Sulfosalt Systematics: a Review
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The Crystal Structure of Gillulyite, TI2(As,Sb)Ssm from the Mercur Gold Deposit, Tooele County, Utah, U.S.A
American Mineralogist, Volume 80, pages 394-399, 1995 The crystal structure of gillulyite, TI2(As,Sb)sSm from the Mercur gold deposit, Tooele County, Utah, U.S.A. FRANKLIN F. FOIT, JR. Department of Geology, Washington State University, Pullman, Washington 99164, U.S.A. PAUL D. ROBINSON Department of Geology, Southern Illinois University, Carbondale, Illinois 62901, U.S.A. JAMES R. WILSON Department of Geology, Weber State University, Ogden, Utah 84408-2507, U.S.A. ABSTRACT Gillulyite, TI2(AsH ,SbH )8S13,is monoclinic with space group P2/n and a = 9.584(3), b = 5.679(2), c = 21.501(6) A, ~ = 100.07(2)°, V = 1152.2(7) A3, and Z = 2, The average structure was determined using direct methods and refined to a final residual of 0.046 using 930 reflections. The structure consists of TI-As-S- and As-S-bearing sheets, each present statistically 50% of the time. Four sheets, linked together by Tl-S, As-S, and S-S bonds, are stacked parallel to (00 I), yielding the 21-A c-axis repeat of the average unit cell. The Tll atom within the TI-As-S sheet is coordinated by six S nearest neighbors, which form a distorted trigonal prism. The partially occupied Tl2 position between the sheets is split symmetrically about the twofold axis with a separation of 1.28 A and equal but partial occupancies of25%. The disordering of the Tl2 position and extreme distortion of its coordination polyhedron is probably the result of the Tl+ 6s2lone pair effect. The mean bond distances for the AsS3pyramids range from 2.263 to 2.319 A. -
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 -
Using 2D Gis to Assist 3D Modelling of the Zarshuran Gold Deposit, Iran
Asadi, Hooshang USING 2D GIS TO ASSIST 3D MODELLING OF THE ZARSHURAN GOLD DEPOSIT, IRAN * Hooshang ASADI HARONI, Edmund SIDES, Kiiza NGONZI International Institute for Aerospace Survey and Earth Sciences (ITC), The Netherlands * Ministry of Higher Education, Tehran, Iran harouni @itc.nl [email protected] Technical Commission Session Themes TC VII-8 KEY WORDS: Spatial data, Integration, Geology, Geophysics, GIS, Data mining, Information extraction ABSTRACT The Zarshuran gold deposit in NW Iran is an area of historic mining for gold and arsenic with considerable potential for discovery of economic gold mineralisation. Geological, geochemical and geophysical data, collected by the Ministry of Mines and Metals were compiled and analysed in a 2-dimensional (2D) GIS. This resulted in the definition of major structural features, and lithological units, that control the gold mineralisation. Spatial modelling and interpretation of the geochemical and geophysical data showed that the mineralization is mainly controlled by chemically-reactive Precambrian carbonates and black shales, extending in a NW-SE direction, and also by NE-SW high angle faults and their intersections with NW-SE structures. The results obtained, from the 2D GIS analysis, were used in the initial phase of the construction and validation of the 3-dimensional (3D) models used for resource estimation. Comparison of the statistical analyses of geochemical data in soils and in drillcore indicated enhanced concentrations of gold in soils at surface, due to residual enrichment. An enrichment relationship was established based on interpretation of the cumulative frequency plots for gold in soil and drillcore samples. Based on this relationship the gold anomalies interpreted from the soil geochemical data were used to infer a resource potential, to a depth of 200m below surface, of 10Mt at an average grade of 0.2 g/t gold. -
NEW MINERAL NAMES Micnabr, Frprschnn Mohrite
THE AMERICAN MINERALOGIST, VOL. 50, MAY JUNE, 1965 NEW MINERAL NAMES MIcnaBr, FrprscHnn Mohrite canro L. Gana.vrr,r,r, Mohrite: un nuovo minerale della zona borifera toscana. Atti Aecad. Nozl. Lineei.,Rend.., Classe sci. f,s. mat. e nat.,36,52+533 (1964). Pale green incrustations were collected by Professor A. Pelloux in 7927 fuom the borif- erous soffioni of rravale, Val di Cecina, Tuscany, rtaly. They consisted of irregular Iamina and of minute quasieuhedral crystals; these were selected under the binoculars and analyzed separately, giving respectively: SO3 41.05,42.69; FeO 17.49,9.86; MnO 0 11, 0.34; MgO 0.56, 5.08; (NHr)zO 13.13, 13.40;IlrO 27.10,28.69; insol. in HrO 0.16, 0.15; sum 9960, 100.217a. These correspond to (NHn)r(Feo ean4gss5Mno r)(SOr)r.6HrO and (NHr)r (FeonMgonzMnou)(SOr)2.6H:O. The name mohiite is given to the end-member (NHr)zFe(SOn)z'6H2O;a complete solid solution seriesprobably existswith boussingaultite. X-ray study shows the mineral to be monoclinic, space grotp p21f c; the unit cell con- stants for the two analyzed samples are, respectively o 6.237,6.234; b 12.613, 12.618; c 9.292,9.290A.,B 106053'106"54',Gcalc. 1.870,1.805; meas. 1.862,1.800. X-ray powder data aregivenl the strongest lines for the first sampleare 3.801 (100) (031), 4.200 (65) (T02), 2 (28)(Is3), 460 3.1s3 (2s)(040), s.025 (20)811), s.40 (1s)(110). -
University of Nevada, Reno Issues Affecting Heap Biooxidation of Low
University of Nevada, Reno Issues affecting heap biooxidation of low-grade refractory gold ore: Formation of secondary sulfates, ore lithology, alteration and sulfide mineralogy at Gold Quarry, Carlin, Nevada A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology by Wes K. Sherlock Dr. Tommy B Thompson/Thesis Advisor August, 2010 i Abstract The Gold Quarry mine is located in the Maggie Creek District in the northern section of the southern half of the Carlin Trend, 11 km north of the town of Carlin, Eureka County, Nevada. The primary metal of interest is gold. The majority of the ore is sulfidic-refractory consisting primarily of homogenously distributed extremely small gold particles, generally ranging in size from colloidal to approximately 50Å, hosted primarily as a solid solution within the structural lattice of arsenian pyrite rims which surround some pre-ore pyrite crystals (Arehart et al., 1993). Arsenian pyrite is also commonly found as discrete fine-grain disseminated crystals or in local fine-grain masses or clouds. High-grade sulfidic refractory ore is processed via roasting methods where as, the low-grade ore cannot be economically processed through the roaster and is instead oxidized by a cost mediated biological heap method on three nominal 800,000 ton pads. The oxidized low-grade ore is then utilized as supplementary mill feed. Recycling of the biooxidation fluid over time has resulted in a solution highly saturated in sulfate and various metals of which iron and aluminum are the largest contributors to sulfate formation. Consequently, local areas within the heap pad that experience dehydration may experience substantial secondary hydrous sulfate mineral accumulations. -
STRONG and WEAK INTERLAYER INTERACTIONS of TWO-DIMENSIONAL MATERIALS and THEIR ASSEMBLIES Tyler William Farnsworth a Dissertati
STRONG AND WEAK INTERLAYER INTERACTIONS OF TWO-DIMENSIONAL MATERIALS AND THEIR ASSEMBLIES Tyler William Farnsworth A dissertation submitted to the faculty at the University of North Carolina at Chapel Hill in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of Chemistry. Chapel Hill 2018 Approved by: Scott C. Warren James F. Cahoon Wei You Joanna M. Atkin Matthew K. Brennaman © 2018 Tyler William Farnsworth ALL RIGHTS RESERVED ii ABSTRACT Tyler William Farnsworth: Strong and weak interlayer interactions of two-dimensional materials and their assemblies (Under the direction of Scott C. Warren) The ability to control the properties of a macroscopic material through systematic modification of its component parts is a central theme in materials science. This concept is exemplified by the assembly of quantum dots into 3D solids, but the application of similar design principles to other quantum-confined systems, namely 2D materials, remains largely unexplored. Here I demonstrate that solution-processed 2D semiconductors retain their quantum-confined properties even when assembled into electrically conductive, thick films. Structural investigations show how this behavior is caused by turbostratic disorder and interlayer adsorbates, which weaken interlayer interactions and allow access to a quantum- confined but electronically coupled state. I generalize these findings to use a variety of 2D building blocks to create electrically conductive 3D solids with virtually any band gap. I next introduce a strategy for discovering new 2D materials. Previous efforts to identify novel 2D materials were limited to van der Waals layered materials, but I demonstrate that layered crystals with strong interlayer interactions can be exfoliated into few-layer or monolayer materials. -
New Mineral Names*
American Mineralogist, Volume 62, pages 1259-1262, 1977 NewMineral Names* MtcHe.rr-Flrlscsnn, Lours J. CesRrAND ADoLF Pe.ssr Franzinite* Six microprobe analyses gave (range and av.): AsrOu 44.96-45.68,45.36; CuO 16.84-20.22,18.81; ZnO 16.78-18.57, Stefano Merlino and Paolo Orlandi (1977)Franzinite, a new min- 17.90;CdO l3 58-14.93,14.08; CaO 0.41-l.ll' 0.80; PbO 0.14- eral phase from Pitigliano,ltaly. Neues Jahrb. Mineral. Mon- 1.42,0.63: MnO 0.'79-1.27,1.07; sum 97 8l-99 54' 98.65 percent, atsh., 163-167. corresponding to (Cu,Zn,Cd).(AsOa), with Cu:Zn:Cd : 1.19: Microchemical analysis gave SiO, 32.44, Al2Os 25.21, Fe"O" Lll:0.55. The mineral is readily dissolvedby concentratedacids 0.04,MgO 0.14,CaO 12.08,Na,O 11.50,K,O 4.24,SOa 10.65, CO, X-ray study showsthe mineral to be monoclinic,space group 12' 154, Cl 036,H,O 1.88,sum 100.08- (O:Cl,) 0.08 : 100.00 Im. or 12/m, a ll.65, b 12.68,c 6.87(all + 0.01A)' B 98 95 + 0.05'' percent. "SiO, and AlrO, were determined by X-ray fluorescence, Z = 6, G calc 4.95 The strongest X-ray lines (46 given) are 6.41 (vvs) account being taken of the proper correction factor for S and Cl (MS) (020, l0T), 3.29 (vSXll2), 2.876 (vSX400), 2.79s and assuming that the weight percentages sum up to 100 0." (222, 321, 240), 1.644(MS). -
Christite, a New Thallium Mineral from the Carlin Gold Deposit, Nevada
American Mineralogist, Volume62, pages421425, 1977 Christite,a newthallium mineral from the Carlin golddeposit, Nevada ARruuRS. Rlorxn U.S. GeologicalSuruey, Menlo Park, California 94025 FnnNr W. Dlcrsor Departmentof Geology,Stanford Uniuersity St anfo rd, Cal ift rnia 9430 5 JoHNF. Slecr U.S. GeologicalSuruey, Reston, Virginia 22092 lNn KevtNL. Bnowx ChemistryDiuision, Diuision of Scientffic and IndustrialResearch, Petone, New Zealand Abstract Christite,TlHgAsSr, occurs with realgar,orpiment, and loranditein bariteveins and with realgar,lorandite, and getchellitein mineralizedcarbonaceous silty dolomite in the Carlin gold deposit,north-central Nevada. The mineralis namedfor Dr. CharlesL. Christof the U.S. GeologicalSurvey. The color is crimsonor deep red, but variesto bright orangein thinnerplates and crystals;the streakis bright orange,and the lusteris adamantine.The mineralis monoclinic,space group P2,/n,a -- 6.113(l),b = 16.188(4),c = 6.1Il(l) A, with0 : 96.71(2)',Z = 4, and cell volume: 600.6A8. Strongest X-ray powderdiffraction lines, in A, andtheir relative intensities are2.98 (10),3.62 (8),3.49 (6),2.692(6),2.216 (5),4.03 (6), and 3.36(5). Electronmicroprobe analyses gave Tl 35.2,Hg 35.1,As 13.1,S 16.6,sum 100.0 weight percent.The mineraloccurs in smallsubhedral to anhedralgrains which usuallylack well-developedforms but may showa bladedor flattenedhabit. Synthetic crystals are tabular, show{010) and {T0l}pinacoids, and {1l0} and {01l} prisms,and haveperfect {010}, excellent {ll0} and {001},and good {T0l} cleavages.Vickers hardness varied from 28.3-34.6and averaged31.5 kg mm-' (10 determinations).Density of syntheticTlHgAsSs is 6.2(2)(meas) and6.37g cm-e (calc).In reflectedlight christiteis grayish-whitewith a faint blue tint, lacks visiblebireflectance, is anisotropic,and has a brilliant red-orangeinternal reflection. -
Dictionary of Geology and Mineralogy
McGraw-Hill Dictionary of Geology and Mineralogy Second Edition McGraw-Hill New York Chicago San Francisco Lisbon London Madrid Mexico City Milan New Delhi San Juan Seoul Singapore Sydney Toronto All text in the dictionary was published previously in the McGRAW-HILL DICTIONARY OF SCIENTIFIC AND TECHNICAL TERMS, Sixth Edition, copyright ᭧ 2003 by The McGraw-Hill Companies, Inc. All rights reserved. McGRAW-HILL DICTIONARY OF GEOLOGY AND MINERALOGY, Second Edi- tion, copyright ᭧ 2003 by The McGraw-Hill Companies, Inc. All rights reserved. Printed in the United States of America. Except as permitted under the United States Copyright Act of 1976, no part of this publication may be reproduced or distributed in any form or by any means, or stored in a database or retrieval system, without the prior written permission of the publisher. 1234567890 DOC/DOC 09876543 ISBN 0-07-141044-9 This book is printed on recycled, acid-free paper containing a mini- mum of 50% recycled, de-inked fiber. This book was set in Helvetica Bold and Novarese Book by the Clarinda Company, Clarinda, Iowa. It was printed and bound by RR Donnelley, The Lakeside Press. McGraw-Hill books are available at special quantity discounts to use as premi- ums and sales promotions, or for use in corporate training programs. For more information, please write to the Director of Special Sales, McGraw-Hill, Professional Publishing, Two Penn Plaza, New York, NY 10121-2298. Or contact your local bookstore. Library of Congress Cataloging-in-Publication Data McGraw-Hill dictionary of geology and mineralogy — 2nd. ed. p. cm. “All text in this dictionary was published previously in the McGraw-Hill dictionary of scientific and technical terms, sixth edition, —T.p. -
Oreshoot Zoning in the Carlin-Type Betze Orebody, Goldstrike Mine, Eureka County, Nevada
Oreshoot Zoning in the Carlin-type Betze Orebody, Goldstrike Mine, Eureka County, Nevada By Stephen G. Peters1, Gregory C. Ferdock2, Maria B. Woitsekhowskaya1, Robert Leonardson3, and Jerry Rahn3 Open-File Report 98–620 1998 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY 1U.S. Geological Survey, Reno Field Office, Mackay School of Mines, MS-176, University of Nevada, Reno, Nevada 89557-0047 2Department of Geological Sciences, Mackay School of Mines, University of Nevada, Reno, Nevada 89557-0047 3Mine Geology Department, Barrick Goldstrike Mines, Inc., P.O. Box 29, Elko, Nevada 89803. Oreshoot Zoning in the Carlin-type Betze Orebody, Goldstrike Mine, Eureka County, Nevada by Stephen G. Peters1, Gregory C. Ferdock2, Maria B. Woitsekhowskaya1, Robert Leonardson3, and Jerry Rahn3 1U.S. Geological Survey, Reno, Nevada. 2Mackay School of Mines, University of Nevada, Reno, Nevada. 3Barrick Goldstrike Mines, Inc., Elko, Nevada Abstract Field and laboratory investigations of the giant Betze gold orebody, the largest Carlin-type deposit known, in the north-central Carlin trend, Nevada document that the orebody is composed of individual high-grade oreshoots that contain different geologic, mineralogic, and textural characteristics. The orebody is typical of many structurally controlled Carlin-type deposits, and is hosted in thin-bedded, impure carbonate or limy siltstone, breccia bodies, and intrusive or calc-silicate rock. -
Σ24S48, a New Sulfosalt from the Vorontsovskoe Gold Deposit
Preprints (www.preprints.org) | NOT PEER-REVIEWED | Posted: 3 May 2018 doi:10.20944/preprints201805.0067.v1 Peer-reviewed version available at Minerals 2018, 8, 218; doi:10.3390/min8050218 1 Tsygankoite, Mn8Tl8Hg2(Sb21Pb2Tl)Σ24S48, a new 2 sulfosalt from the Vorontsovskoe gold deposit, 3 Northern Urals, Russia 4 Anatoly V. Kasatkin1, Emil Makovicky2, Jakub Plášil3*, Radek Škoda4, Atali A. Agakhanov1, 5 Vladimir Y. Karpenko1 and Fabrizio Nestola5 6 7 1 Fersman Mineralogical Museum of Russian Academy of Sciences, Leninsky Prospekt 18-2, 119071 Moscow, 8 Russia; [email protected] (A.K.); [email protected] (A.A.); [email protected] (V.K.) 9 2 Department of Geoscience and Resource Management, University of Copenhagen, Østervoldgade 10, DK-1350, 10 Copenhagen K, Denmark; [email protected] 11 3 Institute of Physics ASCR, v.v.i., Na Slovance 1999/2, 18221 Praha 8, Czech Republic 12 4 Department of Geological Sciences, Faculty of Science, Masaryk University, Kotlářská 2, 611 37, Brno, Czech 13 Republic; [email protected] 14 5 Dipartimento di Geoscienze, Università di Padova, Via Gradenigo 6, I-35131, Padova, Italy; 15 [email protected] 16 * Correspondence: [email protected]; Tel. : +420-775-21-27-57 17 18 19 Abstract: Tsygankoite, ideally Mn8Tl8Hg2(Sb21Pb2Tl)Σ24S48, is a new sulfosalt discovered at the 20 Vorontsovskoe gold deposit, Northern Urals, Russia. It occurs as lath-like elongated crystals up to 21 0.2 mm embedded in calcite-dolomite-clinochlore matrix. The associating minerals also include 22 aktashite, alabandite, arsenopyrite, barite, cinnabar, fluorapatite, orpiment, pyrite, realgar, 23 routhierite, sphalerite, tilasite, titanite, etc. -
Kobe, Japan, July 23-28
19TH GENERAL MEETING OF THE INTERNATIONAL MINERALOGICAL ASSOCIATION KOBE, JAPAN, JULY 23-28 COMMISSION ON ORE MINERALOGY REPORT OF THE SULFOSALT SUBCOMMITTEE BY Y. MOËLO (SECRETARY) AND E. MAKOVICKY (ASSOCIATE SECRETARY) & N.N. MOZGOVA (PAST PRESIDENT OF THE SULFOSALT SUBCOMMITTEE), J.L. JAMBOR, N. COOK, A. PRING, W. PAAR, E. H. NICKEL, S. GRAESER, S. KARUP-MOLLER, T. BALIĆ-ŽUNIĆ, W. G. MUMME, F. VURRO, D. TOPA, L. BINDI, K. BENTE - 1 - SULFOSALT SUB-COMMITTEE – INTERNAL REPORT Preamble Y. Moëlo & E. Makovicky This report deals with a general reexamination of the systematics of sulfosalts. In the Part I are presented generalities concerning the definition and chemistry of sulfosalts, as well as some basic principles relative to their crystal chemical classification. Part II is a detailed presentation of all known sulfosalts species, with selected references about their definition (if recent) and crystal structure (when solved). Problems concerning the definition and nomenclature of some species are discussed on the basis of published data. This internal report will be provided to members of the C.O.M. for critical reading, in order that they may give additional information, as well as suggest corrections. A copy will also be sent to the Chairman of the CNMMN of the IMA, for information of the national representatives of this commission, who are also invited to give their comments. While Part I was written by ourselves (E. M. & Y. M.), Part II reflects a fruitful collaboration, past or present, of many specialists of sulfosalt mineralogy. Their names are given at the beginning of part II. It is a provisional list, until the final approval of the official report these co-authors; some names may be added later when relevant.