Usgs Open-File Report 02-303Epa, Mineral Commodity Profiles— Gold

Total Page:16

File Type:pdf, Size:1020Kb

Usgs Open-File Report 02-303Epa, Mineral Commodity Profiles— Gold PEBBLE PROJECT RECORD OF DECISION ENVIRONMENTAL IMPACT STATEMENT USGS OPEN-FILE REPORT 02-303EPA, MINERAL COMMODITY PROFILES— GOLD (BUTTERMAN AND AMEY III, 2005) Mineral Commodity Profiles—Gold By W.C. Butterman and Earle B. Amey III Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government Open-File Report 02-303 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia 2005 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. iii Contents Overview .............................................................................................................................................................................................1 Descriptive terms and units of measure........................................................................................................................................1 Historical background.......................................................................................................................................................................2 Gold in jewelry and ornamentation......................................................................................................................................2 Gold in other nonmonetary uses ..........................................................................................................................................3 Gold as a monetary metal......................................................................................................................................................3 Production and supply ...........................................................................................................................................................4 Mining in the United States...................................................................................................................................................8 Description........................................................................................................................................................................................10 Salient facts ...........................................................................................................................................................................10 Principal forms, alloys, compounds...................................................................................................................................10 Commercial grades, shapes, specifications ....................................................................................................................11 Sources .............................................................................................................................................................................................12 Primary....................................................................................................................................................................................12 Crustal abundance.....................................................................................................................................................12 Geochemistry..............................................................................................................................................................13 Mineralogy ..................................................................................................................................................................13 Gold deposits ..............................................................................................................................................................14 Reserves, reserve base, resources ........................................................................................................................16 Secondary ..............................................................................................................................................................................16 Other sources ........................................................................................................................................................................17 Production technologies ................................................................................................................................................................18 Exploration .............................................................................................................................................................................18 Mine development ................................................................................................................................................................18 Mining .....................................................................................................................................................................................19 Placer mining ..............................................................................................................................................................19 Lode mining .................................................................................................................................................................20 Ore processing ......................................................................................................................................................................21 Placer gold ..................................................................................................................................................................21 Lode gold .....................................................................................................................................................................22 Recycling...........................................................................................................................................................................................26 Uses ...................................................................................................................................................................................................27 Properties that determine use ............................................................................................................................................27 Use in industry and the arts ................................................................................................................................................27 Jewelry ........................................................................................................................................................................28 Electronic/electrical uses.........................................................................................................................................33 Dental and medical uses...........................................................................................................................................35 Other industrial uses..................................................................................................................................................37 Use as an investment good .................................................................................................................................................39 Competitive materials and processes ...............................................................................................................................39 Industry..............................................................................................................................................................................................39 Structure.................................................................................................................................................................................39 iv Mines ......................................................................................................................................................................................40 Refineries ...............................................................................................................................................................................42 Fabricators .............................................................................................................................................................................42 Jewelry ........................................................................................................................................................................42 Other manufacturers .................................................................................................................................................43 Traders....................................................................................................................................................................................43
Recommended publications
  • Toward the Crystal Structure of Nagyagite, [Pb(Pb,Sb)S2][(Au,Te)]
    American Mineralogist, Volume 84, pages 669–676, 1999 Toward the crystal structure of nagyagite, [Pb(Pb,Sb)S2][(Au,Te)] HERTA EFFENBERGER,1,* WERNER H. PAAR,2 DAN TOPA,2 FRANZ J. CULETTO,3 AND GERALD GIESTER1 1Institut für Mineralogie und Kristallographie, Universität Wien, Althanstrasse 14, A-1090 Vienna, Austria 2Institut für Mineralogie, Universität Salzburg, Hellbrunnerstrasse 34, A-5020 Salzburg 3Kärntner Elektrizitäts AG, Arnulfplatz 2, A-9021 Klagenfurt, Austria ABSTRACT Synthetic nagyagite was grown from a melt as part of a search for materials with high-tempera- ture superconductivity. Electron microprobe analyses of synthetic nagyagite and of nagyagite from the type locality Nagyág, Transylvania (now S˘ac˘arîmb, Romania) agree with data from literature. The crystal chemical formula [Pb(Pb,Sb)S2][(Au,Te)] was derived from crystal structure investi- gations. Nagyagite is monoclinic pseudotetragonal. The average crystal structure was determined from both synthetic and natural samples and was refined from the synthetic material to R = 0.045 for 657 single-crystal X-ray data: space group P21/m, a = 4.220(1) Å, b = 4.176(1) Å, c = 15.119(3) Å, β = 95.42(3)°, and Z = 2. Nagyagite features a pronounced layer structure: slices of a two slabs thick SnS-archetype with formula Pb(Pb,Sb)S2 parallel to (001) have a thickness of 9.15 Å. Te and Au form a planar pseudo-square net that is sandwiched between the SnS-archetype layers; it is [4Te] assumed that planar Au Te4 configurations are edge connected to chains and that Te atoms are in a zigzag arrangement.
    [Show full text]
  • Extraction of Gold by Dr
    Extraction of Gold By Dr. Ahmed Ameed 1 Characteristics and uses of gold 3 o Density : 19.3 g/cm , Tm:1064 C Shinny: for Jewelry Durable: does not tarnish or corrode easily, sometimes used in dentistry to make the crowns for teeth. Malleable and ductile: can be bent & flattened . For this reason it is used to make fine wires and thin, flat sheets Good conductor for heat & electricity: used in transistors, computer circuits & firefighting cloths. 2 Types of ores Gold occurs principally as a Native metal, usually alloyed with silver (as Electrum), or with mercury(as an Amalgam). Native gold can occur as sizeable nuggets, flakes, grains or microscopic particles embedded in other rocks. Ores in which gold occurs in chemical composition with other elements are comparatively rare. They include calaverite, sylvanite,nagyagite, petzite and kren nerite 3 Gold extraction Gold mining • Hard rock mining – used to extract gold encased in rock. Either open pit mining or underground mining. sand and gravel – )الفصل( Panning • containing gold is shaken (حصى) around with water in a pan. Gold is much denser than rock, so quickly settles to the bottom of the pan. 4 Gold extraction Gold mining • Sluicing – water is channelled to flow through a sluice-box with at the bottom which )تموجات( riffles create dead-zones in the water current which allows gold to drop out of suspension. • Sluicing and panning results in the direct recovery of .and flakes)خامات الذهب( small gold nuggets 5 Gold extraction Gold ore processing Gold cyanidation: • The most commonly used process for gold extraction.
    [Show full text]
  • Gold in Minerals and the Composition of Native Gold
    Gold in Minerals and the Composition of Native Gold Gold in Minerals and the Composition of Native Gold By Robert S. Jones and Michael Fleischer GEOLOGICAL SURVEY CIRCULAR 612 Washington 1969 United States Department of the Interior WAl.TfR J. HICKEL, Secretary Geological Survey William T. Pecora, Director Free on application to the U.S. Geological Survey, Washington, D.C. 20242 CONTENTS Page Abstract -----------------------------------------------~----------------- 1 Introduction -------------------------------------------------------------- 1 General geochenrlcal considerations ----------------------------------------- 1 Gold in minerals ------------------------------------------------------ _ 2 Composition and the fineness of gold ---------------------------- ___ 13 References cited --------·-------_____________________ ______________ ____ _ 15 TABLES Page 'fABLE 1. Major gold-bearing minerals ----------------------------------- __ 2 2. Analyses of precious metals in minerals made before 1955 _______ _ . _ 3 3. Analyses of gold in minerals made since 1954 --------------------- 10 4. Variation in fineness of gold with depth, Lily mine, Transvaal, South Jlfrica -------------------------------------------------------- 14 5. Fineness of mill bullion prior to 1882 at the Homestake nrlne, South Dakota -------------------------------------------------------- 15 Ill GOLD IN MINERALS AND THE COMPOSITION OF NATIVE GOLD By ROBERT S. JONES and MICHAEL FLEISCHER ABSTRACT much lower concentrations in the sulfiie phase, Gold occurs in nature mainly as the metal and as and occurs in much lesser amount~ in the various alloys. It forms complete series of solid solu­ silicate phase. Gold occurs in natur~ mainly tions with silver, copper, nickel, palladium, and as the metal and as various alloys, especially platinum. In association with the platinum metals, gold with silver, and as intermetallic co:'llpounds. occurs as free gold as well as in solid solution. Laboratory studies show that gold can form The native elements contain the most gold, followed by the sulfide minerals.
    [Show full text]
  • Mineralogical Setting of Precious Metals at the Assarel Porphyry
    minerals Article Mineralogical Setting of Precious Metals at the Assarel Porphyry Copper-Gold Deposit, Bulgaria, as Supporting Information for the Development of New Drill Core 3D XCT-XRF Scanning Technology Mihaela-Elena Cioacă 1,*, Marian Munteanu 1 , Edward P. Lynch 2, Nikolaos Arvanitidis 2, Mikael Bergqvist 3, Gelu Costin 4, Desislav Ivanov 5, Viorica Milu 1, Ronald Arvidsson 2, Adina Iorga-Pavel 1, Karin Högdahl 6 and Ventsislav Stoilov 5 1 Geological Institute of Romania, 012271 Bucharest, Romania; [email protected] (M.M.); [email protected] (V.M.); [email protected] (A.I.-P.) 2 Geological Survey of Sweden, Box 670, 75128 Uppsala, Sweden; [email protected] (E.P.L.); [email protected] (N.A.); [email protected] (R.A.) 3 Orexplore, 164 40 Kista, Sweden; [email protected] 4 Department of Earth, Environmental and Planetary Sciences, Keith-Wiess Geological Laboratories, Rice University, Houston, TX 77005, USA; [email protected] 5 Asarel Medet AD, 4500 Panagyurishte, Bulgaria; [email protected] (D.I.); [email protected] (V.S.) 6 Department of Earth Sciences, Uppsala University, Villavägen 16, 752 36 Uppsala, Sweden; [email protected] * Correspondence: [email protected]; Tel.: +40-0314033491 Received: 25 September 2020; Accepted: 21 October 2020; Published: 24 October 2020 Abstract: A petrographic investigation of ore samples from the Assarel porphyry copper deposit in the Srednogorie metallogenic zone (Bulgaria) constrains the setting and character of precious metals (Au, Ag, PGE) and related minerals within the deposit. This work supports renewed interest in understanding the deportment of precious metals and provides mineralogical knowledge during the testing and validation of novel drill core 3D X-ray computed tomography–X-ray fluorescence (XCT-XRF) scanning technology being developed as part of the X-MINE project.
    [Show full text]
  • New Mineral Names*
    American Mineralogist, Volume 94, pages 399–408, 2009 New Mineral Names* GLENN POIRIER,1 T. SCOTT ERCIT ,1 KIMBERLY T. TAIT ,2 PAULA C. PIILONEN ,1,† AND RALPH ROWE 1 1Mineral Sciences Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada 2Department of Natural History, Royal Ontario Museum, 100 Queen’s Park, Toronto, Ontario M5S 2C6, Canada ALLORIITE * epidote, magnetite, hematite, chalcopyrite, bornite, and cobaltite. R.K. Rastsvetaeva, A.G. Ivanova, N.V. Chukanov, and I.A. Chloro-potassichastingsite is semi-transparent dark green with a Verin (2007) Crystal structure of alloriite. Dokl. Akad. Nauk, greenish-gray streak and vitreous luster. The mineral is brittle with 415(2), 242–246 (in Russian); Dokl. Earth Sci., 415, 815–819 perfect {110} cleavage and stepped fracture. H = 5, mean VHN20 2 3 (in English). = 839 kg/mm , Dobs = 3.52(1), Dcalc = 3.53 g/cm . Biaxial (–) and strongly pleochroic with α = 1.728(2) (pale orange-yellow), β = Single-crystal X-ray structure refinement of alloriite, a member 1.749(5) (dark blue-green), γ = 1.751(2) (dark green-blue), 2V = of the cancrinite-sodalite group from the Sabatino volcanic complex, 15(5)°, positive sign of elongation, optic-axis dispersion r > v, Latium, Italy, gives a = 12.892(3), c = 21.340(5) Å, space group orientation Y = b, Z ^ c = 11°. Analysis by electron microprobe, wet chemistry (Fe2+:Fe3+) P31c, Raniso = 0.052 [3040 F > 6σ(F), MoKα], empirical formula and the Penfield method (H2O) gave: Na2O 1.07, K2O 3.04, Na18.4K6Ca4.8[(Si6.6Al5.4)4O96][SO4]4.8Cl0.8(CO3)x(H2O)y, crystal- CaO 10.72, MgO 2.91, MnO 0.40, FeO 23.48, Fe2O3 7.80, chemical formula {Si26Al22O96}{(Na3.54Ca0.46) [(H2O)3.54(OH)0.46]} + Al2O3 11.13, SiO2 35.62, TiO2 0.43, F 0.14, Cl 4.68, H2O 0.54, {(Na16.85K6Ca1.15)[(SO4)4(SO3,CO3)2]}{Ca4[(OH)1.6Cl0.4]} (Z = 1).
    [Show full text]
  • New Mineral Names
    American Mineralogist, Volume 80, pages 630-635, 1995 NEW MINERAL NAMES. JOHN L. JAMBOR Departmentof Earth Sciences,Universityof Waterloo,Waterloo,OntarioN2L 3Gl, Canada VLADIMIR A. KOVALENKER IGREM RAN, Russian Academy of Sciences, Moscow 10917, Staromonetnii 35, Russia ANDREW C. ROBERTS Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario KIA OE8, Canada Briziite* Co and increased Ni content in conireite, the name allud- F. Olmi, C. Sabelli (1994) Briziite, NaSb03, a new min- ing to the principal cations Co-Ni-Fe. eral from the Cetine mine (Tuscany, Italy): Description Discussion. An unapproved name for an incompletely and crystal structure. Eur. Jour. MineraL, 6, 667-672. described mineral. J.L.J. The mineral occurs as light pink to yellow, compact aggregates of platy to thin tabular crystals that encrust Grossite* weathered waste material and slag at the Cetine antimony D. Weber, A Bischoff(1994) Grossite (CaAl.O,)-a rare (stibnite) mine near Siena, Tuscany, Italy. Electron mi- phase in terrestrial rocks and meteorites. Eur. Jour. croprobe analysis gave Na20 15.98, Sb20s 83.28 wt%, Mineral., 6,591-594. corresponding to NaSb03. Platy crystals are hexagonal in D. Weber, A Bischoff (1994) The occurrence of grossite outline, up to 0.2 mm across, colorless, transparent, white (CaAl.O,) in chondrites. Geochim. Cosmochim. Acta, streak, pearly luster, perfect {001} cleavage, flexible, 58,3855-3817. VHNIS = 57 (41-70), nonfluorescent, polysynthetically twinned on (100), Dmeas= 4.8(2), Deale= 4.95 g/cm3 for Z Electron microprobe analysis gave CaO 21.4, A1203 = 6. Optically uniaxial negative, E= 1.631(1), w = 1.84 17.8, FeO 0.31, Ti02 0.15, Si02 0.11, MgO 0.06, sum (calculated).
    [Show full text]
  • Invisible Gold Paragenesis and Geochemistry in Pyrite from Orogenic and Sediment-Hosted Gold Deposits
    minerals Article Invisible Gold Paragenesis and Geochemistry in Pyrite from Orogenic and Sediment-Hosted Gold Deposits Ross R. Large 1,* and Valeriy V. Maslennikov 2 1 Australian Research Council Hub for Transforming the Mining Value Chain, Centre for Ore Deposits and Earth Science, University of Tasmania, Hobart 7005, Australia 2 Institute of Mineralogy, Russian Academy of Science, Miass 456300, Russia; [email protected] * Correspondence: [email protected] Received: 13 February 2020; Accepted: 27 March 2020; Published: 9 April 2020 Abstract: LA-ICPMS analysis of pyrite in ten gold deposits is used to determine the precise siting of invisible gold within pyrite, and thus the timing of gold introduction relative to the growth of pyrite and related orogenic events. A spectrum of invisible gold relationships in pyrite has been observed which suggests that, relative to orogenic pyrite growth, gold introduction in some deposits is early at the start of pyrite growth; in other deposits, it is late toward the end of pyrite growth and in a third case, it may be introduced at the intermediate stage of orogenic pyrite growth. In addition, we report a distinct chemical association of invisible gold in pyrite in the deposits studied. For example, in the Gold Quarry (Carlin type), Mt Olympus, Macraes and Konkera, the invisible gold is principally related to the arsenic content of pyrite. In contrast, in Kumtor and Geita Hill, the invisible gold is principally related to the tellurium content of pyrite. Other deposits (Golden Mile, Bendigo, Spanish Mountain, Witwatersrand Carbon Leader Reef (CLR)) exhibit both the Au-As and Au-Te association in pyrite.
    [Show full text]
  • The Crystal Structure of Synthetic Buckhornite, [Pb2bis3][Aute2]
    10 Z. Kristallogr. 215 (2000) 10- I 6 by Oldenbourg Wissenschaftsverlag, MUnchen The crystal structure of synthetic buckhornite, [Pb2BiS3][AuTe2] H. Effenberger*.l, F. 1. Culetto ", D. Tapa III and W. H. paarlIl I Universiiat Wien, Inslitut fUr Mineralogie und Kristallographie, Althan,traBe 14, A-lOgO Vienna. Austria II Kamtner Elektrizitiits AG. Amulfplatz 2, A-902 I Klagenfurt. Austria III Universitat Salzburg. lnstitut fUr Mineralogie. Hellbrunnerstrafk 34. A-S020 Salzburg. Auslria Received February 24. 1999: accepted May 26, 1999 Abstract. Synthetic buckhornite, [Pb2BiS,][AuTe2L was parameters from an X-ray powder pattern: a = grown from melts in connection with the search for high- 4.092(2) A, b = 12.245(4) A, c = 9.322(4) A; based on temperature superconductive materials. Chcmical analyses additional weak powder lines violating the extinction rnle were performed by electron-microprobe investigations. the authors assumed the extinction symbol P- - - for buck- The crystal structure was determined from 726 single-crys- hornite. Close relationships betwccn buckhornite and na- tal X-ray reflections of a twinned crystal. The refinement gyagite were derived from similarities of physical proper- gave R( F) = 0.10 I for 33 variable parameters. The space ties, X-ray data and chemical formula which suggested group is Pmmn, a = 4.IOR(3) A, b = 12.308(9) A, c = that these two minerals are part of a homologous series. 9.331 (6.) A, Z = 2. The atomic arrangement features a Some years earlier, two papers dealt with probable new pronounced laycr structure formed by two different sheets. minerals from the .lflove gold deposit, Czech Republic, (a) Planar Aul4TelTe4 configurations are edge-connected to and from Megradzorsk, Armenia (Pasava, Breiter, Malatek ribbons in [100]; they are linked by Te..
    [Show full text]
  • Geology and -Ore Deposits of the : Willow Creek Mining District, Alaska
    , Geology and -Ore Deposits of the : Willow Creek Mining District, Alaska GEOLOGICAL SURVEY BULLETIN 1004 Geology and Ore Deposits of the Willow Creek Mining District, Alaska By RICHARD G. RAY GEOLOGICAL SURVEY BULLETIN 1004 A study of the general and economic geology of a lode gold mining district in southern Alaska, with particular emphasis on the significance of vein, dike, and fau,lt patterns UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1954 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary B GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1.75 (paper cover) CONTENTS Page Abstract_ _ _ _______________________-____..__--_--------_---------- 1 Introduction ______.________________-__._______--._--_-'----------- 2 Previous work____________.__._._...i______-___-_-_--__-_---_ 2 Present work..____________________-_-----_-______--._----_---- 3 Scope of investigation and methods of field 'study... _ ---------- 4 Acknowledgments. ________-____--____-___-_--__--___--------_- 5 Geography__ _ _ __________________________________________________ 5 Location and accessibility-___________-___.___-_-_-_-_-----_---- 5 Topography, climate, and vegetation_____________________________ 5 General geology.______________________________-_.__--___-___-_---- 10 Metamorphic rocks._________________-__________--__--_------__ 10 Schist..._........_.....---_---.---__--------------------- 10 Igneous rocks_________________________________________________
    [Show full text]
  • Tellurium Minerals in New Mexico Virgil W
    Tellurium Minerals in New Mexico Virgil W. Lueth, New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM 87801, [email protected] Red River Anchor Elizabethtown Baldy 25 40 New Placers 40 e d n a r G Chloride o i Wilcox R Piños Altos Hillsboro Tierra Burro Blanca Mountains 25 Organ 10 Sylvanite 0 50 mi Eureka 0 80 km Rift Boundary Figure 1. Map of reported tellurium mineral occurrences in New Mexico. County boundaries in gray. Tellurium (Te) is an element of paradoxes. It is one of the is among the most abundant trace elements in the human most abundant heavy elements in the cosmos (Zemann body (Schroeder et al., 1967). This last paradox has not and Leutwein, 1978), with “heavy” defined as having yet been adequately resolved. an atomic number >40. But it is exceedingly rare in the All tellurium minerals are rare in nature and their earth’s crust, where its abundance is approximately 0.005 associated mineral deposits are usually small. The ppm (Jovic, 1999), and reliable values have never been tellurium minerals themselves are often microscopic, reported in seawater (Cohen, 1984). This is probably observed under high power in petrographic microscopes due to the fact that Te readily forms metal hydrides and or electron microprobes. Macroscopic examples are thus most of the element was lost to space during the Earth’s prized by collectors, especially when found in crystalline formation (Jovic, 1999). In terrestrial environments, it forms. This short paper compliments the lead article in this behaves as a chalcophile element and has a strong affinity volume (Tellurium Resources in New Mexico, by Virginia for the noble elements, transition metals, and sulfur McLemore) by expounding on the various tellurium (with whom it shares the same column in the periodic minerals reported in New Mexico.
    [Show full text]
  • The Geochemistry and Mineralogy of the Gies Gold-Silver Telluride Deposit, Central Montana
    Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1992 The geochemistry and mineralogy of the Gies gold- silver telluride deposit, central Montana Xiaomao Zhang Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Geochemistry Commons, and the Mineral Physics Commons Recommended Citation Zhang, Xiaomao, "The eg ochemistry and mineralogy of the Gies gold-silver telluride deposit, central Montana " (1992). Retrospective Theses and Dissertations. 10164. https://lib.dr.iastate.edu/rtd/10164 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps.
    [Show full text]
  • Mineral Assemblages from the Vein Salband at Sacarimb, Golden Quadrilateral, Romania: II
    • BULGARIAN ACADEMY OF SCIENCES GEOCHMISTRY, MINERALOGY AND PETROLOGY • 4 3 • SOFIA • 200 5 Au-Ag-Te-Se deposits IGCP Project 486, 2005 Field Workshop, Kiten, Bulgaria, 14-19 September 2005 Mineral assemblages from the vein salband at Sacarimb, Golden Quadrilateral, Romania: II. Tellurides Nigel J. Cook1, Cristiana L. Ciobanu2, Nicu Capraru3, Gheorghe Damian4, Petru Cristea3 12Natural History Museum Geology, University of Oslo, Norway; Department of Earth Sciences, University of Adelaide, North Terrace, Adelaide, South Australia; 3Deva Gold S.A., Certeju de Sus, Romania; 4Universitatea de Nord, Baia Mare, Romania Abstract: Bismuth tellurides (tetradymite, tellurobismuthite and buckhornite) are identified in salband mineralization at Sacarimb. Nagyagite is ubiquitously present, whereas other Au(Ag)-tellurides (sylvanite, petzite, hessite, stützite) and native tellurium are only locally abundant. Tellurides are mainly hosted within Sb-As-sulphosalts, textures indicate co-precipitation of sulphosalts and tellurides. A second population of the same Au(Ag)-tellurides, but now also including Bi-tellurides, relates to fluids introduced during vein reopening. The observations indicate that tellurides account for much of the 1-2g/t gold in the salband ore. Key words: Sacarimb, Romania, Epithermal Au-Te mineralization, Bi-tellurides the Sacarimb ore was nagyagite, a Au-telluride Introduction with a highly complex chemistry: [(Pb3(Pb,Sb, As) )S ][(Au,Te ) ]. Sacarimb (formerly Nagyag) is the type 3 6 2 3 Mineralization is formed in a low- locality for several telluride species, including sulphidation epithermal system that comprises nagyagite, krennerite, petzite and stützite. The some 230 veins centred upon a volcanic neck deposit is known for its diverse telluride (CN; Fig.
    [Show full text]