The Behavior of Molybdenum., Tungsten, and Titanium

Total Page:16

File Type:pdf, Size:1020Kb

The Behavior of Molybdenum., Tungsten, and Titanium The behavior of molybdenum, tungsten, and titanium in the porphyry copper environment Item Type text; Dissertation-Reproduction (electronic) Authors Kuck, Peter Hinckley Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 08/10/2021 00:24:06 Link to Item http://hdl.handle.net/10150/565421 THE BEHAVIOR OF MOLYBDENUM., TUNGSTEN, AND TITANIUM IN THE PORPHYRY COPPER ENVIRONMENT Peter' 'Hinckley Kuck A Dissertation Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES. In Partial.Fulfillment of the Requirements. ' ■ For the Degree of DOCTOR OF PHILOSOPHY In the Graduate College ■ THE UNIVERSITY OF ARIZONA 1 9 7 8 THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE I hereby recommend that this dissertation prepared under my Peter Hinckley Kuck direction by ___________ , , The Behavior of Molybdenum, Tungsten, and Titanium entitled ________________________________________________________ in the Porphyry Copper Environment be accepted as fulfilling the dissertation requirement for the Doctor of Philosophy degree of _______________________________________________________ Dissertation Director Date As members of the Final Examination Committee, we certify that we have read this dissertation and agree that it may be presented for final defense. \ R A j r i A hi / 7IT 2 / 1 r 7 - Final approval and acceptance of this dissertation is contingent on the candidate's adequate performance and defense thereof at the final oral examination. STATEMENT BY AUTHOR This dissertation has been submitted in partial fulfillment of requirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of. the .Library. Brief quotations from this dissertation are allow­ able without special permission, provided that accurate ■ acknowledgment of source is made; Requests- for permission for extended quotation from or reproduction of this manu­ script in whole or in part may be granted by the head of the major department or the■Dean of the Graduate College when in his judgment the proposed: use of the material is in the interests of scholarship. In all Other instances, however,. permission must be obtained frOm the author. ACKNOWLEDGMENTS I am deeply indebted to Dr. Paul E. Damon for his supervision and support of this dissertation. Drs. John W. Anthony, John M. Guilbert, and John S. Sumner provided many helpful suggestions, comments, and constructive criticisms. I would.like to especially thank Dr. George W. Nelson fo r _his encouragement 'an d .invaluable.assistance . ■ • in many aspects of the project. Dr. Nelson, Dr. .Morton E . -. Hacks, and other members of the Nuclear Engineering;Depart- . ment irradiated more than one hundred mineral samples in the TRIGA reactor and allowed me to.use their gamma-ray . spectrometry system. It is a pleasure to express my appreciation to Robert B. Scarborough who assisted me in both the laboratory and the field. Dr. Muhammad Shafiqullah, Daniel J. Lynch, and the other members of the Laboratory of Isotope Geo- .chemistry kindly provided potassium^argon data on several mineralized intrusives. Dr. Denis L. Norton and Jerry E. Knight gave useful suggestions and assistance in con­ structing activity diagrams. Dr* Donald .Ev Livingston . provided constructive advice on x-ray fluorescence. Thomas M. Teska and Horton E. Newsom helped with the electron microprobe analyses. iv Michael H. Rauschkolb and his associates.-at AMAX Arizona, Inc. collaborated with me on the .examination of the copper-molybdenum-tungsten mineralization in the Twin Buttes ore body. Calvert D. lies of the Duval Sierrita Corporation provided samples and data on the mineralization at the Esperanza and Sierrita open pit mines. I would also like to thank the following individuals for their help: Janis K. Blainer, the late Thomas Breen, Dr. Donald M. Burt, J. L. Christman, .Richard. Graeme, Dr. Frederick T. , Graybeal , James Guthrie, Dr ^ Herbert E.- Hawke.s, Margo -Jennison, Peter L. Kresan, Norman E . Lehman, Richard Moore, Dr. Henn Oona, Dr. Eberhardt A. Schmidt, and Dr. Anne M. S'igleo. I owe a special debt of thanks to Dr. David L. Perry fdr: introducing me to the problems of molyb­ denite deposition. Mr. Henry G. Worsley, the owner of the Mary G mine, provided information on the mining history of the Las G.uij as and San Luis Mountains. The following mining companies - gave mb permission to. collect samples from their properties or provided samples for this study: ANAMAX . Mining Co., Cyprus Bagdad Copper Corp., Duval Sierrita Corp., Oracle Ridge Mining Partners, the Ray Mines Division of the Kehnecott Copper Corp., and the Phelps Dodge Corp. - .The editorial suggestions of Kathleen Roe Trevena were of great value and helped to make parts of the dis­ sertation smoother and clearer. Finally, I would like to ■thank Professor ter ah L„ Smiley, for his. valuable counsel and timely advice. Financial assistance was furnished in part by the National Science Foundation through a.summer traineeship and under Grant EAR?6-02590 to Paul E. Damon. TABLE OF CONTENTS Page LIST OF TABLES ................ ix ■ LIST OF ILLUSTRATIONS V . ... .... xii ABSTRACT ' . « . .... ......... .. xvi ■THE; MOLYBDENUM-TUNGSTEN' PROBLEM ;. 1 1.1 Differences in Behavior between Molyb­ denum and Tungsten • in Porphyry Copper Deposits . .... , . .1 1.2 Economic Implications of the Molybdenum- .. Tungsten- Problem . :. .. .. 5 1.3 Possible Explanations of the Difference in Behavior between Molybdenum and. Tungsten . 8 GEOCHEMISTRY OF MOLYBDENUM, TUNGSTEN, AND. TITANIUM . ... ... .............. 15 2.1. Differences in Electronic Structure . 15. 2.2 Effect of Differences in Nuclear Struc­ ture on the Abundances of the Three .. ■ Elements . .. ■.■. ..- . *■ . ....... 2 4 2 . 3 Molybdenum and Tungsten Minerals' .'., . .. 30 2.4 Laboratory Synthesis of Molybdates . and Tungstates . > . .40 MOLYBDENUM, TUNGSTEN, AND TITANIUM MINERALIZATION IN SOUTHERN ARIZONA . .. .... 49 3.1 Area of Investigation . ........ 49 3.2 Age Relationships . ...... 52 3.3 Types of Deposits . ..... 53 . 3.4 The Spatial Distribution of Molybdenite and Scheelite in Porphyry Copper Deposits and Related Skarns . ■. , . .. , . , . 57 3.5 . Rutile and Other Titanium-Bearing Minerals Associated with Chalcopyrite- Molybdenite Ores ... .. 68 vii . TABLE OF CONTENTS (Continued) Page CHEMICAL ANALYSES OF ORE MINERALS „ . 80 4.1 Preparation of Standards and .Samples . 80 4.2 Emission Spectrographic Analyses ......... 85 4.3 X-ray Fluorescence Analyses ....... 86 4.4 Neutron Activation Analyses . 87 DISCUSSION OF CHEMICAL ANALYSES . ...... 95 5.1 Minot Elements in Molybdenite . .' . 95 5.2 Rlienium,' Selenium, and Other Trace ' Elements- ' in Molybdeni te " . I . 98 : 5.3 Minor Elements in Wolframite . .114. ' ; 5.4 Scandium, Niobium, and Other Trace Elements in Wolframite . .. .- . 115 l 5.5 Minor and Trace Elements in Scheelite . 12 0 5.6 Tungsten> Copper, and Other Trace Elements in Rutile . ...... ' 127 TRANSPORT AND DEPOSITION OF MOLYBDENUM AND Tungsten , , . .. .. ..... , . 130 ■ 6.1 Transport Problems . a . .. »•. 130 6.2 The Solubility of Different Molybdenum and Tungsten Minerals in Hydrothermal Bf ine s ■' o . a . ;. e .- . * ■ e ‘ a . o . 0.0 e « « . « 132 . 6.3 Depositional Temperatures . 133 ; - 6.4 . Stable. Mineral Assemblages . ... .. 143 6.5 Activity-Activity Diagrams for the Ca—Fe—Cu—Mo—W—S—0—H System . 145 CONCLUSIONS \ . .. 163 APPENDIX A: COMPILATION OF 40K/4°Ar AGE DETERMINA­ TIONS OF LARAMIDE INTRUSIVES IN . SOUTHEASTERN ARIZONA THAT ARE ASSOCI­ ATED WITH COPPER-MOLYBDENUM OR COPPER- ' ■ ' TUNGSTEN MINERALIZATION: : . 1 . .. 167 • APPENDIX B: COMPILATION OF 40K/4°Ar AGE DETERMINAr- .. TIONS OF OLIGOCENE AND MIOCENE IN­ TRUSIVES IN SOUTHEASTERN ARIZONA . 176 APPENDIX C;' SEMIQUANTITATIVE EMISSION SPECTRO­ GRAPHIC ANALYSES OF MOLYBDENITE . 181 viii TABLE OF CONTENTS (Continued) Page APPENDIX D : EMISSION.SPECTROGRAPHIC ANALYSES OF . FERBERITE, WOLFRAMITE, AND HUEBNER- ITE . ' > .. ... 213 APPENDIX E : ' EMISSION SPECTROGRAPHIC ANALYSES OF SCHEELITE AND POWELLITE . 233 APPENDIX F : EMISSION SPECTROGRAPHIC ANALYSES OF : RUTILE, MAGNETITE, AND HEMATITE . ... 242 APPENDIX G :. CONVENTIONAL X-RAY FLUORESCENCE ANALYSES OF FERBERITE, . WOLFRAMITE, "■ AND HUEBNERITE ■ <, . „ . ... 2 51 APPENDIX.H : THERMODYNAMIC. PROPERTIES OF SELECTED MOLYBDENUM AND TUNGSTEN COMPOUNDS, , INCLUDING THE : DATA FOR THE MOLYBDATE. AND TUNG STATE ANIONS . ... 256 REFERENCES. CITED . ... o; ;. ... .. .. ... ... 26.0 LIST OF TABLES Table Page 1. Atomic properties of titanium, molybdenum, an cl ■ tungsten ». e & * « ». « # » -» o » » » » a » « 2 2. Molybdenum-tungsten isomorphism in por­ phyry copper deposits „ « i ° .• « - . .. • 3 3. Values of the Gibbs free-energy of formation for selected molybdenum and tungsten com^ pounds ».o. ................ 9 4. Electronic configurations of. the neutral Cl L- OXi-L £5 e O • e a a a a a -a a a a a a . ■ a a a a a a 1 2 5. Deviations In atdmic orbital filling . 18 . 6. Various covalent, ionic,.and.metallic radii for titanium, molybdenum, and: tungsten. ^ . 22 7» The partial ionic character of different - • bonds formed by titanium, molybdenum, and tungsten a a a a a a a , a O' a a . a a a . a a - a -a ■ a a 2 3 8 a The concentration
Recommended publications
  • Metamorphism of Sedimentary Manganese Deposits
    Acta Mineralogica-Petrographica, Szeged, XX/2, 325—336, 1972. METAMORPHISM OF SEDIMENTARY MANGANESE DEPOSITS SUPRIYA ROY ABSTRACT: Metamorphosed sedimentary deposits of manganese occur extensively in India, Brazil, U. S. A., Australia, New Zealand, U. S. S. R., West and South West Africa, Madagascar and Japan. Different mineral-assemblages have been recorded from these deposits which may be classi- fied into oxide, carbonate, silicate and silicate-carbonate formations. The oxide formations are represented by lower oxides (braunite, bixbyite, hollandite, hausmannite, jacobsite, vredenburgite •etc.), the carbonate formations by rhodochrosite, kutnahorite, manganoan calcite etc., the silicate formations by spessartite, rhodonite, manganiferous amphiboles and pyroxenes, manganophyllite, piedmontite etc. and the silicate-carbonate formations by rhodochrosite, rhodonite, tephroite, spessartite etc. Pétrographie and phase-equilibia data indicate that the original bulk composition in the sediments, the reactions during metamorphism (contact and regional and the variations and effect of 02, C02, etc. with rise of temperature, control the mineralogy of the metamorphosed manga- nese formations. The general trend of formation and transformation of mineral phases in oxide, carbonate, silicate and silicate-carbonate formations during regional and contact metamorphism has, thus, been established. Sedimentary manganese formations, later modified by regional or contact metamorphism, have been reported from different parts of the world. The most important among such deposits occur in India, Brazil, U.S.A., U.S.S.R., Ghana, South and South West Africa, Madagascar, Australia, New Zealand, Great Britain, Japan etc. An attempt will be made to summarize the pertinent data on these metamorphosed sedimentary formations so as to establish the role of original bulk composition of the sediments, transformation and reaction of phases at ele- vated temperature and varying oxygen and carbon dioxide fugacities in determin- ing the mineral assemblages in these deposits.
    [Show full text]
  • Washington State Minerals Checklist
    Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite
    [Show full text]
  • Mineral Processing
    Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19
    [Show full text]
  • A Review on Historical Earth Pigments Used in India's Wall Paintings
    heritage Review A Review on Historical Earth Pigments Used in India’s Wall Paintings Anjali Sharma 1 and Manager Rajdeo Singh 2,* 1 Department of Conservation, National Museum Institute, Janpath, New Delhi 110011, India; [email protected] 2 National Research Laboratory for the Conservation of Cultural Property, Aliganj, Lucknow 226024, India * Correspondence: [email protected] Abstract: Iron-containing earth minerals of various hues were the earliest pigments of the prehistoric artists who dwelled in caves. Being a prominent part of human expression through art, nature- derived pigments have been used in continuum through ages until now. Studies reveal that the primitive artist stored or used his pigments as color cakes made out of skin or reeds. Although records to help understand the technical details of Indian painting in the early periodare scanty, there is a certain amount of material from which some idea may be gained regarding the methods used by the artists to obtain their results. Considering Indian wall paintings, the most widely used earth pigments include red, yellow, and green ochres, making it fairly easy for the modern era scientific conservators and researchers to study them. The present knowledge on material sources given in the literature is limited and deficient as of now, hence the present work attempts to elucidate the range of earth pigments encountered in Indian wall paintings and the scientific studies and characterization by analytical techniques that form the knowledge background on the topic. Studies leadingto well-founded knowledge on pigments can contribute towards the safeguarding of Indian cultural heritage as well as spread awareness among conservators, restorers, and scholars.
    [Show full text]
  • Manganoquadratite, Agmnass3, a New Manganese Bearing
    American Mineralogist, Volume 97, pages 1199–1205, 2012 Manganoquadratite, AgMnAsS3, a new manganese-bearing sulfosalt from the Uchucchacua polymetallic deposit, Lima Department, Peru: Description and crystal structure PAOLA BONAZZI,1,* FRANK N. KEUTSCH,2 AND LUCA BINDI1,3 1Dipartimento di Scienze della Terra, Università degli Studi di Firenze, via La Pira 4, I-50121 Firenze, Italy 2Department of Chemistry, University of Wisconsin-Madison, 1101 University Avenue, Madison, Wisconsin 53706, U.S.A. 3Museo di Storia Naturale, sezione di Mineralogia e Litologia, Università degli Studi di Firenze, via La Pira 4, I-50121 Firenze, Italy ABSTRACT Manganoquadratite, ideally AgMnAsS3, is a new mineral from the Uchucchacua polymetallic deposit, Oyon district, Catajambo, Lima Department, Peru. It occurs as dark gray, anhedral to subhe- dral grains up 0.5 mm across, closely associated with alabandite, Mn-rich calcite, Mn-rich sphalerite, proustite, pyrite, pyrrhotite, tennantite, argentotennantite, stannite, and other unnamed minerals of the system Pb-Ag-Sb-Mn-As-S. Manganoquadratite is opaque with a metallic luster and possesses 2 a reddish-brown streak. It is brittle, the Vickers microhardness (VHN10) is 81 kg/mm (range 75–96) (corresponding Mohs hardness of 2–2½). The calculated density is 4.680 g/cm3 (on the basis of the empirical formula). In plane-polarized reflected light, manganoquadratite is moderately bireflectant and very weakly pleochroic from dark gray to a blue gray. Internal reflections are absent. Between crossed polars, the mineral is anisotropic, without characteristic rotation tints. Reflectance percentages (Rmin and Rmax) for the four standard COM wavelengths are 29.5, 31.8 (471.1 nm), 28.1, 30.5 (548.3 nm), 27.3, 29.3 (586.6 nm), and 26.0, 28.2 (652.3 nm), respectively.
    [Show full text]
  • Characterization and Beneficiation of Iranian Low-Grade Manganese Ore
    Physicochemical Problems Physicochem. Probl. Miner. Process. 49(2), 2013, 725−741 of Mineral Processing ISSN 1643-1049 (print) www.minproc.pwr.wroc.pl/journal/ ISSN 2084-4735 (online) Received July 24, 2012; reviewed; accepted April 26, 2013 CHARACTERIZATION AND BENEFICIATION OF IRANIAN LOW-GRADE MANGANESE ORE Akbar MEHDILO, Mehdi IRANNAJAD, Mohammad Reza HOJJATI-RAD * Department of Mining and Metallurgical Eng., Amirkabir University of Technology, Tehran, Iran *[email protected] Abstract: The mineralogical studies indicated that the Charagah ore deposit contains approximately 17% pyrolusite, 78% calcite and 3–4% quartz. Pyrolusite as a main valuable mineral is found in the forms of coarse and fine pyrolusites. The coarse grains pyrolusite with simple texture is liberated at 180 micrometers. Another kind of pyrolusite with particle size finer than 10 m is disseminated inside gangue phases. This kind of pyrolusite has important effect in beneficiation processes and can affect the manganese grade of the concentrate and its recovery negatively. By jigging machine a pre-concentrate with 20% MnO and a final tailing with about 13% manganese loss are obtained. Using tabling technique or wet high intensity magnetic separation (WHIMS) and also their combination with jigging machine, production of a final pyrolusite concentrate with suitable grade but average recovery is possible. By jigging-tabling a concentrate with – 500+45 m size fraction, 44.3% MnO and 61.3% recovery is obtained while jigging-WHIMS produces a concentrate containing 52.6% MnO with a recovery up to 56.6% and d80 = 180 m. Keywords: pyrolusite, manganese ore, ore characterization, gravity separation, magnetic separation Introduction Manganese is used mainly in steel production, directly in pig iron manufacture and indirectly through upgrading ore to ferroalloys.
    [Show full text]
  • A Specific Gravity Index for Minerats
    A SPECIFICGRAVITY INDEX FOR MINERATS c. A. MURSKyI ern R. M. THOMPSON, Un'fuersityof Bri.ti,sh Col,umb,in,Voncouver, Canad,a This work was undertaken in order to provide a practical, and as far as possible,a complete list of specific gravities of minerals. An accurate speciflc cravity determination can usually be made quickly and this information when combined with other physical properties commonly leads to rapid mineral identification. Early complete but now outdated specific gravity lists are those of Miers given in his mineralogy textbook (1902),and Spencer(M,i,n. Mag.,2!, pp. 382-865,I}ZZ). A more recent list by Hurlbut (Dana's Manuatr of M,i,neral,ogy,LgE2) is incomplete and others are limited to rock forming minerals,Trdger (Tabel,l,enntr-optischen Best'i,mmungd,er geste,i,nsb.ildend,en M,ineral,e, 1952) and Morey (Encycto- ped,iaof Cherni,cal,Technol,ogy, Vol. 12, 19b4). In his mineral identification tables, smith (rd,entifi,cati,onand. qual,itatioe cherai,cal,anal,ys'i,s of mineral,s,second edition, New york, 19bB) groups minerals on the basis of specificgravity but in each of the twelve groups the minerals are listed in order of decreasinghardness. The present work should not be regarded as an index of all known minerals as the specificgravities of many minerals are unknown or known only approximately and are omitted from the current list. The list, in order of increasing specific gravity, includes all minerals without regard to other physical properties or to chemical composition. The designation I or II after the name indicates that the mineral falls in the classesof minerals describedin Dana Systemof M'ineralogyEdition 7, volume I (Native elements, sulphides, oxides, etc.) or II (Halides, carbonates, etc.) (L944 and 1951).
    [Show full text]
  • Rhodochrosite Mn CO3 C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Hexagonal
    2+ Rhodochrosite Mn CO3 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 32/m. Crystals are rhombohedra {1011} or scalenohedra {2131}, to 12 cm, modified by {0001}, {1010}, {1120}, with several other forms, may be rounded or saddle-shaped. Commonly in bladed aggregates, columnar, stalactitic, botryoidal, compact granular, massive. Twinning: On {1012}, contact and lamellar, then flattened. Physical Properties: Cleavage: {1011}, perfect; {0112}, a parting. Fracture: Uneven to conchoidal. Tenacity: Brittle. Hardness = 3.5–4 D(meas.) = 3.70 D(calc.) = 3.70 Optical Properties: Transparent to translucent. Color: Pink, rose-red, cherry-red, yellow, yellowish gray, cinnamon-brown, may be banded; pale rose to colorless in transmitted light. Streak: White. Luster: Vitreous, pearly in aggregates. Optical Class: Uniaxial (–). Pleochroism: Faint. Absorption: O > E. ω = 1.810 = 1.597 Cell Data: Space Group: R3c (synthetic). a = 4.777 c = 15.67 Z = 6 X-ray Powder Pattern: Synthetic. 2.84 (100), 3.66 (35), 1.763 (35), 1.770 (30), 2.172 (25), 2.000 (25), 2.39 (20) Chemistry: (1) (2) CO2 38.26 38.29 FeO 0.77 MnO 60.87 61.71 MgO trace CaO 0.51 Total 100.41 100.00 (1) Ljubija district, Bosnia-Herzegovina. (2) MnCO3. Polymorphism & Series: Forms two series, with calcite and with siderite. Mineral Group: Calcite group. Occurrence: A primary mineral in low- to moderate-temperature hydrothermal veins; in metamorphic deposits; common in carbonatites; authigenic and secondary in sediments; uncommon in granite pegmatites. Association: Calcite, siderite, dolomite, fluorite, barite, quartz, pyrite, tetrahedrite, sphalerite, h¨ubnerite(hydrothermal); rhodonite, garnet, alabandite, hausmannite (metamorphic).
    [Show full text]
  • Petrologic and Crystal-Chemical Implications of Cation Order
    American Mineralogist, Volume 72, pages 319-328, 1987 Petrologicand crystal-chemicalimplications of cation order-disorderin kutnahoriteICaMn(COr)rl* D. R. Pucon, E. J. EssBNn Department of Geological Sciences,The University of Michigan, Ann Arbor, Michigan 48109, U.S.A. A. M. G.qlNns Division of Earth Sciences,National ScienceFoundation, Washington, D.C.20550, U.S.A. Ansrucr The crystal structuresof kutnahorite from Bald Knob (BK), North Carolina, and Sterling Hill (SH), New Jersey,have been refined. The BK kutnahorite (CaorMn'oMg'Feo)is dis- ordered in Ca-Mn distribution, but the SH kutnahorite is substantially ordered: (Ca".roMno1u)(Cao rrMno rrXCOrL. Long-rangecation order in kutnahorite is not detectable using conventional powder X-ray diffraction techniques,but it may be measuredby single- crystal techniques.The largeionic radius of Mn relative to Mg in dolomite leadsto coupled distortion of the Ca and Mn octahedrathat may result in a low ordering potential. Thus, the BK kutnahorite lacks significant cation order despite slow cooling from amphibolite- facies regional metamorphic conditions. Long-range cation order in SH kutnahorite is compatible with a low-temperature solvus between calcite and kutnahorite as well as between kutnahorite and rhodochrosite. Two-phase intergrowths of manganoan calcite (CarrMn,rMg) and calcian kutnahorite (Ca.rMnrrMgr) from SH are interpreted as due to primary coprecipitation of calcite and ordered kutnahorite from solution in the two-phase region at temperaturesbelow the solvus crest. Data on metamorphic Ca-Mn carbonates indicate complete solid solution between calcite and rhodochrosite at 600qCwith solvi betweenkutnahorite-calcite and kutnahorite-rhodochrositeforming at lower temperatures. INrnooucrrou and calcite. The ternary system CaCOr-MnCOr-MgCO.
    [Show full text]
  • Minerals of Arizona Report
    MINERALS OF ARIZONA by Frederic W. Galbraith and Daniel J. Brennan THE ARIZONA BUREAU OF MINES Price One Dollar Free to Residents of Arizona Bulletin 181 1970 THE UNIVERSITY OF ARIZONA TUCSON TABLE OF CONT'ENTS EIements .___ 1 FOREWORD Sulfides ._______________________ 9 As a service about mineral matters in Arizona, the Arizona Bureau Sulfosalts ._. .___ __ 22 of Mines, University of Arizona, is pleased to reprint the long-standing booklet on MINERALS OF ARIZONA. This basic journal was issued originally in 1941, under the authorship of Dr. Frederic W. Galbraith, as Simple Oxides .. 26 a bulletin of the Arizona Bureau of Mines. It has moved through several editions and, in some later printings, it was authored jointly by Dr. Gal­ Oxides Containing Uranium, Thorium, Zirconium .. .... 34 braith and Dr. Daniel J. Brennan. It now is being released in its Fourth Edition as Bulletin 181, Arizona Bureau of Mines. Hydroxides .. .. 35 The comprehensive coverage of mineral information contained in the bulletin should serve to give notable and continuing benefits to laymen as well as to professional scientists of Arizona. Multiple Oxides 37 J. D. Forrester, Director Arizona Bureau of Mines Multiple Oxides Containing Columbium, February 2, 1970 Tantaum, Titanium .. .. .. 40 Halides .. .. __ ____ _________ __ __ 41 Carbonates, Nitrates, Borates .. .... .. 45 Sulfates, Chromates, Tellurites .. .. .. __ .._.. __ 57 Phosphates, Arsenates, Vanadates, Antimonates .._ 68 First Edition (Bulletin 149) July 1, 1941 Vanadium Oxysalts ...... .......... 76 Second Edition, Revised (Bulletin 153) April, 1947 Third Edition, Revised 1959; Second Printing 1966 Fourth Edition (Bulletin 181) February, 1970 Tungstates, Molybdates.. _. .. .. .. 79 Silicates ...
    [Show full text]
  • The Metal Resources of New Mexico and Their Economic Features Through 1954
    BULLETIN 39 The Metal Resources of New Mexico and Their Economic Features Through 1954 A revision of Bulletin 7, by Lasky and Wootton, with detailed information for the years 1932-1954 BY EUGENE CARTER ANDERSON 1957 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Alvin J. Thompson, Director THE REGENTS MEMBERS EX OFFICIO THE HONORABLE EDWIN L. MECHEM………...Governor of New Mexico MRS. GEORGIA L. LUSK ......................Superintendent of Public Instruction APPOINTED MEMBERS ROBERT W. BOTTS ....................................................................Albuquerque HOLM O. BURSUM, JR. .....................................................................Socorro THOMAS M. CRAMER .................................................................... Carlsbad JOHN N. MATHEWS, JR. ...................................................................Socorro RICHARD A. MATUSZESKI ......................................................Albuquerque Contents Page INTRODUCTION .......................................................................................................... 1 Purpose and Scope of Bulletin ..................................................................................... 1 Other Reports Dealing With the Geology and Mineral Resources of New Mexico ......................................................................................................
    [Show full text]
  • Check Lists of Minerals for Mining Districts and Other Localities Near Albuquerque Stuart A
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/12 Check lists of minerals for mining districts and other localities near Albuquerque Stuart A. Northrop, 1961, pp. 172-174 in: Albuquerque Country, Northrop, S. A.; [ed.], New Mexico Geological Society 12th Annual Fall Field Conference Guidebook, 199 p. This is one of many related papers that were included in the 1961 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States.
    [Show full text]