and Stein, 2005) Kohút, M. and Stein, H.J., 2005, Re–Os molybdenite dating of granite-related Sn–W–Mo mineralisation at Hnilec, Gemeric Superunit, Slovakia: Mineralogy and Petrology, v. 85, p. 117–129. (Kuleshevich, 2007) Kuleshevich, L.V., 2007, Gold mineralization in Karelia: Endogenic formation regimes, genetic types, and ore associations: Doklady Earth Sciences, v. 412, p. 89–93. (L. Yang et al., 2017) Yang, L., Deng, J., Gao, X., He, W., Meng, J., Santosh, M., Yu, H., Yang, Z., and Wang, D., 2017, Timing of formation and origin of the Tongchanggou porphyry-skarn deposit: Impications for Late Cretaceous Mo-Cu metallogenesis in the southern Yidun Terrane, SE Tibetan Plateau. Ore Geology Reviews 81: 1015-1032. (Lang et al., 2013) Lang, J.R., Gregory, M.J., Rebagliati, C.M., Payne, J.G., Oliver, J.L., and Roberts, K., 2013, Geology and magmatic-hydrothermal evolution of the giant Pebble porphyry copper–gold-molybdenum deposit, southwest Alaska: Economic Geology, v. 108, p. 437–462. (Lang et al., 2014) Lang, X., Tang, J., Li, Z., Huang, Y., Ding, F., Yang, H., Xie, F., Zhang, L., Wang, Q., and Zhou, Y., 2014, U-Pb and Re-Os geochronological evidence for the Jurassic porphyry metallogenic event of the Xiongcun district in the Gangdese porphyry copper belt, southern Tibet, PRC. Journal of Asian Earth Sciences 29: 608-622. (Langthaler et al., 2004) Langthaler, K.J., Raith, J.G., Cornell, D.H., Stein, H.J., and Melcher, F., 2004, Molybdenum mineralization at Alpeiner Scharte, Tyrol (Austria): results of in-situ U–Pb zircon and Re–Os molybdenite dating: Mineralogy and Petrology, v. 82, p. 33–64. (Large, 1992) Large, R.R., 1992, Australian volcanic-hosted massive sulfide deposits: features, styles, and genetic models: Economic Geology, v. 87, p. 471–510. (Lavrov and Kuleshevich, 2010) Lavrov, O.B. and Kuleshevich, L.V., 2010, The first finds of rhenium minerals in Karelia: Doklady Earth Sciences, v. 432, p. 598–601. (Lawley and Selby, 2012) Lawley, C.J.M. and Selby, D., 2012, Re–Os geochronology of quartz-enclosed ultrafine molybdenite: implications for ore geochronology: Economic Geology, v. 107, p. 1499–1505. (Lawley et al., 2013) Goodfellow, W.D. and Lydon, J.W., 2007, Sedimentary exhalative (SEDEX) deposits, in Goodfellow, W.D., ed., Mineral deposits of Canada: A synthesis of major deposit-types, district metallogeny, the evolution of geological provinces, and exploration methods: Geological Association of Canada, Mineral Deposits Division Special Publication 5, p. 163–183. (Lawley et al., 2013) Lawley, C.J.M. and Selby, D., and Imber, J., 2013, Re-Os molybdenite, pyrite, and chalcopyrite geochronology, Lupa Goldfield, Southwestern Tanzania: Tracing metallogenic time scales at midcrustal shear zones hosting orogenic Au deposits: Economic Geology, v. 108, p. 1591–1613. (Lentz and Creaser, 2005) Lentz, D.R. and Creaser, R.A., 2005, Re-Os Model Age Constraints on the Genesis of the Moss Molybdenite Pegmatite-Aplite Deposit, Southwestern Grenville Province, Quyon, Quebec, Canada: Exploration and Mining Geology, v. 14, p. 95–103. (Li and Jiang, 2017) Li, B., and Jiang, S., 2017, Genesis of the giant Zijinshan epithermal Cu-Au and Luoboling porphyry Cu-Mo deposits in the Zijinshan ore district, Fujian province, SE China: A multi-isotope and trace element investigation. Ore Geology Reviews 88: 753-767. (Li et al., 2008) Li, J.W., Zhao, X.F., Zhou, M.F., Vasconcelos, P.M., Ma, C.Q., Deng, X.D., et al., 2008, Origin of the Tongshankou porphyry–skarn Cu–Mo deposit, eastern Yangtze craton, eastern China: geochronological, geochemical, and Sr–Nd–Hf isotopic constraints: Minerallium Deposita, v. 43, p. 315–336. (Li et al., 2010) Li, X.F., Feng, Z.H., Wang, C.Z., Li, R.S., and Tang, Z.H., 2010, Molybdenite Re–Os and Zircon SHRIMP U–Pb Dating at the Baishiding Deposit, Guposhan District: New Evidence for Silurian Mo Mineralization in South China: Silurian Mo mineralization in South China: Resource Geology, v. 60, p. 260–270. (Li et al., 2012) Li, W.B., Zhong, R.C., Xu, C., Song, B., and Qu, W.J., 2012, U–Pb and Re–Os geochronology of the Bainaimiao Cu–Mo–Au deposit, on the northern margin of the North China Craton, Central Asia Orogenic Belt: Implications for ore genesis and geodynamic setting: Ore Geology Reviews, v. 48, p. 139–150. (Liang et al., 2016) Liang, X., Dong, C., Jiang, Y., Wu, S., Zhou, Y., Zhu, H., Fu, J., Wang, C., and Shan, Y., 2016, Zircon U-Pb, molybdenite Re-Os and muscovite Ar-Ar isotopic dating of the Xitian W-Sn polymetallic deposit, eastern Hunan province, South China and its geological significance. Ore Geology Reviews 78: 85-100. (Liu et al., 2011) Liu, J., Mao, J.W., Ye, H.S., and Zhang, W., 2011, Geology, geochemistry and age of the Hukeng tungsten deposit, southern China: Ore Geology Reviews, v. 43, p. 50–61. (Liu et al., 2012) Liu, J., Wu, G., Li, Y, Zhu, M., and Zhong, W., 2012, Re-Os sulfide (chalcopyrite, pyrite and molybdenite) systematics and fluid inclusion study of the Duobaoshan porphyry Cu (Mo) deposit, Heilongjiang province, China. Journal of Asian Earth Sciences 49: 300-312. (Liu et al., 2014) Liu, F., Zhang, Z.X., Li, Q., Zhang, C., and Li, C., 2014, New precise timing constraint for the Keketuohai No. 3 pegmatite in Xinjiang, China, and identification of its parental pluton: Ore Geology Reviews, v. 56, p. 209–219. (Luck and Allègre, 1982) Luck, J.M. and Allègre, C.J., 1982, The study of molybdenites through the 187Re–187Os chronometer: Earth and Planetary Science Letters, v. 61, p. 291–296. (Ludington et al., 2012a) Ludington, S., Mihalasky, M.J., Hammarstrom, J.M., Robinson, G.R., Jr., Frost, T.P., Gans, K.D., et al., 2012a, Porphyry copper assessment of the Mesozoic of East Asia—China, Vietnam, North Korea, Mongolia, and Russia: U.S. Geological Survey Scientific Investigations Report 2010-5090-G, 53 p. (Ludington et al., 2012b) Ludington, S., Hammarstrom, J.M., Robinson, G.R., Jr., Mars, J.L., and Miller, R.J., 2012b, Porphyry copper assessment of the Tibetan Plateau, China: U.S. Geological Survey Scientific Investigations Report 2010–5090–F, 63 p. (Lydon, 2007) Lydon, J.W., 2007, An overview of the economic and geological contexts of Canada’s major mineral deposit types, in Goodfellow, W.D., ed., Mineral deposits of Canada: A synthesis of major deposit-types, district metallogeny, the evolution of geological provinces, and exploration methods: Geological Association of Canada, Mineral Deposits Division Special Publication 5, p. 3–48. (Maksaev et al., 2004) Maksaev, V., Munizaga, F., McWilliams, M., Fanning, M., Mathur, R.D., Ruiz, J., et al., 2004, New chronology for El Teniente, Chilean Andes, from U/Pb, 40Ar/39Ar, Re/Os and fission-track dating: implications for the evolution of a supergiant porphyry Cu–Mo deposit, in Andean metallogeny: new discoveries, concepts update: Society of Economic Geologists Special Publication 11, p. 15–54. (Mao et al., 1999) Mao, J.W., Zhang, Z.C., Zhang, Z.H., and Du, A.D., 1999, Re–Os isotopic dating of molybdenites in the Xiaoliugou W (Mo) deposit in the northern Qilian mountains and its geological significance: Geochimica et Cosmochimica Acta, v. 63, p. 1815–1818. (Mao et al., 2002) Mao, J.W., Lehmann, Bernd., Du, A.D., Zhang, G., Ma, D., Wang, Y., et al., 2002, Re-Os dating of polymetallic Ni-Mo-PGE-Au mineralization in Lower Cambrian black shales of South China and its geologic significance: Economic Geology, v. 97, p. 1051–1061. (Mao et al., 2003) Mao, J.W., Du, A.D., Seltmann, R., and Yu, J.J., 2003, Re–Os ages for the Shameika porphyry Mo deposit and the Lipovy Log rare metal pegmatite, central Urals, Russia: Minerallium Deposita, v. 38, p. 251–257. (Mao et al., 2006) Mao, J.W., Wang, Y.T., Lehmann, Bernd., Yu, J.J., Du, A.D., Mei, Y.X., et al., 2006, Molybdenite Re–Os and albite 40Ar/39Ar dating of Cu–Au–Mo and magnetite porphyry systems in the Yangtze River valley and metallogenic implications: Ore Geology Reviews, v. 29, p. 307–324. (Mao et al., 2008) Mao, J.W., Xie, G.Q., Bierlein, F., Qü, W.J., Du, A.D., Ye, H.S., et al., 2008, Tectonic implications from Re–Os dating of Mesozoic molybdenum deposits in the East Qinling-Dabie orogenic belt: Geochimica et Cosmochimica Acta, v. 72, p. 4607–4626. (Mao et al., 2013) Mao, Z.H., Cheng, Y.B., Liu, J.J., Yuan, S.D., Wu, S.H., Xiang, X.K., et al., 2013, Geology and molybdenite Re–Os age of the Dahutang granite-related veinlets-disseminated tungsten ore field in the Jiangxin Province, China: Ore Geology Reviews, v. 53, p. 422–433. (Markey et al., 1998) Markey, R.J. and Stein, H.J., and Morgan, J.W., 1998, Highly precise Re–Os dating for molybdenite using alkaline fusion and NTIMS: Talanta, v. 45, p. 935–946. (Markey et al., 2003) Markey, R.J., Hannah, J.L., Morgan, J.W., and Stein, H.J., 2003, A double spike for osmium analysis of highly radiogenic samples: Chemical Geology, v. 200, p. 395–406. (Markey et al., 2007) Markey, R.J., Stein, H.J., Hannah, J.L., Zimmerman, A., Selby, D., and Creaser, R.A., 2007, Standardizing Re–Os geochronology: A new molybdenite reference material (Henderson, USA) and the stoichiometry of Os salts: Chemical Geology, v. 244, p. 74–87. (Marschik et al., 2005) Marschik, R., Mathur, R.D., Ruiz, J., Leveille, R.A., and de Almeida, A.J., 2005, Late Archean Cu–Au–Mo mineralization at Gameleira and Serra Verde, Carajás Mineral Province, Brazil: constraints from Re–Os molybdenite ages: Minerallium Deposita, v. 39, p. 983–991. (Marsh et al., 2003) Marsh, E.E., Goldfarb, R.J., Hart, C.J.R., and Johnson, C.A., 2003, Geology and geochemistry of the Clear Creek intrusion-related gold occurrence, Tintina gold province, Yukon, Canada: Canadian Journal of Earth Sciences, v. 4. (Masterman et al., 2004) Masterman, G.J., Cooke, D.R., Berry, R.F., Clark, A.H., Archibald, D.A., Mathur, R.D., et al., 2004, 40Ar/39Ar and Re–Os geochronology of porphyry copper–molybdenum deposits and related copper–silver veins in the Collahuasi District, northern Chile: Economic Geology, v. 99, p. 673–690. (Mathur et al., 2000) Mathur, R.D. and Ruiz, J., and Munizaga, F., 2000, Relationship between copper tonnage of Chilean base-metal porphyry deposits and Os isotope ratios: Geology, v. 28, p. 555–558. (Mathur et al., 2002) Mathur, R.D., Marschik, R., Ruiz, J., Munizaga, F., Leveille, R.A., and Martin, W., 2002, Age of mineralization of the Candelaria Fe oxide Cu–Au deposit and the origin of the Chilean iron belt, based on Re–Os isotopes: Economic Geology, v. 97, p. 59–71. (Mathur et al., 2005) Mathur, R.D., Titley, S.R., Ruiz, J., Gibbins, S., and Friehauf, K., 2005, A Re–Os isotope study of sedimentary rocks and copper–gold ores from the Ertsberg District, West Papua, Indonesia: Ore Geology Reviews, v. 26, p. 207–226. (Mathur et al., 2010) Mathur, R.D., Brantley, S., Anbar, A.D., Munizaga, F., Maksaev, V., Newberry, R.J.J., et al., 2010, Variation of Mo isotopes from molybdenite in high-temperature hydrothermal ore deposits: Minerallium Deposita, v. 45, p. 43–50. (McCandless and Ruiz, 1993) McCandless, T.E. and Ruiz, J., 1993, Rhenium–osmium evidence for regional mineralization in southwestern North America: Science, v. 261, p. 1282–1282. (McCandless et al., 1993) McCandless, T.E. and Ruiz, J., and Campbell, A.R., 1993, Rhenium behavior in molybdenite in hypogene and near-surface environments: Implications for Re–Os geochronometry: Geochimica et Cosmochimica Acta, v. 57, p. 889–905. (McFall, 2016) McFall, K., 2016, Critical metals in porphyry copper deposits. Unpublished Ph.D. thesis, University of Southampton, Southampton, UK, 269 p. (Meinert, 1992) Meinert, L.D., 1992, Skarns and skarn deposits: Geoscience Canada, v. 19, p. 145–162. (Migisha and Both, 1991) Migisha, C.J.R. and Both, R.A., 1991, Mineralogy and genesis of the Trench tungsten–molybdenum deposit, Mount Mulgine, Western Australia: Minerallium Deposita, v. 26, p. 247–256. (Mihalasky et al., 2011) Mihalasky, M.J., Bookstrom, A.A., Frost, T.P., and Ludington, S., 2011, Porphyry copper assessment of British Columbia and Yukon Territory, Canada: U.S. Geological Survey Scientific Investigations Report 2010-5090-C, 128 p. (Mihalasky et al., 2015a) Mihalasky, M.J., Ludington, S., Alexeiev, D.V., Frost, T.P., Light, T.D., Briggs, D.A., et al., 2015a, Porphyry copper assessment of northeast Asia—Far East Russia and Northeasternmost China: U.S. Geological Survey Scientific Investigations Report 2010– 5090–W, 104 p. (Mihalasky et al., 2015b) Mihalasky, M.J., Ludington, S., Hammarstrom, J.M., Alexeiev, D.V., Frost, T.P., Light, T.D., et al., 2015b, Porphyry Copper Assessment of the Central Asian Orogenic Belt and eastern Tethysides—China, Mongolia, Russia, Pakistan, Kazakhstan, Tajikistan, and India: U.S. Geological Survey Scientific Investigations Report 2010–5090–X, 106 p. (Mikulski and Stein, 2007) Mikulski, S.Z. and Stein, H.J., 2007, Re-Os age for molybdenite from the West Sudetes, SW Poland, in Kozłowski, A., and Wiszniewska, J., eds., Granitoids in Poland: Archivum Mineralogiae Monograph no. 1, p. 203–216. (Mirnejad et al., 2013) Mirnejad, H., Mathur, R.D., Hassanzadeh, J., Shafie, B., and Nourali, S., 2013, Linking Cu mineralization to host porphyry emplacement: Re–Os ages of molybdenites versus U–Pb ages of zircons and sulfur isotope compositions of pyrite and chalcopyrite from the Iju and Sarkuh porphyry deposits in Southeast Iran: Economic Geology, v. 108, p. 861–870. (Moore, 2010) Moore, J.M., 2010, Comparative study of the Onganja copper mine, Namibia: A link between Neoproterozoic mesothermal Cu(-Au) mineralization in Namibia and Zambia: South African Journal of Geology, v. 113, p. 445–460. (Morgan et al., 1968) Morgan, J.W. and Lovering, J.F., and Ford, R.J., 1968, Rhenium and non-radiogenic osmium in Australian molybdenites and other sulphide minerals by neutron activation analysis: Journal of the Geological Society of Australia, v. 15, p. 189–194. (Nabatian et al., 2017) Nabatian, G., Wan, B., and Honarmand, M., 2017, Whole rock geochemistry, molybdenite Re-Os geochronology, stable isotope and fluid inclusion investigations of the Siah-Kamar deposit, western Alborz-Azerbayjan: New constraints on the porphyry Mo deposit in Iran. Ore Geology Reviews, accessed online Oct. 7, 2017 at http://www.sciencedirect.com/science/article/pii/S0169136816306230. (Nelson and Colpron, 2007) Nelson, J. and Colpron, M., 2007, Tectonics and metallogeny of the British Columbia, Yukon and Alaskan Cordillera, 1.8 Ga to the present, in Goodfellow, W.D., ed., Mineral deposits of Canada: A synthesis of major deposit-types, district metallogeny, the evolution of geological provinces, and exploration methods: Geological Association of Canada, Mineral Deposits Division Special Publication 5, p. 775–791. (Ni et al., 2014) Ni, Z.Y. and Li, N., and Zhang, H., 2014, Hydrothermal mineralization at the Dahu Au–Mo deposit in the Xiaoqinling goldfield, Qinling Orogen, central China: Geological Journal, v. 49, p. 501–524. (Nigatu, 2011) Nigatu, W., 2011, Rhenium in the Aitik Cu–Au–Ag–(Mo) deposit: Unpublished M.Sc. Thesis, Luleå University of Technology, Luleå, 48 p. (Oberthür et al., 2009) Oberthür, T., Melcher, F., Henjes-Kunst, F., Gerdes, A., Stein, H.J., Zimmerman, A., et al., 2009, Hercynian age of the cobalt–nickel–arsenide–(gold) ores, Bou Azzer, Anti-Atlas, Morocco: Re–Os, Sm–Nd, and U–Pb age determinations: Economic Geology, v. 104, p. 1065–1079. (Paganelli, 1963) Paganelli, L., 1963, On rhenium content of molybdenite of Mount Mulat (Predazzo) and other Italian molybdenites: Geochimica et Cosmochimica Acta, v. 27, p. 401–404. (Pan et al., 2017) Pan, X., Hou, Z., Li, Y., Chen, G., Zhao, M., Zhang, T., Zhang, C., Wei, J., and Kang, C., 2017, Dating the giant Zhuxi W-Cu deposit (Taqian-Fuchun Ore Belt) in South China using molybdenite Re-Os and muscovite Ar-Ar system. Ore Geology Reviews 86: 719-733. (Pang et al., 2014) Pang, A.J., Li, S.R., Santosh, M., Yang, Q.Y., Jia, B.J., and Yang, C.D., 2014, Geochemistry, and zircon U–Pb and molybdenite Re–Os geochronology of Jilongshan Cu–Au deposit, southeastern Hubei Province, China: Geological Journal, v. 49, p. 52–68. (Pasava et al., 2016) Pasava, J., Svojtka, M., Veselovsky, F., Durisova, J., Ackerman, L., Pour, O., Drabek, M., Halodova, P., and Haluzova, E., 2016, Laser ablation ICPMS study of trace element chemistry in molybdenite coupled with scanning electron microscopy (SEM) - An important tool for identification of different types of mineralization. Ore Geology Reviews 72: 874-895. (Peng et al., 2006) Peng, J.T., Zhou, M.F., Hu, R.Z., Shen, N.P., Yuan, S.D., Bi, X.W., et al., 2006, Precise molybdenite Re–Os and mica Ar–Ar dating of the Mesozoic Yaogangxian tungsten deposit, central Nanling district, South China: Minerallium Deposita, v. 41, p. 661–669. (Pirajno, 2013) Pirajno, F., 2013, The Geology and Tectonic Settings of China's Mineral Deposits: Dordrecht, Springer Netherlands, 679 p. (Q. Leng et al., 2015) Leng, Q., Tang, J., Zheng, Q., Lin, B., Tang, P., Wang, H., and Li, H., 2015, Zircon U-Pb and molybdenite Re-Os ages of the Lakange porphyry Cu-Mo deposit, Gangdese porphyry copper belt, southern Tibet, China. Resource Geology 66.2: 163-182. (Q. Li et al., 2014) Li, Q., Zhang, Z.X., Geng, X.X., Li, C., Liu, F., Chai, F.M., et al., 2014, Geology and geochemistry of the Qiaoxiahala Fe–Cu–Au deposit, Junggar region, northwest China: Ore Geology Reviews, v. 57, p. 462–481. (Qiu et al., 2016a) Qiu, K., Deng, J., Taylor, R., Song, K., Song, Y., Li, Q., and Goldfarb, R., 2016, Paleozoic magmatism and porphyry Cu-mineralization in an evolving tectonic setting in the Norht Qilian Orogenic Belt, NW China. Journal of Asian Earth Sciences 122: 20-40. (Qiu et al., 2016b) Qiu, K., Taylor, R., Song, Y., Yu, H., Song, K., and Li, N., 2016, Geologic and geochemical insights into the formation of the Taiyangshan porphyry copper-molybdenum deposit, Western Qinling Orogenic Belt, China. Gondwana Research 35: 40-58. (Qu et al., 2012) Qu, H.Y., Pei, R.F., Fei, H.C., Li, J.W., Wang, Y.L., Wang, H.L., et al., 2012, Geology, Geochemistry, and Geochronology of the Fenghuangshan Skarn-type Copper Deposit in the Tongling Ore Cluster, Anhui Province, East China: Acta Geologica Sinica (English Edition), v. 86, p. 700–718. (Raith and Stein, 2000) Raith, J.G. and Stein, H.J., 2000, Re–Os dating and sulfur isotope composition of molybdenite from tungsten deposits in western Namaqualand, South Africa: implications for ore genesis and the timing of metamorphism: Minerallium Deposita, v. 35, p. 741–753. (Rathkopf, 2015) Rathkopf, C.A., 2015, Distribution of Re in molybdenite at the Bagdad Porphyry Cu-Mo deposit: Unpublished Master's Thesis, University of Arizona, Tucson. (Reid et al., 2013) Reid, A., Smith, R.N., Baker, T., Jagodzinski, E.A., Selby, D., Gregory, C.J., et al., 2013, Re–Os dating of molybdenite within hematite breccias from the Vulcan Cu–Au prospect, Olympic Cu–Au province, South Australia: Economic Geology, v. 108, p. 883–894. (Ren et al., 2017) Ren, L., Sun, J., Han, J., Liu, Y., Wang, C., Gu, A., Zhao, K., and Y, R., 2017, Magmatism and metallogenic mechanisms of the Baoshan Cu-polymetallic deposit from the Lesser Xing'an Range, NE China: Constraints from geology, geochronology, geochemistry, and Hf isotopes. Ore Geology Reviews 88: 270-288. (Requia et al., 2003) Requia, K., Stein, H.J., Fontboté, L., and Chiaradia, M., 2003, Re–Os and Pb–Pb geochronology of the Archean Salobo iron oxide copper?gold deposit, Carajás mineral province, northern Brazil: Minerallium Deposita, v. 38, p. 727–738. (Riley, 1967) Riley, G.H., 1967, Rhenium concentration in Australian molybdenites by stable isotope dilution: Geochimica et Cosmochimica Acta, v. 31, p. 1489–1497. (Romer et al., 2007) Romer, R.L., Thomas, R., Stein, H.J., and Rhede, D., 2007, Dating multiply overprinted Sn-mineralized granites—examples from the Erzgebirge, Germany: Minerallium Deposita, v. 42, p. 337–359. (Romero et al., 2011) Romero, B., Kojima, S., Wong, C., Barra, F., Véliz, W., and Ruiz, J., 2011, Molybdenite Mineralization and Re–Os Geochronology of the Escondida and Escondida Norte Porphyry Deposits, northern Chile: Molybdenite of the Escondida deposits Chile: Resource Geology, v. 61, p. 91–100. (Rosa and Ulrich, 2015) Rosa, D., and Ulrich, T., 2015, A quartz-wolframite-molybdenite vein and scheelite in amphibolite horizons from Thrudvang peninsula, Skjoldungen, SE Greenland. Geological Survey of Denmark and Greenland Bulletin 33: 49-52. (Ross and Keays, 1979) Ross, J.R. and Keays, R.R., 1979, Precious metals in volcanic-type nickel culfide deposits in Western Australia: Canadian Mineralogist, v. 17, p. 417–435. (Rubin and Kyle, 1988) Rubin, J.N. and Kyle, J.R., 1988, Mineralogy and geochemistry of the San Martin skarn deposit, Zacatecas, Mexico: Economic Geology, v. 83, p. 1782–1801. (S. Li et al., 2014) Li, S., Yang, X.Y., Huang, Y., and Sun, W.D., 2014, Petrogenesis and mineralization of the Fenghuangshan skarn Cu–Au deposit, Tongling ore cluster field, Lower Yangtze metallogenic belt: Ore Geology Reviews, v. 58, p. 148–162. (Santosh et al., 1994) Santosh, M. and Suzuki, K., and Masuda, A., 1994, Re-Os dating of molybdenites from Southern India - Implication for pan-African metallogeny: Journal of the Geological Society of India, v. 43, p. 585–590. (Schindler, 1975) Schindler, N.J., 1975, Rhenium and osmium in some Canadian ores by neutron activation analysis: Unpublished Ph.D. Dissertation, McMaster University, Hamilton, 254 p. (Schütte et al., 2012) Schütte, P., Chiaradia, M., Barra, F., Villagómez, D., and Beate, B., 2012, Metallogenic features of Miocene porphyry Cu and porphyry-related mineral deposits in Ecuador revealed by Re–Os, 40Ar/39Ar, and U–Pb geochronology: Minerallium Deposita, v. 47, p. 383–410. (Seedorff et al., 2005) Seedorff, E., Dilles, J.H., Proffet, J.M., Jr., Einaudi, M.T., Zürcher, L., Stavast, W.J.A., et al., 2005, Porphyry deposits: Characteristics and origin of hypogene features: Economic Geology, 100th Anniversary Volume, p. 251–298. (Selby and Creaser, 2001a) Selby, D. and Creaser, R.A., 2001a, Late and mid-Cretaceous mineralization in the northern Canadian Cordillera: Constraints from Re–Os molybdenite dates: Economic Geology, v. 96, p. 1461–1467. (Selby and Creaser, 2001b) Selby and Creaser, 2001b, Re–Os geochronology and systematics in molybdenite from the Endako porphyry molybdenum deposit, British Columbia, Canada: Economic Geology, v. 96, p. 197–204. (Selby and Creaser, 2004) Selby, D. and Creaser, R.A., 2004, Macroscale NTIMS and microscale LA-MC-ICP-MS Re–Os isotopic analysis of molybdenite: Testing spatial restrictions for reliable Re–Os age determinations, and implications for the decoupling of Re and Os within molybdenite: Geochimica et Cosmochimica Acta, v. 68, p. 3897–3908. (Selby et al., 2002) Selby, D., Creaser, R.A., Hart, C.J.R., Rombach, C.S., Thompson, J.F.H., Smith, M., et al., 2002, Absolute timing of sulfide and gold mineralization: A comparison of Re–Os molybdenite and Ar–Ar mica methods from the Tintina Gold Belt, Alaska: Geology, v. 30, p. 791–794. (Selby et al., 2003) Selby, D., Creaser, R.A., Heaman, L.M., and Hart, C.J.R., 2003, Re–Os and U–Pb geochronology of the Clear Creek, Dublin Gulch, and Mactung deposits, Tombstone Gold Belt, Yukon, Canada: absolute timing relationships between plutonism and mineralization: Canadian Journal of Earth Sciences, v. 40, p. 1839–1852. (Selby et al., 2004) Selby, D. and Creaser, R.A., and Feely, M., 2004, Accurate and precise Re–Os molybdenite dates from the Galway Granite, Ireland. Critical comment on "Disturbance of the Re–Os chronometer of molybdenites from the late-Caledonian Galway Granite, Ireland, by hydrothermal fluid circulation" by Suzuki et al., Geochemical Journal, 35, 29-35, 2001: Geochemical Journal, v. 38, p. 291–294. (Selby et al., 2007) Selby, D., Creaser, R.A., Stein, H.J., Markey, R.J., and Hannah, J.L., 2007, Assessment of the 187Re decay constant by cross calibration of Re–Os molybdenite and U–Pb zircon chronometers in magmatic ore systems: Geochimica et Cosmochimica Acta, v. 71, p. 1999–2013. (Shen et al., 2013) Shen, P., Pan, H.D., Xiao, W.J., Chen, X.H., Eleonorad, S., and Shen, Y.C., 2013, Two geodynamic–metallogenic events in the Balkhash (Kazakhstan) and the West Junggar (China): carboniferous porphyry Cu and Permian greisen W–Mo mineralization: International Geology Review, v. 55, p. 1660–1687. (Sillitoe et al., 2017) Sillitoe, R., Perello, J., Creaser, R., Wilton, J., Wilson, A., and Dawborn, T., 2017, Age of the Zambian Copperbelt. Mineralium Deposita 52: 1245-1268. (Simmonds and Moazzen, 2015) Simmonds, V., and Moazzen, M., 2015, Re-Os dating of molybdenites from Oligocene Cu-Mo-Au mineralized veins in the Qarachilar area, Qaradagh batholith (northwest Iran): implications for understanding Cenozoic mineralization in South Armenia, Nakhchivan, and Iran. International Geology Review 57.3: 290-304. (Sinclair et al., 2009) Sinclair, W.D., Jonasson, I.R., Kirkham, R.V., and Soregaroli, A.E., 2009, Rhenium and other platinum-group metals in porphyry deposits: Geological Survey of Canada Open File 6181, 1 p. (Sinclair, 2007) Sinclair, W.D., 2007, Porphyry deposits, in Goodfellow, W.D., ed., Mineral deposits of Canada: A synthesis of major deposit-types, district metallogeny, the evolution of geological provinces, and exploration methods: Geological Association of Canada, Mineral Deposits Division Special Publication 5, p. 223–243. (Singer et al., 2008) Singer, D.A. and Berger, V.I., and Moring, B.C., 2008, Porphyry Copper Deposits of the World: Database And Grade and Tonnage Models: U.S. Geological Survey Open-File Report 2008–1155 (http://pubs.usgs.gov/of/2008/1155). (Skirrow et al., 2007) Skirrow, R.G., Bastrakov, E.N., Barovich, K., Fraser, G.L., Creaser, R.A., Fanning, M., et al., 2007, Timing of iron oxide Cu–Au–(U) hydrothermal activity and Nd isotope constraints on metal sources in the Gawler craton, south Australia: Economic Geology, v. 102, p. 1441–1470. (Somarin and Ashley, 2004) Somarin, A.K. and Ashley, P., 2004, Hydrothermal alteration and mineralisation of the Glen Eden Mo–W–Sn deposit: a leucogranite-related hydrothermal system, southern New England Orogen, NSW, Australia: Minerallium Deposita, v. 39, p. 282–300. (Sotnikov et al., 2001) Sotnikov, V.I., Berzina, A.N., Economou-Eliopoulos, M., and Eliopoulos, D.G., 2001, Palladium, platinum and gold distribution in porphyry Cu±Mo deposits of Russia and Mongolia: Ore Geology Reviews, v. 18, p. 95–111. (Stein and Bingen, 2002) Stein, H.J. and Bingen, B., 2002, 1.05-1.01 Ga Sveconorwegian metamorphism and deformation of the supracrustal sequence at Sæsvatn, South Norway: Re-Os dating of Cu-Mo mineral occurrences, in The timing and location of major ore deposits in an evolving orogen: Geological Society of London Special Publication 204, p. 319–335. (Stein et al., 1997) Stein, H.J., Markey, R.J., Morgan, J.W., Du, A.D., and Sun, Y., 1997, Highly precise and accurate Re–Os ages for molybdenite from the East Qinling molybdenum belt, Shaanxi Province, China: Economic Geology, v. 92, p. 827–835. (Stein et al., 1998) Stein, H.J., Sundblad, K., Markey, R.J., Morgan, J.W., and Motuza, G., 1998, Re–Os ages for Archean molybdenite and pyrite, Kuittila-Kivisuo, Finland and Proterozoic molybdenite, Kabeliai, Lithuania: testing the chronometer in a metamorphic and metasomatic setting: Minerallium Deposita, v. 33, p. 329–345. (Stein et al., 2001a) Stein, H.J., Markey, R.J., Morgan, J.W., Selby, D., Creaser, R.A., McCuaig, T.C., et al., 2001a, Re-Os Dating of Boddington Molybdenite, SW Yilgarn: Two Au Mineralization Events, Geoscience Australia, Record: International Archaean Symposium, 4th, Perth, 24-28 September 2001, Extended Abstracts, v. 37, p. 469–471. (Stein et al., 2001b) Stein, H.J., Markey, R.J., Morgan, J.W., Hannah, J.L., and Scherstén, A., 2001b, The remarkable Re–Os chronometer in molybdenite: how and why it works: Terra Nova, v. 13, p. 479–486. (Stein et al., 2004) Stein, H.J., Hannah, J.L., Zimmerman, A., Markey, R.J., Sarkar, S.C., and Pal, A.B., 2004, A 2.5 Ga porphyry Cu–Mo–Au deposit at Malanjkhand, central India: implications for Late Archean continental assembly: Precambrian Research, v. 134, p. 189–226. (Stein et al., 2006) Stein, H.J., Hannah, J.L., Zimmerman, A., and Markey, R.J., 2006, Mineralization and deformation of the Malanjkhand terrane (2,490-2,440 Ma) along the southern margin of the Central Indian Tectonic Zone: Minerallium Deposita, v. 40, p. 755–765. (Stein, 2006) Stein, H.J., 2006, Low-rhenium molybdenite by metamorphism in northern Sweden: Recognition, genesis, and global implications: Lithos, v. 87, p. 300–327. (Strashimirov et al., 2002) Strashimirov, S. and Petrunov, R., and Kanazirski, M., 2002, Porphyry-copper mineralization in the central Srednogorie zone, Bulgaria: Minerallium Deposita, v. 37, p. 587–598. (Su et al., 2007) Su, Y.P., Tang, H.F., Sylvester, P.J., Liu, C.Q., Qu, W.J., Hou, G.S., et al., 2007, Petrogenesis of Karamaili alkaline A-type granites from East Junggar, Xinjiang (NW China) and their relationship with tin mineralization: Geochemical Journal, v. 41, p. 341–357. (Sutphin et al., 2013) Sutphin, D.M., Hammarstrom, J.M., Drew, L.J., Large, D.E., Berger, B.R., Dicken, C.L., et al., 2013, Porphyry copper assessment of Europe, exclusive of the Fennoscandian Shield: U.S. Geological Survey Scientific Investigations Report 2010–5090–K, 197 p. (Suzuki and Masuda, 1993) Suzuki, K. and Masuda, A., 1993, The Re-Os age of molybdenite from the Hirase Ore Deposit, Japan, and its comparison with Rb-Sr and K-Ar ages for host rocks. Proc. Japan Acad. 69, 79-82.: Proceedings of the Japan Academy, v. 69, p. 79–82. (Suzuki et al., 1993) Suzuki, K. and Shimizu, H., and Masuda, A., 1993, Reliable Re–Os age for molybdenite: Geochimica et Cosmochimica Acta, v. 57, p. 1625–1628. (Suzuki et al., 1996) Suzuki, K. and Shimizu, H., and Masuda, A., 1996, Re Os dating of molybdenites from ore deposits in Japan: Implication for the closure temperature of the Re Os system for molybdenite and the cooling history of molybdenum ore deposits: Geochimica et Cosmochimica Acta, v. 60, p. 3151–3159. (Suzuki et al., 2000) Suzuki, K., Kagi, H., Nara, M., Takano, B., and Nozaki, Y., 2000, Experimental alteration of molybdenite: evaluation of the Re–Os system, infrared spectroscopic profile and polytype: Geochimica et Cosmochimica Acta, v. 64, p. 223–232. (Suzuki et al., 2001) Suzuki, K. and Feely, M., and O'Reilly, C., 2001, Disturbance of the Re–Os chronometer of molybdenites from the late-Caledonian Galway Granite, Ireland, by hydrothermal fluid circulation.: Geochemical Journal, v. 35, p. 29–35. (Taner et al., 1998) Taner, H. and Williams-Jones, A.E., and Wood, S.A., 1998, The nature, origin and physicochemical controls of hydrothermal Mo-Bi mineralization in the Cadillac deposit, Quebec, Canada: Minerallium Deposita, v. 33, p. 579–590. (Tarkian and Koopman, 1995) Tarkian, M. and Koopman, G., 1995, Platinum-group minerals in the Santo Thomas II (Philex), porphyry copper-gold deposit Luzon Island: Minerallium Deposita, v. 30, p. 39–47. (Tarkian and Stribrny, 1999) Tarkian, M. and Stribrny, B., 1999, Platinium group elements in porphyry copper deposits: a reconnaissance study: Mineralogy and Petrology, v. 65, p. 161–183. (Taylor, 2007) Taylor, B.E., 2007, Epithermal gold deposits, in Goodfellow, W.D., ed., Mineral deposits of Canada: A synthesis of major deposit-types, district metallogeny, the evolution of geological provinces, and exploration methods: Geological Association of Canada, Mineral Deposits Division Special Publication 5, p. 113–139. (Terada et al., 1967) Terada, K., Yoshimura, Y., Osaki, S., and Kiba, T., 1967, Determination of rhenium in molybdenite by neutron-activation analysis: Talanta, v. 14, p. 53–60. (Terada et al., 1971) Terada, K., Osaki, S., Ishihara, S., and Kiba, T., 1971, Distribution of rhenium in molybdenites from Japan: Geochemical Journal, v. 4, p. 123–141. (Tessalina and Plotinskaya, 2017) Tessalina, S., and Plotinskaya, O., 2017, Silurian to Carboniferous Re-Os molybdenite ages of the Kalinovskoe, Mikheevskoe, and Talitsa Cu- and Mo porphyry deposits in the Urals: Implications for geodynamic setting. Ore Geology Reviews 85: 174-180. (Torrealday et al., 2000) Torrealday, H.I., Hitzman, M.W., Stein, H.J., Markey, R.J., Armstrong, R., and Broughton, D., 2000, Re–Os and U–Pb dating of the vein-hosted mineralization at the Kansanshi copper deposit, northern Zambia: Economic Geology, v. 95, p. 1165–1170. (U.S. Geological Survey, 2005) U.S. Geological Survey, 2005, Mineral Resource Data System: Reston, Virginia (http://mrdata.usgs.gov/mrds). (Valencia et al., 2005) Valencia, V.A., Ruiz, J., Barra, F., Geherls, G., Ducea, M., Titley, S.R., et al., 2005, U–Pb zircon and Re–Os molybdenite geochronology from La Caridad porphyry copper deposit: insights for the duration of magmatism and mineralization in the Nacozari District, Sonora, Mexico: Minerallium Deposita, v. 40, p. 175–191. (Valencia et al., 2006) Valencia, V.A., Noguez-Alcántara, B., Barra, F., Ruiz, J., Gehrels, G., Quintanar, F., et al., 2006, Re–Os molybdenite and LA-ICPMS-MC U–Pb zircon geochronology for the Milpillas porphyry copper deposit: insights for the timing of mineralization in the Cananea District, Sonora, Mexico: Revista Mexicana de Ciencias Geológicas, v. 23, p. 39–53. (Voudouris et al., 2009) Voudouris, P.C., Melfos, V., Spry, P.G., Bindi, L., Kartal, T., Arikas, K., et al., 2009, Rhenium-rich molybdenite and rheniite in the Pagoni Rachi Mo–Cu–Te–Ag–Au prospect, northern Greece: implications for the Re geochemistry of porphyry-style Cu–Mo and Mo mineralization: The Canadian Mineralogist, v. 47, p. 1013–1036. (Voudouris et al., 2010) Voudouris, P.C., Melfos, V., Moritz, R., Spry, P.G., Ortelli, M., and Kartal, T., 2010, Molybdenite occurrences in Greece: Mineralogy, geochemistry and depositional environment: Congress of the Carpathian-Balkan Geological Association, 19th, Thessaloniki, 38982, Proceedings, v. 2, p. 369–378. (Voudouris et al., 2013) Voudouris, P.C., Melfos, V., Spry, P.G., Bindi, L., Moritz, R., Ortelli, M., et al., 2013, Extremely Re-rich molybdenite from porphyry Cu–Mo–Au prospects in northeastern Greece: mode of occurrence, causes of enrichment, and implications for gold exploration: Minerals, v. 3, p. 165–191. (Wan et al., 2014) Wan, B., Xiao, W.J., Han, C.M., Windley, B.F., Zhang, L.C., Qu, W.J., et al., 2014, Re–Os molybdenite age of the Cu–Mo skarn ore deposit at Suoerkuduke in East Junggar, NW China and its geological significance: Ore Geology Reviews, v. 56, p. 541–548. (Wang et al., 2008) Wang, Y.L., Pei, R.F., Li, J.W., Qu, W.J., Li, L., Wang, H.L., et al., 2008, Re–Os Dating of Molybdenite from the Yaogangxian Tungsten Deposit, South China, and Its Geological Significance: Acta Geologica Sinica (English Edition), v. 82, p. 820–825. (Wang et al., 2012) Wang, Z.H., Liu, Y.L., Liu, H.F., Guo, L.S., Zhang, J.S., and Xu, K.F., 2012, Geochronology and geochemistry of the Bangpu Mo–Cu porphyry ore deposit, Tibet: Ore Geology Reviews, v. 46, p. 95–105. (Wang et al., 2014) Wang, X.S., Bi, X.W., Leng, C.B., Zhong, H., Tang, H.F., Chen, Y., et al., 2014, Geochronology and geochemistry of Late Cretaceous igneous intrusions and Mo–Cu–(W) mineralization in the southern Yidun Arc, SW China: Implications for metallogenesis and geodynamic setting: Ore Geology Reviews, v. 61, p. 73–95. (Wang et al., 2015) Wang, Y., Zhao, C., Zhang, F., Liu, J., Wang, J., Peng, R., and Liu, B., 2015, SIMS zircon U-Pb and molybdenite Re-Os geochronology, Hf isotope, and whole-rock geochemistry of the Wunugetushan porphyry Cu-Mo deposit and granitoids in NE China and their geological significance. Gondwana Research 28: 1228-1245. (Wang et al., 2016) Wang, Y., Zhou, L., Gao, S., Li, J., Hu, Z., Lu, Y., and Hu, Z., 2016, Variation of molybdenum isotopes in molybdenite from porphyry and vein Mo deposits in the Gangdese metallogenic belt, Tibetan plateau and its implications. Mineralium Deposita 51: 201-210. (Wanhainen et al., 2005) Wanhainen, C., Billström, K., Martinsson, O., Stein, H.J., and Nordin, R., 2005, 160 Ma of magmatic/hydrothermal and metamorphic activity in the Gällivare area: Re–Os dating of molybdenite and U–Pb dating of titanite from the Aitik Cu–Au–Ag deposit, northern Sweden: Minerallium Deposita, v. 40, p. 435–447. (Wanhainen et al., 2014) Wanhainen, C., Nigatu, W., Selby, D., McLeod, C., Nordin, R., and Bolin, N., 2014. The distribution, character, and rhenium content of molybdenite in the Aitik Cu-Au-Ag-(Mo) deposit and its southern extension in the northern Norrbotten ore district, northern Sweden. Minerals 4: 788-814. (Watanabe and Stein, 2000) Watanabe, Y. and Stein, H.J., 2000, Re–Os ages for the Erdenet and Tsagaan Suvarga porphyry Cu–Mo deposits, Mongolia, and tectonic implications: Economic Geology, v. 95, p. 1537–1542. (Wilson et al., 2007) Wilson, A.J., Cooke, D.R., Stein, H.J., Fanning, M., Holliday, J.R., and Tedder, I.J., 2007, U–Pb and Re–Os geochronologic evidence for two alkalic porphyry ore-forming events in the Cadia District, New South Wales, Australia: Economic Geology, v. 102, p. 3–26. (Wu et al., 2011) Wu, H.Y., Zhang, L.C., Wan, B., Chen, Z.G., Xiang, P., Pirajno, F., et al., 2011, Re–Os and 40Ar/39Ar ages of the Jiguanshan porphyry Mo deposit, Xilamulun metallogenic belt, NE China, and constraints on mineralization events: Minerallium Deposita, v. 46, p. 171–185. (Wu et al., 2017) Wu, G., Li, X., Xu, L., Wang, G., Liu, J., Zhang, T., Quan, Z., Wu, H., Li, T., Zeng, Q., and Chen, Y., 2017, Age, geochemistry, and Sr-Nd-Hf-Pb isotopes of the Caosiyao porphyry Mo deposit in Inner Mongolia, China. Ore Geology Reviews 81: 706-727. (X.F. Li et al., 2014) Li, X.F., Wang, C.Z., Mao, W., Xu, Q.H., and Liu, Y.H., 2014, The fault-controlled skarn W–Mo polymetallic mineralization during the main India–Eurasia collision: Example from Hahaigang deposit of Gangdese metallogenic belt of Tibet: Ore Geology Reviews, v. 58, p. 27–40. (Xiao et al., 2014) Xiao, B., Li, Q.G., Liu, S.W., Wang, Z.Q., Yang, P.T., Chen, J.L., et al., 2014, Highly fractionated Late Triassic I-type granites and related molybdenum mineralization in the Qinling orogenic belt: Geochemical and U–Pb–Hf and Re–Os isotope constraints: Ore Geology Reviews, v. 56, p. 220–233. (Xie et al., 2007) Xie, G.Q., Mao, J.W., Li, R.L., Qü, W.J., Pirajno, F., and Du, A.D., 2007, Re–Os molybdenite and Ar–Ar phlogopite dating of Cu–Fe–Au–Mo (W) deposits in southeastern Hubei, China: Mineralogy and Petrology, v. 90, p. 249–270. (Xie et al., 2011) Xie, G.Q., Mao, J.W., Zhao, H.J., Wei, K.T., Jin, S.G., Pan, H.J., et al., 2011, Timing of skarn deposit formation of the Tonglushan ore district, southeastern Hubei Province, Middle-Lower Yangtze River Valley metallogenic belt and its implications: Ore Geology Reviews, v. 43, p. 62–77. (Xie et al., 2017) Xie, G., Mao, J., Wang, R., Meng, D., Sun, J., Dai, J., Ren, T., Li, J., and Zhao, H., 2017. Origin of the Lengshuigou porphyry-skarn Cu deposit in the Zha-Shan district, South Qinling, central China, and implications for differences between porphyry Cu and Mo deposits. Mineralium Deposita 52: 621-639. (Xu et al., 2011) Xu, X.C., Lou, J.W., Xie, Q.Q., Xiao, Q.X., Liang, J.F., and Lu, S.M., 2011, Geochronology and tectonic setting of Pb–Zn–Mo deposits and related igneous rocks in the Yinshan region, Jinzhai, Anhui province, China: Ore Geology Reviews, v. 43, p. 132–141. (Xu et al., 2012) Xu, L.L., Bi, X.W., Hu, R.Z., Zhang, X.C., Su, W.C., Qu, W.J., et al., 2012, Relationships between porphyry Cu–Mo mineralization in the Jinshajiang-Red River metallogenic belt and tectonic activity: Constraints from zircon U–Pb and molybdenite Re–Os geochronology: Ore Geology Reviews, v. 48, p. 460–473. (Xu et al., 2016) Xu, D., Wu, C., Hu, G., Chen, M., Fu, Y., Wang, Z., Chen, H., and Hollings, P., 2016, Late Mesozoic molybdenum mineralization on Hainan Island, South China: Geochemistry, geochronology and geodynamic setting. Ore Geology Reviews 72: 402-433. (Y. Li et al., 2017) Li, Y., Selby, D., Feely, M., Costanzo, A., and Li, X., 2017, Fluid inclusion characteristics and molybdenite Re-Os geochronology of the Qulong porphyry copper-molybdenum deposit, Tibet. Mineralium Deposita 52: 137-158. (Y. Yang et al., 2017) Yang, Y., Wang, P., Chen, Y., and Li, Y., 2017, Geochronology and geochemistry of the Tianmugou Mo deposit, Dabie Shan, eastern China: Implications for ore genesis and tectonic setting. Ore Geology Reviews 81: 484-503. (Z. Wang et al., 2017) Wang, Z., Wang, K., Wan, D., Knoare, Y., Yang, T., and Liang, Y., 2017, Metallogenic age and hydrothermal evolution of the Jidetun Mo deposit in central Jilin Province, northeast China: Evidence from fluid inclusions, isotope systematics, and geochronology. Ore Geology Reviews 89: 731-751. (Zachariáš et al., 2001) Zachariáš, J., Pertold, Z., Pudilová, M., Žák, K., Pertoldová, J., Stein, H.J., et al., 2001, Geology and genesis of Variscan porphyry-style gold mineralization, Petráčkova hora deposit, Bohemian Massif, Czech Republic: Minerallium Deposita, v. 36, p. 517–541. (Zeng et al., 2010) Zeng, Q.D., Liu, J.J., Qin, F., and Zhang, Z.L., 2010, Geochronology of the Xiaodonggou Porphyry Mo Deposit in northern Margin of North China Craton: Geochronology of Xiaodonggou Deposit: Resource Geology, v. 60, p. 192–202. (Zeng et al., 2012) Zeng, Q.D., Chu, S.X., Liu, J.M., Sun, S., and Chen, W.J., 2012, Mineralization, alteration, structure, and Re–Os age of the Lanjiagou porphyry Mo deposit, North China Craton: International Geology Review, v. 54, p. 1145–1160. (Zeng et al., 2014) Zeng, Q., Liu, J., Chu, S., Wang, Y., Sun ,Y., Duan, X., Zhou, L., and Qu, W., 2014, Re-Os and U-Pb geochronology of the Duobaoshan porphyry Cu-Mo-(Au) deposit, northeast China, and its geological significance. Journal of Asian Earth Sciences 79: 895-909. (Zhang et al., 2005) Zhang, L.C., Xiao, W.J., Qin, K.Z., Qu, W.J., and Du, A.D., 2005, Re–Os isotopic dating of molybdenite and pyrite in the Baishan Mo–Re deposit, eastern Tianshan, NW China, and its geological significance: Minerallium Deposita, v. 39, p. 960–969. (Zhang et al., 2009) Zhang, L.C., Wu, H.Y., Wan, B., and Chen, Z.G., 2009, Ages and geodynamic settings of Xilamulun Mo–Cu metallogenic belt in the northern part of the North China Craton: Gondwana Research, v. 16, p. 243–254. (Zhang et al., 2015) Zhang, F., Wang, Y., Liu, J., and Wang, J., 2015, Zircon U-Pb and molybdenite Re-Os geochronology, Hf isotope analyses, and whole-rock geochemistry of the Donggebi Mo deposit, eastern Tianshan, Northwest China, and their geological significance. International Geology Review 57.4: 446-462. (Zhang et al., 2016) Zhang, P., Zhao, Y., Kou, L., Yang, H., and Yang, F., 2016. Zircon U-Pb and molybdenite Re-Os geochronology of copper-molybdenum deposits in southeast Liaoning Province, China. International Geology Review 58.12: 1481-1491. (Zhao et al., 2013) Zhao, X.F., Zhou, M.F., Li, J.W., Selby, D., Li, X.H., and Qi, L., 2013, Sulfide Re–Os and Rb–Sr isotope dating of the Kangdian IOCG metallogenic province, southwest China: implications for regional metallogenesis: Economic Geology, v. 108, p. 1489–1498. (Zhao et al., 2014) Zhao, J.X., Qin, K.Z., Li, G.M., Li, J.X., Xiao, B., Chen, L., et al., 2014, Collision-related genesis of the Sharang porphyry molybdenum deposit, Tibet: Evidence from zircon U–Pb ages, Re–Os ages and Lu–Hf isotopes: Ore Geology Reviews, v. 56, p. 312–326. (Zhao et al., 2017) Zhao, X., Xue, C., Chi, G., Mo, X., Nurtaev, B., and Zhang, G., 2017, Zircon and molybdenite geochronology and geochemistry of the Kalmakyr porphyry Cu-Au deposit, Almalyk district, Uzbekistan: Implications for mineralization processes. Ore Geology Reviews 86: 807-824. (Zheng et al., 2015) Zheng, W., Mao, J., Zhao, C., Ouyang, H., and Wang, X., 2015. Re-Os geochronology of molybdenite from Yinyan porphyry Sn deposit in South China. Resource Geology 66.1: 63-70. (Zhirov and Ivanova, 1959) Zhirov, K.K. and Ivanova, G.F., 1959, Zhirov, K. K., and Ivanova, G. F., 1959, The distribution of rhenium in molybdenites from deposits of a series of genetic types: Geokhimiya, 1959, No. 6, p. 518–523 (in Russian): , v. 6, p. 518–523. (Zhong et al., 2014) Zhong, J., Chen, Y.J., Pirajno, F., Chen, J., Li, J., Qi, J.P., et al., 2014, Geology, geochronology, fluid inclusion and H–O isotope geochemistry of the Luoboling Porphyry Cu–Mo deposit, Zijinshan Orefield, Fujian Province, China: Ore Geology Reviews, v. 57, p. 61–77. (Zhong et al., 2017) Zhong, J., Chen, Y., and Pirajno, F., 2017, Geology, geochemistry and tectonic settings of the molybdenum deposits in South China: A review. Ore Geology Reviews 81:829-855. (Zhou et al., 2012) Zhou, Q., Jiang, Y., Zhao, P., Liao, S., and Jin, G., 2012, Origin of the Dexing Cu-bearing porphyries, SE China: elemental and Sr-Nd-Pb-Hf isotopic constraints. International Geology Review 54.5: 572-592. (Zhou et al., 2013) Zhou, L., Zeng, Q., Liu, J., Friis, H., Zhang, Z., and Duan, X., 2013, Geochronology of the Xingshan molybdenum deposit, Jilin Province, NE China, and its Hf isotope significance. Journal of Asian Earth Sciences 75: 58-70. (Zimmerman et al., 2008) Zimmerman, A., Stein, H.J., Hannah, J.L., Koželj, D., Bogdanov, K., and Berza, T., 2008, Tectonic configuration of the Apuseni–Banat—Timok–Srednogorie belt, Balkans-South Carpathians, constrained by high precision Re–Os molybdenite ages: Minerallium Deposita, v. 43, p. 1–21. (Zimmerman et al., 2014) Zimmerman, A., Stein, H.J., Morgan, J.W., Markey, R.J., and Watanabe, Y., 2014, Re–Os geochronology of the El Salvador porphyry Cu–Mo deposit, Chile: Tracking analytical improvements in accuracy and precision over the past decade: Geochimica et Cosmochimica Acta, v. 131, p. 13–32. EXPLANATION OF TERMS IN APPENDIX A

SAMPLE TYPES DESCRIPTION ANALYSIS TYPEDESCRIPTION concentrate, unknown method molybdenite samples concentrated to high purity but method not described EPMA electron probe microanalyzer condensate gas sample collected and cooled to condense sublimated phases ICP-MS inductively coupled plasma mass spectrometer drill core drill core assay with Mo and Re values ID isotope dilution flotation concentrate high-purity molybdenite concentrate produced by froth flotation, either in a mill or a lab LA laser ablation hand samples sampling method described as hand sample or drill core sample collection but without further detail as to preparation MS mass spectrometer hand-picked flotation concentrate hand-picked flotation concentrate NAA neutron activation analysis hand-picked grains hand-picked grains NTIMS negative thermal ionization mass spectrometry hand-picked heavy liquids concentrate hand-picked heavy liquids concentrate SEM scanning electron microscopy hand-picked magnetic concentrate hand-picked magnetic concentrate TIMS thermal ionization mass spectrometry hand-picked magnetic/heavy liquids concentrate hand-picked magnetic/heavy liquids concentrate hand-picked magnetic/heavy liquids/HF concentrate hand-picked magnetic/heavy liquids/HF concentrate magnetic and heavy liquid concentrate sample concentrated by magnetic separation and heavy liquids but no additional processing mentioned magnetic concentrate sample concentrated by magnetic separation but no additional processing mentioned micro-drilled hand samples molybdenite obtained by precision drilling of macroscopic grains Mo powder powdered molybdenite produced by undescribed method polished mounts highly polished epoxy mounts, blocks, or thin sections of rocks thin sections petrographic thin sections unknown not described in reference various reference includes multiple undifferentiated sample types APPENDIX C

1. Abdar: Porphyry Cu based on Agazhadeh et al., 2015; no resource is reported, so this deposit could belong in the porphyry Cu-Mo class. 2. Adanac, Glacier Gulch: Porphyry Mo based on Nelson and Colpron, 2007, Tectonics and metallogeny of the British Columbia, Yukon and Alaskan Cordillera, Mineral Deposits of Canada. 3. Aigedzor: Clearly porphyry Cu-Mo based on multiple references including Moritz et al., 2016, Gondwana Research 4. Airshoko: Identified as greisen Mo-Sn-W based on description of “cassiterite- wolframite-molybdenite (high-temperature)” in Fleischer, 1960. 5. Aittojarvi: Granite Mo based on Frietsch, 1991, New ore types in the northern part of the Fennoscandian shield, Geologiska Foreningen. 6. Aksug, Ankavan: Porphyry Cu-Mo based on Berzina et al.. 7. Aktogai, Kounrad, Borly: Porphyry Cu based on Shen et al., 2013, Two geodynamic-metallogenic events in the Balkhash, International Geology Review. 8. Alford: IOCG based on Skirrow et al., 2007, Timing of iron oxide Cu-Au-(U) hydrothermal activity and Nd isotope constraints on metal sources in the Gawler craton, south Australia, Economic Geology. 9. Allatu, Metchagoja, Lobash, Jalonvaara, Bergaul: Porphyry Cu-Mo based on Lavrov and Kuleshevich. 10. Allebuoda, Kataberget, Munka: Granite Mo based on Stein, 2006, Low-rhenium molybdenite by metamorphism in northern Sweden: Recognition, genesis, and global implications, Lithos. 11. Alpeiner Scharte: Quartz vein-hosted Mo based on Langthaler et al., 2004, Molybdenum mineralization at Alpeiner Scharte, Tyrol, Mineralogy and Petrology. 12. Altenberg: Greisen Sn based on Romer et al., 2007, Dating multiply overprinted Sn-mineralized granites, Mineralium Deposita. 13. Amanan-Makit, Amudzhikan: Porphyry Mo based on Berzina et al., 2005. No other references were found. 14. Ambalavayal: Granite Mo based on Santosh, 1988, Granite-molybdenite system of Ambalavayal, Kerala, Geological Society of India. 15. American Eagle: Porphyry Cu based on McCandless et al.. 16. Andacollo: Classified as porphyry based on Reyes, 1991, The Andacollo strata- bound gold deposit, Chile, and its position in a porphyry copper-gold system, Economic Geology; however, other geologists consider Andacollo an IOCG. 17. Anticlimax: Porphyry Mo based on Sinclair, 2007., and on Stevenson, 1940, Molybdenum deposits of British Columbia, BC Department of Mines Bull, 9. 18. Antietam Reservoir: Tentatively identified as granite Mo based on descriptions in Pierotti et al., 2006, Re-Os Molybdenite Ages for the Antietam Reservoir, Eastern Pennsylvania, a Story of Open System Behavior Re-Os Isotopes in Molybdenite, GSA Abstracts with Programs. No other references were found. 19. Arburese: Porphyry Mo based on Boni et al.. 20. Arendal: Tentatively classified as skarn Fe based on Bugge, 1951, Minerals from the skarn iron ore deposits at Arendal, Norway. 21. Assarel: Porphyry Cu based on Voudouris et al., 2013. 22. Axiopoulis: Porphyry Mo based on Voudouris et al., 2010, Molybdenite occurrences in Greece, Proceedings of the XIX CBGA Congress. Also called Axiopolis or Pigi. 23. Bagh Khoshk, Now Chun, Sar Kuh, Kuh Panj, Dar Alu, Kerver, Chah Firouzeh, Iju: Porphyry Cu based on Agazhadeh et al., 2015. 24. Baie des Moutons: Syenite Mo tentatively included in the porphyry class based on texture; Gauthier and Chartrand, 2005, Metallogeny of the Grenville province revisited, Canadian Journal of Earth Sciences. 25. Baishan: Porphyry Mo based on Han et al., 2014, Tectonic implications of Re-Os dating of molybdenite deposits, International Geology Review. 26. Baishiding: Porphyry Mo based on Zhong et al., 2017. 27. Baita Plai, Cerbia, Baita Bihor, Savarsin, Tincova, Valea Capisoara, Tincova, Dognecea, Oravita, Ciclova: Classification follows Zimmerman et al., 2008, Apuseni-Banat-Timok-Srednogorie belt, Balkans, Mineralium Deposita. Savarsin and Ciclova are listed as quartz vein-hosted based on descriptions but this is uncertain. 28. Baizhangyan: Skarn W-Mo based on Zhong et al., 2017. 29. Balzapamba, Telimbela: Porphyry Cu based on Schutte et al.. 30. Banchang: The deposit includes both porphyry and skarn Cu mineralization styles, but the samples in the database were all from the skarn type according to Mao et al., 2008. 31. Bancroft: Granite-related U based on Robinson, 1960, Economic uranium deposits in granitic dykes, Bancroft District, Ontario, Canadian Mineralogist. 32. Bangpu: Porphyry Cu-Mo based on Wang et al., 2012, Geochronology and geochemistry of the Bangpu Mo-Cu porphyry, Ore Geology Reviews. 33. Baogaocun: Porphyry Mo based on Xu et al., 2016, Late Mesozoic molybdenum mineralization on Hainan Island, Ore Geology Reviews. 34. Baoshan: Skarn Cu based on Ren et al., 2017, Magmatism and metallogenic mechanisms of the Baoshan Cu-polymetallic deposit, Ore Geology Reviews. 35. Basnayayla: Porphyry Cu based on Mirnejad et al., 2013, Linking Cu mineralization to host porphyry emplacement, Economic Geology. 36. Baxiannao: Classification is dubious but best matches the quartz vein-hosted W- Sn class, based on Mao et al., 2013, Major types and time-space distribution of Mesozoic ore deposits in South China, Mineralium Deposita. 37. BC Moly, Red Bird, Lucky Ship: Porphyry Mo based on Theodore, 1986, Descriptive model of porphyry Mo, USGS Bulletin 1693. 38. Beikengchang: Skarn Mo based on Zhong et al., 2017, Geology, geochemistry, and tectonic settings of the molybdenum deposits in South China, Ore Geology Reviews. 39. Big Bell: Intrusion-related Au based on Mueller et al., 1996, Constraints on the age of granitoid emplacement, metamorphism, gold mineralization, and subsequent cooling of the Archean greenstone terrane at Big Bell, Western Australia, Economic Geology. 40. Biggenden: Skarn Au based on Ray, 1998, Au skarns, Geological Fieldwork Paper 1998-1 of the British Columbia Ministry of Employment and Investment. 41. Blafoddalen: Quartz vein-hosted Mo-W based on Holwell et al., 2012. 42. Blomskog: Pegmatite based on Bingen et al., 2006, Molybdenite Re-Os dating constrains gravitational collapse of the Sveconorwegian orogen, Lithos. 43. Blue Tier: Granite Sn based on Groves, 1972, The geochemical evolution of tin- bearing granites in the Blue Tier batholith, Tasmania, Economic Geology. 44. Bondar-e-Hanza, Darreh Zar: Porphyry Cu-Mo based on Agazhadeh et al.. 45. Bora Creek: No details could be found for this deposit, which was tentatively classified as granite Mo based on the description in Riley, 1967. 46. Boshchekul: Porphyry Cu-Au based on Voudouris et al., 2013. 47. Boss Mountain: Porphyry Mo based on Voudouris et al., 2013, and Berzina et al., 2005. 48. Boy Scout: Pegmatite based on Giles and Schilling. 49. Brejui: Skarn W based on Beurlen, 1984, “Tactites” formed by Ca-Al metasomatism on amphiboles, Syngenesis and Epigenesis in the Formation of Mineral Deposits. 50. Brenda: Porphyry Cu-Mo based on Schindler, 1975, Rhenium and osmium in some Canadian ores, McMaster University Ph.D. Thesis. 51. Bronson Slope: Also called Bronson and porphyry Cu-Au type according to Voudouris et al., 2013, and Singer et al., 2005. 52. Brownstone: Skarn W based on Newberry, 1979. 53. Bugdaya, Davenda: Porphyry Mo based on Berzina et al.. 54. Cadia East, Cadia Hill, Cadia Quarry: Porphyry Au-Cu based on Wilson et al., 2007, U-Pb and Re-Os geochronologic evidence for two alkalic porphyry ore- forming events, Economic Geology. 55. Callie Soak: Unknown deposit tabulated in Morgan, 1968. If identical to the Callie deposit in Cook et al., 2013, Economic Geology, could be orogenic Au. 56. Cangrejos: Porphyry Au-Cu based on Schutte et al., 2012. 57. Carmi: Porphyry Mo based on Kenyon and Morton, 1978, The Carmi Mo-(U) deposit, southern British Columbia, Bulletin of the Canadian Institute of Mining and Metallurgy. However, this is dubious given the extraordinary UO2 content, which is not typical of porphyries. 58. Carpenter’s Gully: Granite Mo-W based on Denaro, T., 1992, Mineralization of the Stanthorpe-Texas area, in Willmott, W., Regional and Economic Geology of the New England District, Geol. Soc. Australia 1992 Field Conference. Also spelled Carpenters Gully. 59. Cash, Casino: Porphyry Cu-Mo based on Selby and Creaser, 2001. 60. Cassiar Moly, Storie: Porphyry Mo based on Panteleyev, 1980, Cassiar map-area (104P), British Columbia Ministry of Energy, Mines, and Petroleum Resources. 61. Catface: Porphyry Cu based on Sinclair et al., 2009. 62. Chagele: Porphyry Mo based on Wang et al., 2016, Variation of molybdenum isotopes in molybdenite from porphyry and vein Mo deposits, Mineralium Deposita. 63. Chalice, Westonia: Orogenic Au based on Duuring et al., 2007. 64. Chang’anchong: Porphyry Cu-Mo based on Xu et al., 2012, Relationships between porphyry Cu-Mo mineralization, Ore Geology Reviews. 65. Chaucha: Porphyry Cu based on Schutte et al., 2012. 66. Chengmenshan: Porphyry Cu based on Mao et al., 2003. 67. Chilu: Porphyry Mo based on Zhong et al., 2017. 68. Clark Lake: Porphyry Cu-Mo based on Selby and Creaser, 2004. 69. Cleo: Quartz vein-hosted Au based on Brown et al., 2002, Geochronological constraints on pre-, syn-, and postmineralization events at the world-class Cleo gold deposit, eastern Goldfields province, Western Australia: Economic Geology. Possibly also orogenic Au based on Duuring et al., 2007, Granitoid-associated orogenic, intrusion-related, and porphyry style metal deposits in the Archean Yilgarn craton, western Australia, Ore Geology Reviews. 70. Copaquirre: Porphyry Cu-Mo based on Berzina et al.. 71. Copper Hill: Breccia pipe based on Johnston and Lowell, 1961, Geology and origin of mineralized breccia pipes in Copper Basin, Arizona, Economic Geology. 72. Costelloe, Omey, Murvey, Mace Head, Kilkieran, and Inveran: Granite Mo based on Feely et al., 2010, Long-lived granite-related molybdenite mineralization at Connemara, western Irish Caledonites, Geological Magazine. 73. Cuajone: Porphyry Cu-Mo based on Mastemran et al., 2004, 40Ar/39Ar and Re- Os geochronology of porphyry copper-molybdenum deposits, Economic Geology. 74. Da’ao: Greisen W-Mo based on Guo et al., 2011, SHRIMP U-Pb (zircon), Ar-Ar (muscovite) and Re-Os (molybdenite) isotopic dating, Ore Geology Reviews. 75. Daheishan: Porphyry Mo based on Han et al., 2014, Re-Os age of molybdenite from the Daheishan Mo deposit, Resource Geology. 76. Dahu: Quartz vein-hosted Au based on Ni et al., 2012, Pb-Sr-Nd isotope constraints on the fluid source of the Dahu Au-Mo deposit in Qinling Orogen, central China, and implication for Triassic tectonic setting, Ore Geology Reviews. 77. Dahutang: Granite W based on Mao et al., 2013, Geology and molybdenite Re-Os age of the Dahutang granite-related veinlets-disseminated tungsten ore field, Ore Geology Reviews. 78. Dal’nensk: Identified as greisen Mo-Sn-W based on description of “cassiterite- wolframite-molybdenite (high-temperature)” in Fleischer, 1960. Mentioned by Gonevchuk, V., et al., 2005, Genesis of the Tigrinoe Tin Deposit, Geology of Ore Deposits, but type is unclear. 79. Dal’neye, Dzhindara, Elpin: Porphyry Cu based on Berzina et al.. 80. Dalen: Quartz vein-hosted based on Bingen et al., 2006. 81. Dastakert: Porphyry Cu-Mo based on Simmonds and Moazzen, 2015, Re-Os dating of molybdenites from Oligocene Cu-Mo-Au mineralized veins, International Geology Review. 82. Datuanshan: Skarn Cu based on Mao et al., 2006, Molybdenite Re-Os and albite 40Ar/39Ar dating of Cu-Au-Mo and magnetite porphyry systems, Ore Geology Reviews. The ores are stratabound but related to igneous intrusions. 83. Dawan: Porphyry and skarn Mo based on Mao et al., 1999. 84. Dawangzhuang: Porphyry and skarn Mo, subdivided as in Mao et al., 2008, Tectonic implications from Re-Os dating of Mesozoic molybdenum deposits, Geochimica et Cosmochimica Acta. 85. Dayinjian, Donggou: Porphyry Mo based on Mao et al., 2008. 86. Dazhuangke: Breccia-pipe Mo based on Mao et al., 1999. 87. Deepwater: Pegmatite Bi based on Riley, 1967. 88. Devgaon: Granitoid Mo based on Stein et al., 2006, Mineralization and deformation of the Malanjkhand terrane (2,490-2,440 Ma) along the southern margin of the Central Indian Tectonic Zone, Mineralium Deposita. 89. Dexing: Porphyry Cu based on Shuo et al., 2012, Geological characterics and ore- forming time, Acta Geologica Sinica. 90. Diamond Joe: Porphyry Cu based on Keith et al., 1983, Metallic mineral districts and production in Arizona, Arizona Geological Survey Bulletin 194. 91. Dimbulah: Unknown, probably W-Mo deposit type mentioned in Riley, 1967. 92. Dongbeigou: Porphyry Mo based on Zhang et al., 2016, Zircon U-Pb and molybdenite Re-Os geochronology of copper-molybdenum deposits in southeast Liaoning, International Geology Review. 93. Donggebi: Porphyry Mo based on Zhang et al., 2015, Zircon U-Pb and molybdenite Re-Os geochronology, Hf isotope analyses, and whole-rock geochemistry of the Donggebi Mo deposit, International Geology Review. 94. Drammen: Granite Mo based on Lerchbaumer and Audetat, 2013, The metal content of silicate melts and aqueous fluids, Economic Geology. 95. Dublin Gulch, Clear Creek: Intrusion-related Au based on Lang and Baker, 2001, Intrusion-related gold systems, Mineralium Deposita, and Selby et al., 2003, Re- Os and U-Pb geochronology of the Clear Creek, Dublin Gulch, and Mactung deposits, Tombstone Gold Belt, Yukon, Canada, Canadian Journal of Earth Sciences. 96. Dumitri Potok, Majdanpek, Veliki Krivelj: Classification follows Zimmerman et al.. 97. Duobaoshan: Porphyry Cu-Mo based on Mao et al., 1999. 98. East Kounrad, Zhanet, Akshatau, Suyunhe, Hongyuan: Greisen or quartz vein- hosted based on Shen et al., 2013. Akshatau is also spelled Akchatau. The descriptions strongly suggest that the division between quartz vein-hosted and greisen types is gradational. 99. Ebisu: Quartz vein-hosted based on Shibata and Ishihara, 1974, K-Ar ages of the major tungsten and molybdenum deposits in Japan, Economic Geology. 100. El Creston: Porphyry Cu based on Damon et al., 1983, Geochronology of the porphyry copper deposits and related mineralization of Mexico, Metallogeny and Tectonics of the North American Cordillera. 101. El Tierrero, Guaysimi-David: Skarn Au based on Chiaradia et al., 2009. 102. Elsmore: Granite Sn based on Riley, 1968., and on Brown and Stroud, 1993, Mineralisation related to the Gilgai granite, Tingha-Inverell area, New England Orogen conference proceedings 1993. 103. Everton: Granodiorite Mo based on Blevin and Chappell. 104. Fakos: Porphyry Cu according to Voudouris et al., 2013. 105. Fenghuangshan: Skarn Cu based on Qu et al. 2012, Geology, geochemistry, and geochronology of the Fenghuangshan skarn-type copper deposit, Acta Geologica Sinica. 106. Fengshandong: Porphyry Cu-Mo based on Xie et al., 2007. 107. Flammefjeld: Porphyry Mo based on Holwell et al., 2012, An Re-Os date for molybdenite-bearing quartz vein mineralization, Economic Geology. 108. Flekkefjord: Granite Mo based on Hess, 1924, Molybdenum deposits: a short review, USGS Bull. 761. 109. Flinders Island: Classified as granite-related Mo but this is uncertain; Morgan et al. (op. cit.) only state that the molybdenite occurs within a granite. 110. Flottorp: Granite Mo based on Bingen et al., 2006. 111. Freiberg: Classified as a five-element-suite (polymetallic vein-type) deposit or district (Bastin, 1939, The nickel-cobalt-native silver ore type, Economic Geology). 112. Fukuoka: Tentatively classified as granite Mo based on Terada et al., 1971. 113. Fukuoko-Suien, Endani, Ida, Iyadani, Ichihata, Kaifu, Kakeya, Kamiyamasa, Kamo, Kamokura, Kawauchi, Kobayashiyama, Komaki, Minami Ikuchi, Nippo, Nisshin, Obayashi, Osa, Otome/Otomi, Owashe/Owashi, Shimizu, Shiratori, Shiro, Takagi, Takashiro, Tamatsukuri, Yamasa, Hiyoshi, Busshoji, Fukagadani, Ishizuchi: Quartz vein-hosted based on Ishihara, 1988. The relationship between this deposits and the granite Mo type is uncertain. 114. Gaby-Papa Grande: Porphyry Au based on Schutte et al., 2012, Metallogenic features of Miocene porphyry Cu, Mineralium Deposita. 115. Galeno: Voudouris et al., 2013, Extremely Re-rich molybdenite from porphyry Cu-Mo-Au prospects, Minerals. 116. Gameleira, Garimpo Fernando, Serra Verde: IOCGs based on Marschik et al., 2004, Late Archean Cu-Au-Mo mineralization at Gameleira and Serra Verde, Carajas Mineral Province, Brazil, Mineralium Deposita. 117. Gaotongling: Quartz vein-hosted Mo based on Xu et al., 2016. 118. Gaspe: Porphyry and skarn Cu based on Allcock, 1982, Skarn and porphyry copper mineralization at Mines Gaspe, Economic Geology. The samples in the database came from a molybdenite concentrate and porphyry/skarn origin was not stated. 119. Gibraltar, La Caridad, Mission: Porphyry Cu-Au based on Singer et al., 2005. 120. Gladstone: Unknown deposit with molybdenite Re measurement in Morgan et al.., but no other available references. 121. Glen Eden: Granite Mo based on Somarin et al., 2004, Hydrothermal alteration and mineralisation of the Glen Eden Mo-W-Sn deposit, Mineralium Deposita. There may be some overlap with the greisen class. 122. Grasberg: Porphyry Cu-Au based on Sinclair, 2007. 123. Gravelotte: Pegmatite based on McCandless et al., 1993 124. Guadalupe: Part of La Caridad porphyry Cu system, therefore classified as porphyry although pegmatites are locally dominant (Valencia et al., 2005, U-Pb zircon and Re-Os molybdenite geochronology from La Caridad porphyry copper deposit, Mineralium Deposita). 125. Gursli: This was classified as a metamorphosed granite Mo deposit based on Bingen et al., 2006, but the description given could also suggest a quartz vein- hosted categorization. 126. Haft Cheshmeh: Porphyry Cu-Mo based on Agazhadeh et al.. 127. Hagi, Kokurobe, Makari, Shinomachi: Tentatively identified as quartz vein-hosted based on Terada et al., 1971.; however, could have some affinities with the greisen group. 128. Hankus: Classified as pegmatite after Lavrov and Kuleshevich, 2010, The first finds of rhenium minerals in Karelia, Doklady Earth Sciences. No further details are given. 129. Harrachov, Krupka, Cinovec, Sadisdorf, Krasno, Jachymov, Celina, Mokrsko, Kasejovice, Vidly, Obri Dul, Stare Ransko, Bohutin, Cerna Hora, Cerna Voda, Derflice, Hurky, Fojtke u Liberce, Skalsko, Moldava, Vrchoslav, Padrt, Vsestary, Pribram, Kamenny Privoz, Skutec, Pohled, Kozi Hora, Stachlovice, Dolni Bory, Rozna, Vrancice: Classifications follow Pasava et al., 2016, Laser ablation ICPMS study of trace element chemistry in molybdenite coupled with scanning electron microscopy (SEM) – An important tool for identification of different types of mineralization, Ore Geology Reviews; and Ackerman et al., 2017, Temporal evolution of mineralization events in the Bohemian Massif inferred from the Re-Os geochronology of molybdenite, Mineralium Deposita. Bohutin data from Zak et al., 2014, Padrt Stock (Tepla-Barrandian Unit, Bohemian Massif): petrology, geochemistry… Journal of Geosciences. 130. Hata, Kamitani, Kongo-san: Tentatively classified as quartz vein-hosted deposits based on Terada et al., 1971., and Suzuki et al., 1996. 131. Heemskirk: Granite Sn based on Blevin and Campbell. 132. Herberton, Kingsgate, Wonbah, Bamford, and Wolfram: Classified as breccia pipe deposits based on description in Blanchard, R., 1947, Some pipe deposits of eastern Australia, Economic Geology; however, the relationship to the granite-related class is not clear. Wolfram is also called Wolfram Camp. 133. Highmont, Berg, Maggie: Porphyry Cu-Mo based on Singer et al., 2005. 134. Hilltop: Combines porphyry and epithermal characteristics and therefore could not be cleanly placed in either category (Ciobanu et al., 2013, Trace element heterogeneity in molybdenite fingerprints stages of mineralization, Chemical Geology). These data were not used in calculating any of the statistics presented. 135. Hnilec: Granite-related Sn-W-Mo based on Kohut and Stein, 2005, Re-Os dating of granite-related Sn-W-Mo mineralization at Hnilec, Gemeric Superunit, Slovakia, Mineralogy and Petrology. 136. Hongling: Quartz vein-hosted Mo based on Feng et al., 2015, Temporal consistency between granite evolution and tungsten mineralization in Huamei’ao, Ore Geology Reviews. However, Liang et al. (2016), Zircon U-Pb, molybdenite Re-Os, and muscovite Ar-Ar isotopic dating of the Xitian W-Sn polymetallic deposit, Ore Geology Reviews, list Hongling as a possible altered granite-related deposit as well as a possible quartz vein-hosted deposit. 137. Hongmenling: Porphyry Mo-W based on Xu et al., 2016, Late Mesozoic molybdenum mineralization on Hainan Island, Ore Geology Reviews. 138. Horado, Nakatatsu: Pb-Zn skarn according to Ishihara, 1988. 139. Huanglongpu: Could not be classified with other deposits as it displays many porphyry characteristics but is related to carbonatite rather than felsic or intermediate intrusions (Xu et al., 2010, A unique Mo deposit associated with carbonatites in the Qinling orogenic belt, central China, Lithos). This deposit was deemed sui generis in the database and was not used in calculating any of the statistics presented. 140. Huangshaping: Polymetallic and includes several mineralization styles; the samples in the database appear to be from the skarn Pb-Zn mineralization (Guo et al., 2011). 141. Huatong: Cu skarn based on Zhang, 2016, Zircon U-Pb and molybdenite Re-Os geochronology of copper-molybdenum deposits in southeast Liaoning, International Geology Review. 142. Huckleberry: Porphyry Cu based on Voudouris et al., 2013. 143. Hukeng: Quartz vein-hosted W based on Guo et al.. 144. Huky u Rakovnika: Carbonatite-related or fenite Pb-Zn deposit, sui generis; Ackerman et al., 2017. 145. Hvaleroyene: Tentatively classified as granite Mo based on location, local geology, and Fleischer. 146. Ingerbelle: Porphyry Cu-Au based on Voudouris et al., 2013 147. Io-zima: Volcanic sublimate based on Terada et al., 1971. 148. Island Copper: Porphyry Cu-Au based on Arancibia and Clark. 149. Jiama: Porphyry Cu based on Hou et al., 2009, The Miocene Gangdese porphyry copper belt, Ore Geology Reviews. 150. Jigongcun: Quartz vein-hosted Mo based on Wang et al., 2016. 151. Jiguanshan: Porphyry Mo based on Wu et al., 2011, Re-Os and 40Ar/39Ar ages of the Jiguanshan porphyry Mo deposit, Mineralium Deposita. 152. Jiguanzi, Taohuazui: Skarn Au-Cu based on Xie et al., 2011. 153. Jinduncheng: Porphyry Mo based on Mao et al., 1999. 154. Jingera: Classified as a breccia pipe based on description in Riley, 1967. 155. Jiru, Zhuonuo: Porphyry Mo based on Wang et al., 2016, Variation of molybdenum isotopes in molybdenite from porphyry and vein Mo deposits, Mineralium Deposita. 156. Jitoushan: Porphyry W-Mo based on Mao et al., 2013. 157. Junin: Porphyry Cu-Mo based on Schutte et al., 2012. 158. Kabeliai: Granite Cu-Mo based on Sundblad et al., 1994, Geology, geochemistry, and age of a Cu-Mo-bearing granite at Kabeliai, Southern Lithuania, Mineralogy and Petrology. 159. Kadzharan, Agarak: Porphyry Cu-Au based on Voudouris et al., 2013. 160. Kafang: Skarn and sediment-hosted Cu-Sn, divided after Cheng et al., 2012, Geology and genesis of Kafang Cu-Sn deposit, Ore Geology Reviews. 161. Kahang: Porphyry Cu-Mo based on Agazhadeh et al., 2015, Temporal- spatial distribution and tectonic setting of porphyry copper deposits in Iran, Ore Geology Reviews. 162. Kalinovskoe: Porphyry Cu-Mo based on Plotinskaya et al., 2015, Rhenium in ores of the Mikheevskoe porphyry Cu-Mo deposit, Geology of Ore Deposits. 163. Kalmakyr or Kal’makyr: Porphyry Cu-Mo based on Berzina et al.. 164. Kara Oba: Greisen W-Mo based on Mutschler et al., 1999, Giant porphyry-related metal camps of the world, USGS OFR 99-556. 165. Karacaali and Baliseyh: Granite Mo based on Delibas and Genc, 2012, Re-Os molybdenite ages of granitoid-hosted Mo-Cu occurrences from central Anatolia (Turkey), Ore Geology Reviews. 166. Keketuohai: Pegmatite based on Liu et al., 2014, New precise timing constraint, Ore Geology Reviews. 167. Kemess South, Taseko: Porphyry Cu-Au based on Singer et al., 2005. 168. Kenge, Porcupine: Orogenic Au based on Lawley et al., 2013, Re-Os molybdenite, pyrite, and chalcopyrite geochronology, Lupa goldfield, southwestern Tanzania, Economic Geology. 169. Keskin: Skarn Pb-Zn from Kuscu and Erler, 2010, Mineralization events in a collision-related setting, International Geology Review. May be different from the Keskin deposit referred to by Fleischer (1959), from whom the data come. 170. Kilkivan: Epithermal based on Riley, 1968., and Blake and Withnall, 2010, Geology and mineralization of the New England Orogen in Queensland, Proc. 2010 New England Orogen Conference. 171. Kimberley: Quartz-vein hosted Au, but possibly orogenic and/or granitoid-related, based on Vinyu et al., 1996, Timing between granitoid emplacement and associated gold mineralization, Canadian Journal of Earth Sciences. 172. Kimmeria: Porphyry Mo-W based on Voudouris et al., 2013. 173. King Island: Skarn W based on Kwak, 1978, Mass balance relationships and skarn-forming processes, American Journal of Science. 174. Kitsault: Porphyry Mo based on Voudouris et al., 2013. 175. Kivisuo: Quartz vein-hosted Au based on Stein et al., 1998, Re-Os ages for Archean molybdenite and pyrite, Mineralium Deposita. 176. Kliphoog, Narrap, Nababeep Far West, Tweedam: Quartz vein-hosted W based on Raith and Stein, 2000, Re-Os dating and sulfur isotope composition of molybdenite from tungsten deposits in western Namaqualand, Mineralium Deposita. 177. Kobberknuten, Langvatn: Virtually no references were found. The molybdenites at these sites occur in metabasalts and metagabbros, but, Hannah et al. (2007) Molybdenum isotope variations in molybdenite, Geology, attribute mineralization to metamorphism long after host rock formation. Classified as mafic-hosted metamorphic deposits on this basis. 178. Korongvale: Tentatively identified as granite-related Au based on Riley, 1967 but could be quartz vein-hosted as well. 179. Kowary, Graniczna, Siedlimowice, Borow, Andrzej, Paszowice, Lomnica Gorna, and Michalowice: Classified as a granite Mo deposits based on descriptions by Mikulski and Stein, 2007, Re-Os ages for molybdenite from the West Sudetes, SW Poland, AM Monograph No.1. 180. Kucing Liar: Skarn Cu based on Graham et al., 2004, Tracing Cu and Fe from source to porphyry, Chemical Geology. 181. Kuittila: Intrusion-related Au based on Stein et al., 1998. 182. Kulitu: Porphyry Cu-Mo based on Zhang et al., 2009, Ages and geodynamic settings of Xilamulun Mo-Cu metallogenic belt, Gondwana Research. 183. Kuridala: IOCG based on Beardsmore, 1992, Petrogenesis of Mount Dore- style breccia-hosted copper and gold mineralization in the Kuridala-Selwyn region of northwestern Queensland: thesis, James Cook University. 184. Kvinesdal, Sira, Vardal: Granite Mo based on Bingen et al., 2006. 185. Lady Ella, SWAN, Mount Dore, Mount Elliott, Starra: IOCGs based on Duncan et al., 2011, A new geochronological framework, Economic Geology. 186. Lahnanen: Granodiorite Mo based on Nurmi and Haapala, 1986, The Proterozoic granitoids of Finland, Bulletin of the Geological Society of Finland. 187. Lainejaur: Likely a VMS nickel deposit in the Boliden group, but this is not certain enough to list conclusively. 188. Lakange: Porphyry Cu-Mo based on Leng et al., 2015, Zircon U-Pb and molybdenite Re-Os ages of the Lakange porphyry Cu-Mo deposit, Resource Geology. 189. Lanjiagou: Quartz vein-hosted based on Dai et al., 2009, New U-Pb and Re-Os age data an the geodynamic setting of the Xiaojiayingzi Mo(Fe) deposit, Ore Geology Reviews. 190. Larap: Porphyry Cu-Mo based on Arancibia and Clark, 1999, Early magnetite-amphibole-plagioclase alteration-mineralization, Economic Geology. 191. Lavrion: This district includes intrusion-related, sediment-hosted, and granite-related systems; since all the data in the database came from articles by Voudouris et al., 2010, 2013., Lavrion is classified as an intrusion-related system following those authors’ system. 192. Leimengou, Shijiawan, Tangjiaping, Tianmugou: Porphyry Mo based on Mao et al., 2008. 193. Lengshuigou: Porphyry Cu based on Xie et al., 2017, Origin of the Lengshuigou porphyry-skarn Cu deposit, Mineralium Deposita. 194. Liikavaara, Salmijarvi: Somewhat enigmatic but classified as porphyry Cu based on apparent relationship to Aitik; Nigatu, 2011, Rhenium in the Aitik Cu- Au-Ag(-Mo) deposit, M.S. thesis, Lulea Univ. of Technology. 195. Linka: Skarn W based on Sherlock et al., 1996, Known mineral deposits and occurrences in Nevada, Nevada Bureau of Mines and Geology OFR 96-2. 196. Lipovy Log: Pegmatite based on Mao et al., 2003, Re-Os ages for the Shameika porphyry Mo deposit and the Lipovy Log rare metal pegmatite, Mineralium Deposita 197. Liushan: Porphyry Mo based on Han et al., 2014, Tectonic implications of Re-Os dating of molybdenum deposits, International Geology Review. Also appears in paper as Liushanshan. 198. Logtung: Porphyry Mo-W based on Sinclair et al., 2009. 199. Lorelei: Porphyry Cu-Mo based on McCandless et al., 1993. 200. Luoboling: Porphyry Cu-Mo based on Zhong et al., 2014, Geology, geochronology, fluid inclusion and H-O isotope geochemistry of the Luoboling porphyry Cu-Mo deposit, Ore Geology Reviews. 201. Luokuidong, Xincun: Porphyry Mo based on Xu et al., 2016. 202. Macksville: Tentatively assigned to granite Cu-W based on Riley, 1967. 203. Mactung: Skarn W from Selby et al., 2003. 204. Malanjkhand: Porphyry Cu based on Stein et al., 2006. 205. Maldon: Quartz vein-hosted Au based on Arne et al., 2001, Re-Os dating of sulfides associated with gold mineralization in central Victoria, Economic Geology. 206. Malmbjerg: Porphyry Mo based on Holwell et al.. 207. Malpica: Porphyry Cu based on Barra et al., 2005, Applications of the Re- Os isotopic system in the study of mineral deposits, Univ. Arizona Ph.D. thesis. 208. Maoping: Greisen W based on Feng et al., 2011, SHRIMP zircon U-Pb and molybdenite Re-Os isotopic dating of the tungsten deposits in the Tianmenshan-Hongtaoling W-Sn orefield, Ore Geology Reviews. 209. Maronia: Porphyry Cu-Mo based on Voudouris et al., 2010. 210. Masjed Daghi: Porphyry Cu-Au based on Agazhadeh et al., 2015.; however, also contains Mo. 211. Matasvaara: Greisen Mo-W based on Kotlyar et al., 1995, Descriptive, grade, and tonnage models for molybdenum-tungsten greisen deposits, USGS OFR 95-584. 212. Matou: Porphyry Cu-Mo based on Zhong et al.. 213. Medet: Porphyry Cu based on Singer et al., 2005. 214. Meiling: Porphyry Cu-Mo based on Xu et al., 2016. 215. Melitena, Myli: Porphyry Cu-Mo based on Voudouris et al., 2010, 2013. 216. Merlin: Classified here as IOCG based on the observation by Duncan et al (2014) that the Merlin system is indistinguishable from the clearly IOCG-type mineralization at Mount Dore (Duncan, R., et al., 2014, Structural and lithological controls on iron oxide copper-gold deposits of the southern Selwyn-Mount Dore corridor, Eastern fold belt, Queensland, Australia, Economic Geology). However, this is disputed; Babo et al., 2017, The high grade Mo-Re Merlin deposit, Cloncurry district, Australia, Economic Geology. Many unique aspects distinguish Merlin from conventional IOCG deposits, and with some hesitation we include it in that class because it is the closest fit of the available options. 217. Michiquillay: Porphyry Cu based Voudouris et al., 2013. 218. Middlesex, Moina: Quartz vein-hosted W-Sn based on Collins, 1974, Exploratory diamond drilling in the Moina area, Technical report of the Department of Mines of Tasmania. 219. Mikheev/Mikheevskoe, Talitsa: Porphyry Cu-Mo based on Tessalina and Plotinskaya, 2017, Silurian to Carboniferous Re-Os molybdenite ages, Ore Geology Reviews. 220. Milpillas: Porphyry Cu based on Valencia et al., 2006, Re-Os molybdenite and LA-ICP-MS-MC U-Pb zircon geochronology for the Milpillas porphyry copper deposit, Revista Mexicana de Ciencias Geologicas. 221. Mitchell: Porphyry Cu-Au based on Sinclair et al., 2009. 222. Molybdenum Corp of Canada: Tentatively identified as porphyry Mo based on Schindler’s (1975) reference to Sawkins, 1972. 223. Moonta, Pridhams, Wallarroo: IOCGs based on Skirrow et al., 2007. 224. Moss: Pegmatite Mo based on Lentz and Suzuki. 225. Mount Antero: Porphyry Mo with granitic affiliations; Barton and Young, 2002, Non-pegmatitic deposits of beryllium, Reviews in Mineralogy and Geochemistry 50. 226. Mount Bischoff: Skarn Sn based on Halley and Walshe, 1995, A reexamination of the Mount Bischoff cassiterite sulfide skarn, Economic Geology. However, some characteristics of the deposit indicate a possible relationship to greisen-type mineralization. 227. Mount Haskin: Porphyry Mo based on Sinclair, 2007. 228. Mount Lyell: VMS based on Galley et al., 2007, Volcanogenic massive sulfide deposits, Mineral Deposits of Canada. 229. Mount Merapi, Mount Momotombo, Mount St. Helens: Volcanic sublimate based on Bernard et al., 1990. 230. Mount Moliagul: Granodiorite Mo based on Blevin and Campbell, 1995, Chemistry, origin, and evolution of mineralized granites in the Lachlan fold belt, Australia, Economic Geology. 231. Mount Morgan: VMS based on Blake and Withnall, 2010, Geology and mineralization of the New England Orogen in Queensland, Proc. 2010 New England Orogen Conference. 232. Mount Mulat, S’Abba Gana, Punta de Salvia, Bivongi, Gonnosfanadiga: Granite Mo based on Paganelli, 1963, On rhenium content of molybdenite of Mount Mulat (Predazzo) and other Italian molybdenites, Geochimica et Cosmochimica Acta. 233. Mount Mulgine: Granite W based on Duuring et al., 2007, Granitoid- associated orogenic, intrusion-related, and porphyry style metal deposits, Ore Geology Reviews. 234. Mount Nansen: Fits in the general intrusion-related class although a possible porphyry-epithermal origin has been suggested; Hart and Langdon, 1997, Geology and mineral deposits of the Mount Nansen camp, Yukon, Yukon Exploration Geology; Saager and Bianconi, 1971, The Mount Nansen gold-silver deposit, Yukon territory, Canada, Mineralium Deposita. 235. Mount Perry: Tentatively identified as granite Mo based on Riley, 1967, but this is uncertain. 236. Mount Pleasant: Porphyry W-Sn based on Samson, 1990, Fluid evolution and mineralization in a subvolcanic granite stock, Economic Geology. 237. Mount Stanley, Bega, Queensgate, Sundown: Tentatively assigned to quartz vein-hosted based on Riley, 1967. Some overlap with the granite-related class is possible. 238. Mount Washington: Porphyry Cu based on Mueller, 1989, Tertiary low angle faulting and related gold and copper mineralization on Mount Washington, Geological Fieldwork. 239. Nambucca: Granite Mo based on Riley, 1967., but description could also match porphyry Mo. 240. Nannihu: Porphyry Mo-W based on Yang et al., 2012, Fluid inclusion study of the Nannihu giant porphyry Mo-W deposit, Ore Geology Reviews. 241. Nanyangshan, Shatanjiao: Skarn Cu-Mo based on Mao et al., 2006. 242. Naruo: Porphyry Cu-Au based on Zhu et al., 2015, Zircon U-Pb, molybdenite Re-Os, and K-feldspar 40Ar/39Ar dating of the Bolong porphyry Cu-Au deposit, Resource Geology. 243. Nianzigou: Porphyry Mo based on Zhang et al., 2013, Re-Os and U-Pb geochronology of porphyry Mo deposits in central Jilin province, International Geology Review. 244. Niuling, Zhangdou: Quartz vein-hosted W based on Feng et al., 2011. 245. Nucleus: Deposit contains both skarn and epithermal types of Au mineralization; Bineli Betsi et al., 2013. 246. OK: Porphyry Cu based on Sinclair et al., 2009, Rhenium and other platinum-group metals in porphyry deposits, TGA3 Cordillera. 247. Old Fort: Porphyry Cu based on Godwin, 1975, Imbricate subduction zones, Canadian Journal of Earth Sciences. 248. Onganja: Does not fit cleanly into any of the classifications but was categorized as metamorphic Cu-Au based on Moore, 2010, Comparative study of the Onganja copper mine, Namibia, South African Journal of Geology. Some affinities for the quartz vein-hosted class but vein mineralogy varies. 249. Orsdalen: Granite Mo based on Schonwandt and Peterson, 1983. 250. Otjozonjati: Classified as quartz vein-hosted based on brief description by Moore, 2010. 251. Paavaara: Porphyry Mo based on Sviridenko and Ivashchenko, 2000, Ore- bearing granites of Karelia, IMGRE. 252. Pagoni Rachi: Porphyry Cu-Mo based on Berzina et al., 2005, and Voudouris et al., 2013. 253. Panantza, Sutsu, San Carlos: Porphyry Cu-Mo based on Chiaradia et al., 2009, U-Pb, Re-Os, and 40Ar/39Ar geochronology of the Nambija Au-skarn and Pangui porphyry Cu deposits, Mineralium Deposita. 254. Pax Mine: Unknown. A locality for 3R molybdenite (Newberry.) but none of the available references gives any further description of the geology of the deposit. 255. Petrackova hora: Intrusion-related gold for sure, porphyry connection possible but not conclusive; Zacharias et al., 2001, Geology and genesis of Variscan porphyry-style gold mineralization, Petrackova hora deposit, Bohemian Massif, Czech Republic, Mineralium Deposita. 256. Pingdi, Shankou, Shizitou, Tongkengzhang, Xin’an, Zhilingtou, Lishan: Porphyry Mo based on Zhong et al., 2017. 257. Pogo, Fort Knox: Intrusion-related Au based on Hart, 2007, Reduced intrusion-related gold systems, Mineral Deposits of Canada. 258. Port Hedland: This is a city name and could refer to several ore deposits in the area, of different types. Accordingly, it has been left as Unknown. 259. Preissac-Lacorne: Granite Mo based on Mulja et al., 1995, The rare- element-enriched monzogranite-pegmatite-quartz vein systems in the Preissac- Lacorne Batholith, Canadian Mineralogist. 260. Premier: Tentatively classified as granite Mo based on brief description by Morgan et al..; no other references were found. 261. Qarachilar: Porphyry Cu-Mo based on Simmonds and Moazzen. 262. Qianjiawan: Skarn Cu-Au based on Xie et al., 2007, Re-Os molybdenite and Ar-Ar phlogopite dating, Mineralogy and Petrology. Also appears in paper as Qijiawan. 263. Qiaoxiahala: IOCG based on Li et al., 2014, Geology and geochemistry of the Qiaoxiahala Fe-Cu-Au deposit, Junggar region, northwest China, Ore Geology Reviews. 264. Qiushuwan: This deposit contains both porphyry Cu-Mo and skarn Mo types of mineralization. Samples were assigned to one or the other following Mao et al., 2008. 265. Qulong: Porphyry Cu-Mo based on Li et al., 2017, Fluid inclusion characteristics and molybdenite Re-Os geochronology of the Qulong porphyry copper-molybdenum deposit, Mineralium Deposita. 266. Ragunda: Granite Mo based on Selby et al., 2007, Assessment of the 187Re decay constant by cross calibration of Re-Os molybdenite and U-Pb zircon chronometers in magmatic ore systems, Geochimica et Cosmochimica Acta. 267. Ray, Cumobabi: Porphyry Cu-Mo based on Singer et al., 2005. 268. Red Hills: Classified as porphyry Cu-Mo based on Gilmer et al., 2003, Extension of Laramide magmatism, Geology; however, classification as porphyry Cu-Au may also be viable based on Singer et al., 2005. 269. Red Mountain: Porphyry Mo based on Brown and Kahlert, 1995, Geology and mineralization of the Red Mountain porphyry molybdenum deposit, Porphyry deposits of the Northwestern Cordillera of North America. 270. Renfrew: Skarn W based on Giles and Schilling., and on Lentz and Suzuki, 2000, A low F pegmatite-related Mo skarn, Economic Geology. 271. Revenue: Porphyry Cu-Au based on Bineli Betsi et al., 2013, Genesis of the Au-Bi-Cu-As, Cu-Mo+/-W, and base-metal Au-Ag mineralization at the Mountain Freegold, Mineralium Deposita. 272. Roundy Creek: Porphyry Mo based on Taylor et al., 2010. 273. Ruanjiawan: Skarn Cu based on Xie et al., 2007. 274. San Antonio: Skarn Cu based on Sillitoe, 2010, Porphyry copper systems, Economic Geology. 275. San Martin: Skarn Cu based on McCandless et al., 1993. 276. Sanaeda: Tentaively classified as a porphyry Mo deposit based on Terada et al.’s (1971.) description of both vein and disseminated ores. 277. Sandaozhuang, Shangfanggou: Deposits contain both porphyry and skarn Mo-W ores, divided according to Mao et al., 2008. 278. Santo Tomas II: Porphyry Cu-Au based on Tarkian and Koopmann, 1995, Platinum-group minerals in the Santo Tomas II (Philex) porphyry copper-gold deposit, Mineralium Deposita. 279. Sanzhishu: Porphyry Mo based on Zhong et al., 2017. 280. Sardes: Porphyry Cu-Mo based on Voudouris et al., 2013, although Voudouris et al., 2010 mentions that epithermal-style mineralization is also present. 281. Sary Cheku: Porphyry Cu-Mo based on Seltmann et al., 2011, Hercynian post-collisional magmatism, Journal of Asian Earth Sciences. 282. Schaft Creek: Porphyry Cu-Mo based on Scott et al., 2009, The Schaft Creek Porphyry Cu-Mo(-Au) deposit, Exploration and Mining Geology. 283. Sekigane: Greisen Mo based on Suzuki et al., 1996. 284. Sennai: Quartz vein-hosted based on Terada et al., 1971. 285. Seriphos: Porphyry Mo-W based on Voudouris et al., 2010. 286. Setting Net Lake: Porphyry Mo based on Ayres et al., 1982, An Archean molybdenite occurrence of possible porphyry type, Economic Geology. 287. Shakhtama: Porphyry Cu-Mo based on Berzina et al.. 288. Shalgiya: Porphyry Mo based on Berzina et al.. 289. Shameika: Porphyry Mo based on Mao et al., 2003. 290. Shand: Porphyry Cu-Mo based on Berzina et al., 2016, Paleozoic- Mesozoic porphyry Cu(Mo) and Mo(Cu) deposits, Minerals. 291. Sharang: Porphyry Mo based on Zhao et al., 2014, Collision-related genesis of the Sharang porphyry molybdenum deposit, Ore Geology Reviews. 292. Shedong: Porphyry W-Mo based on Zhong et al., 2017. 293. Shigushan, Shirenzhang, Taoxikeng: Quartz vein-hosted W based on Guo et al., 2011. 294. Shimenshan: Porphyry Mo based on Xu et al., 2016. 295. Shipingchuan: Quartz vein-hosted Mo based on Zhong et al., 2017. 296. Shirakawa, Hokuto, Hata, Takatori, Owashi/Owashe, Otome, Hirase, Daito, Higashiyama, Kamitani, Seikyu, Yamasi, Takakigawa, Komaki, Okawame, Fusamata, Sekigane: Classified after Suzuki et al., 1996, Re-Os dating of molybdenites form ore deposits in Japan, Geochimica et Cosmochimica Acta, and Terada et al.. 297. Shizhuyuan: Skarn W based on Guo et al., 2011. 298. Shouwangfei: Porphyry and skarn Cu-Mo ores, undifferentiated, based on Mao et al., 1999. 299. Shuikoushan: granodiorite Pb-Zn from Huang et al., 2015, Precise zircon U-Pb and molybdenite Re-Os dating of the Shuikoushan granodiorite-related Pb- Zn mineralization, southern Hunan, south China, Ore Geology Reviews. 300. Siah-Kamar: Porphyry Mo based on Nabatian et al., 2017, Whole rock geochemistry, molybdenite Re-Os geochronology, stable isotope and fluid inclusion investigations of the Siah-Kamar deposit, Ore Geology Reviews. 301. Sileurian Chieftain: Porphyry Cu-Mo based on de Geoffroy and Wignall 1972, A statistical study of geological characteristics of porphyry copper- molybdenum deposits, Economic Geology. 302. Sipalay: Porphyry Cu based on Sinclair, 2007. 303. Sodagawa: Granite Mo based on Terada et al., 1971. 304. Sonoma Pass: Pegmatite deposit based on classification by Giles and Schilling, 1972. No other references have been found. 305. Sora: Porphyry Cu-Mo based on Berzina et al.. 306. South Mountain Batholith: The batholith contains granites, greisens, pegmatites, and many other phases; details are lacking for the molybdenite Re values presented in Selby and Creaser, 2004. Based on preponderance of granites, the samples here are classified as granite-related Mo. 307. Squaw Peak: Porphyry Cu-Au based on Singer et al., 2005. 308. St. Helens: This location could match either granite-related W or vein- hosted Cu and has been left as Unknown in accordance with this uncertainty. See Walker, 1957, Geology of the St. Helens-Scamander area, Proceedings of the Royal Society of Tasmania. 309. Star: Skarn W-Mo based on McCandless et al., 1993. 310. Su Seinargiu: Granite Mo based on Boni et al., 2003, Re-Os age for molybdenite from SW Sardinia, Mineral Exploration and Sustainable Development. 311. Suoerkuduke: Skarn Cu-Mo based on Wan et al., 2014, Re-Os molybdenite age of the Cu-Mo skarn ore deposit at Suoerkuduke, Ore Geology Reviews. 312. Susap: Porphyry Cu-Mo based on MacLeod, 1989, Prospect evaluation report on the Susap property, Unpublished consulting report. 313. Taiyangshan: Porphyry Cu-Mo based on Qiu et al., 2016, Geologic and geochemical insights into the formation of the Taiyangshan porphyry copper- molybdenum deposit, Gondwana Research. 314. Takagigawa: Classified as unknown Mo since the descriptions by Suzuki et al., 1996, were not sufficient to identify it. 315. Telemark and Knaben: Classified as granite-related Mo based on descriptions by Schonwandt and Petersen, 1983, Continental rifting and porphyry- molybdenum occurrences in the Oslo region, Norway, Tectonophysics. Some of the characteristics described could also correspond to a porphyry origin. 316. Tempiute or Tem Piute: Skarn W according to Buseck, 1967, Contact metasomatism and ore deposition, Tem Piute, Nevada, Economic Geology. 317. Tenabo: Tentatively classified as porphyry Cu-Au based on Kelson et al., 2008, Geochemical and geochronological constraints on mineralization, Economic Geology. 318. Tepasto: Granite Mo based on Selby et al., 2007. 319. Thrudvang: Quartz vein-hosted Mo-W based on Rosa and Ulrich, 2015, A quartz-wolframite-molybdenite vein and scheelite in amphibole horizons from the Thrudvang peninsula, Geological Survey of Denmark and Greenland Bulleting. 320. Tidewater: Porphyry Mo based on Taylor et al., 2010, Arc-related porphyry molybdenum deposit model, USGS Mineral Deposit Model for Resource Assessment, Chapter D. 321. Tinggong: Porphyry Cu-Mo based on Hou et al.. 322. Tintaya: Porphyry Cu-Au based on Singer et al., 2005. 323. Tominskoe: Porphyry Cu based on Voudouris et al., 2013. 324. Tongchang: Porphyry Cu-Mo based on Xu et al., 2012, Relationships between porphyry Cu-Mo mineralization, Ore Geology Reviews. 325. Tongcun, Dabaoshan: Porphyry and skarn Mo based on Zhong et al., 2017. 326. Tongkuangli: Skarn Mo based on Mao et al., 2006. 327. Tongkuangyu: Porphyry Cu based on Mao et al., 1999, Re-Os isotopic dating of molybdenites in the Xiaoliugou W(Mo) deposit, Geochimica et Cosmochimica Acta. 328. Tonglushan: There are several types of skarns in this district but most are Au- and Cu-dominated, so the deposit type is given as skarn Au-Cu after Xie et al., 2011, Timing of skarn deposit formation of the Tonglushan ore district, Ore Geology Reviews. 329. Tongniujing: Quartz vein-hosted Cu-Au based on Gu et al., 2011, Comparative study of ore-forming fluids of hydrothermal copper-gold deposits, International Geology Review. 330. Tongshankou: Porphyry and skarn based on Li et al., 2008, Origin of the Tongshankou porphyry-skarn Cu-Mo deposit, eastern Yangtze craton, eastern China, Mineralium Deposita. 331. Travore: Quartz vein-hosted Mo based on Suzuki et al., 2001, Disturbance of the Re-Os chronometer of molybdenites, Geochemical Journal. 332. Tres Chorreras: Breccia pipe based on Schutte et al., 2012. 333. Tsagaan Suvarga: Porphyry Cu-Mo based on Watanabe and Stein, 2006, Re-Os ages for the Erdenet and Tsagaan Suvarga porphyry Cu-Mo deposits, Economic Geology. 334. Tumen: Intrusion-related Mo based on Deng et al., 2013, Re-Os geochronology, fluid inclusions and genesis of the 0.85 Ga Tumen molybdenite- fluorite deposit, Geological Journal. This deposit also bears some similarity to quartz vein-hosted Mo. 335. Tyrny-Auz/Tyrnyauz: Skarn W-Mo based on Kurdyukov, 1980, Lithologic control on mineralization in the Tyrnyauz deposit, International Geology Review. 336. Uchitomi, Kinpozan/Kimpuzan: Tentatively identified as quartz vein- hosted based on Terada et al., 1971., but the data are so scanty that this is doubtful. 337. Umal’ta: Quartz vein-hosted Mo based on Schneider et al., 2011, Complex mineralization at large ore deposits in the Russian far east, Geology of Ore Deposits. 338. Unkurtash: Porphyry Mo based on Berzina et al.. 339. Valley: Porphyry Cu based on Casselman et al., 1995, Highland Valley porphyry copper deposits near Kamloops, British Columbia: A review and update with emphasis on the Valley deposit, Canadian Institute of Mining, Metallurgy and Petroleum. 340. Vlaykov Vruh: Porphyry Cu based on Zimmerman et al., 2008. 341. Vulcan: IOCG based on Reid et al., 2014, Re-Os dating of molybdenite within hematite breccias from the Vulcan Cu-Au prospect, Olympic Cu-Au province, South Australia, Economic Geology. 342. Wangdian: Porphyry Cu based on Qiu et al., 2016, Paleozoic magmatism and porphyry Cu-mineralization, Journal of Asian Earth Sciences. 343. Wasagadawa, Yamatsuri, Atsuho: Granite Mo based on Ishihara, 1988, since only disseminated endogranitic mineralization is mentioned. 344. Whiting Creek, Lornex: Porphyry Cu-Mo based on Singer and Berger, 2006, Porphyry copper deposit density, Economic Geology. 345. Wilson’s Downfall: Granite Sn-Mo-W based on Cumming and Lowe, 2010, Using volcanic facies analysis to unlock the mineral potential of the Drake gold field, New England Orogen 2010. 346. Wunugetushan: Porphyry Cu-Mo based on Chen et al., 2011, Geochronlogy and geochemistry of the Wunugetushan porphyry Cu-Mo deposit, Ore Geology Reviews. 347. Xamchab: Pegmatite based on McCandless et al., 1993. 348. Xiaodonggou: Porphyry Mo based on Zeng et al., 2010, Geochronology of the Xiaodonggou porphyry Mo deposit, Resource Geology. 349. Xiaojiayingzi: Skarn Mo based on Dai et al., 2009, New U-Pb and Re-Os age data and the geodynamic setting of the Xiaojiayingzi Mo (Fe) deposit, Ore Geology Reviews. 350. Xiaoliugou: Samples were divided between quartz vein-hosted W and skarn W ores after Mao et al., 1999. 351. Xiaoshigou: Porphyry and skarn Mo based on Mao et al., 1999. 352. Xingluokeng: Porphyry Mo-W based on Zhong et al., 2017. 353. Xioabaishitou: Skarn W based on Deng et al., 2017, U-Pb zircon, Re-Os molybdenite geochronology and Rb-Sr geochemistry form the Xioabaishitou W (- Mo) deposit, Ore Geology Reviews. 354. Xiongcun: Porphyry Cu-Au based on Lang et al., 2014, U-Pb and Re-Os geochronological evidence for the Jurassic porphyry metallogenic event, Journal of Asian Earth Sciences. 355. Xiongjiashan: Quartz vein-hosted Mo based on Zhong et al., 2017. 356. Xitian: Skarn Sn-W based on Xu et al., 2006, Geological characteristics and ore-controlling factors of Xitian skarn-type W-Sn deposit in Hunan province, Geology and Mineral Resources of South China. 357. Yamato: Skarn Cu based on Ishihara, 1988 358. Yangakly, Vardenis: Porphyry Cu based on Berzina et al.. 359. Yaogangxian: Quartz vein-hosted W based on Guo et al., 2011. 360. Yaolanzai: Greisen Sn-W based on Feng et al., 2011. 361. Yea: Granite Mo-W based on Van Krieken and Wilson, 2016, Structural and timing constraints on molybdenum and tungsten mineralization at Yea, Australian Journal of Earth Sciences. 362. Yetholme: The district contains some pegmatites but is mostly skarn Mo- W according to Downes et al., 2004, World-class mineral deposits of the Lachlan orogen, Geological Survey of New South Wales. 363. Yinachang: IOCG based on Xiantao et al., 2013, Zircon U-Pb and chalcopyrite Re-Os geochronology, REE geochemistry of the Yinachang Fe-Cu- REE deposit in Yunnan Province and its geological significance, Acta Petrological Sinica. 364. Yinyan: Porphyry Sn based on Zheng et al., 2015, Re-Os geochronology of molybdenite from Yinyan, Resource Geology 365. Ylitornio: Presumably the same as the Rompas deposit in Finland, which is sui generis and does not fit any of the deposit models in this database. 366. Yuanzhuding: Porphyry Cu-Mo based on Zhong et al., 2017. 367. Yulong, Machangqing, Xifanping: Porphyry Cu-Mo based on Hou et al., 2006, Himalayan Cu-Mo-Au mineralization, Mineralium Deposita. 368. Zappa-Koffee, Pattison, Idaho Creek: Porphyry Cu-Mo based on Selby and Creaser, 2001, Late and mid-Cretaceous mineralization in the northern Canadian Cordillera, Economic Geology. 369. Zhaiwa: Porphyry Cu-Mo based on Deng et al., 2013, Metallogeny during continental outgrowth in the Columbia supercontinent, Ore Geology Reviews. 370. Zhifang: Quartz vein-hosted Mo based on Deng et al., 2016, Re-Os and Sr-Nd-Pb isotope constraints on source of fluids in the Zhifang Mo deposit, Gondwana Research. 371. Zhireken: Porphyry Cu-Mo based on Berzina et al.., and Sotnikov et al., 2001, Palladium, platinum, and gold distribution in porphyry Cu +/- Mo deposits of Russia and Mongolia, Ore Geology Reviews.