1 Revision 1 Single-Crystal Elastic Properties of Minerals and Related
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Structure and Composition OXIDATION ZONE
OXIDATION ZONE Structure and Composition The first scanty information on the oxidation zone of the Rubtsovskoe deposit was obtained as a result of drilling in the early 1970s. Three major subzones were distinguished downward: (1) a leached oxidized ore zone largely composed of iron hydroxides and kaolinite; (2) a secondary oxide enrichment subzone with cuprite, native copper, malachite, azurite, cerus - site; and (3) a secondary sulfide enrichment subzone (that transitions to an underlying zone of mixed ores) with chalcocite and covellite (Stroitelev et al. , 1996). As a result of our observation in underground workings, the structure, min - eralogy, and genetic features of the oxidation zone of the deposit were spec - ified substantially. The top of the orebody is supergene altered to the highest degree at the WSW flank, where it is located higher in altitude. The upper boundary of the orebody gently plunges ENE and the oxidation zone (we do not discuss the mixed ores) gradually pinches out; the oxidation zone extends along the strike of the orebody for approximately 300 m. In the WSW part of the ore - body, the oxidized ores occur in the altitude interval from +137–138 to +163 m. The lower boundary of the oxidized ores rise toward the ESE and the main part of the oxidation zone occurs in the range of +144–145 to +153–157 m. The oxidized part of the orebody varies from 2 to 8 m in thickness, reaching 15–17 m in swells and occasionally more than 20 m. Both underlying and overlapping rocks are dominated by clayey minerals; these are wall-rock argillaceous alterations, frequently altered as a result of ore oxidation especially adjacent to the contact of the orebody. -
Calaverite Aute2 C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Monoclinic
Calaverite AuTe2 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m or 2. Bladed and short to slender prisms elongated k [010], striated k [010], to 1 cm; also massive, granular. Twinning: Common on {110}, less common on {031} and {111}. Physical Properties: Fracture: Uneven to subconchoidal. Tenacity: Brittle. Hardness = 2.5–3 VHN = 197–213 (100 g load). D(meas.) = 9.10–9.40 D(calc.) = 9.31 Optical Properties: Opaque. Color: Grass-yellow to silver-white; white in reflected light. Streak: Greenish to yellowish gray. Luster: Metallic. Pleochroism: Weak. Anisotropism: Weak. R1–R2: (400) 45.7–54.4, (420) 48.4–57.1, (440) 51.1–59.6, (460) 53.6–61.8, (480) 56.0–63.6, (500) 57.9–65.2, (520) 59.4–66.4, (540) 60.6–67.3, (560) 61.3–68.0, (580) 61.8–68.3, (600) 62.2–68.4, (620) 62.5–68.6, (640) 62.7–68.5, (660) 62.8–68.4, (680) 62.9–68.2, (700) 63.0–68.1 Cell Data: Space Group: C2/m or C2. a = 7.1947(4) b = 4.4146(2) c = 5.0703(3) β =90.038(4)◦ Z=2 X-ray Powder Pattern: Cripple Creek, Colorado, USA. 3.02 (10), 2.09 (8), 2.20 (4), 2.93 (3), 1.758 (3), 1.689 (3), 1.506 (3) Chemistry: (1) (2) (3) Au 41.66 42.15 43.59 Ag 0.77 0.60 Te 57.87 57.00 56.41 Total 100.30 99.75 100.00 (1) Cripple Creek, Colorado, USA. -
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 -
The Albert Silver Mine and Trippkeite Occurrence, Mpumalanga, South Africa
The Albert silver mine and trippkeite occurrence, Mpumalanga, South Africa Paul M.P.B. Meulenbeld, Department of Water Affairs PO Box 1675 Bronkhorstspruit South Africa, [email protected]. Wiebke Grote, Department of Geology University of Pretoria, Private bag X20 Hatfield, Pretoria 0028, [email protected] Sabine Verryn, XRD Analytical & Consulting, Pretoria, 75 Kafue street Lynnwood Glen, 0081, [email protected] Dr. Paul M.P.B. Meulenbeld is a scientific manager with the Department of Water Affairs, a trained geophysicist and mineral collector. He has a sound knowledge about southern Africa’s mineral deposits and visits abandoned mines in his spare time. One of his last remarkable discoveries was the occurrence of chapmanite at the old Argent silver and lead deposit, Delmas, Mpumalanga, South Africa. Wiebke Grote is responsible for XRD analysis at the Department of Geology, University of Pretoria where prior to this position she was the curator of the geological museum at the same institution. Dr. Sabine Verryn is the owner of XRD Analytical & Consulting. She is the current Vice chair of the Mineralogical Association of South Africa. INTRODUCTION Around 1885 the ore deposit of the Albert Silver mine was discovered and production continued intermittently until 1914 (Robb, Robb, and Walraven 1994). The Albert Silver mine is situated on the farm Roodepoortjie 250JR, north of Bronkhorstspruit, some 80 km east-northeast of Pretoria in Mpumalanga, South Africa (Figure 1) (Robb, Robb, and Walraven 1994). No detailed description of the mine is known to have been published, but a layout plan and a plan indicating the extent of the underground workings (Figure 2), amongst a surface geophysical study of the ore bodies was given by Van Zijl (1965). -
Type of the Paper (Article
Conference Proceedings Paper Gold deposits in Greece: Hypogene ore mineralogy as a guide for precious and critical metal exploration Panagiotis Voudouris 1,*, Paul G. Spry 2, Vasilios Melfos 3, Karsten Haase 4, Reiner Klemd 4, Constantinos Mavrogonatos 1, Alexander Repstock 5 and Dimitrios Alfieris 6 Published: date Academic Editor: name 1 Department of Mineralogy and Petrology, Faculty of Geology & Geoenvironment, National and Kapodistrian University of Athens, Greece; [email protected]; [email protected] 2 Department of Geological and Atmospheric Sciences, Iowa State University, Ames IA 50011-1027, USA ([email protected]); 3 Department of Mineralogy-Petrology-Economic Geology, Faculty of Geology, Aristotle University of Thessaloniki, Greece; [email protected] 4 GeoZentrum Nordbayern, Universität Erlangen-Nürnberg, Erlangen, Germany; [email protected]; [email protected] 5 Institut für Geologie, TU Bergakademie Freiberg, Germany; [email protected] 6 Kairi str., 15126, Athens, Greece; [email protected] * Correspondence: [email protected]; Tel.: +30-210-7274129 Abstract: Gold deposits in Greece are spatially associated with back-arc/arc related volcanic, subvolcanic and plutonic rocks, which were controlled by extensional kinematic conditions when metamorphic core complexes in the Rhodope-Serbomacedonian- and Attico-Cycladic Massifs were uplifted to near surface levels over the south-westward retreating Hellenic subduction zone. Porphyry Cu-Mo-Au, high-intermediate sulfidation epithermal Au-Ag deposits and other intrusion-related proximal to distal systems (skarn, carbonate replacement, metamorphic rock-hosted quartz veins) are characterized by enrichment of trace metallic minerals like bismuth sulfosalts and Bi-sulfotellurides, precious- and base metal tellurides and Se-bearing phases, which can be considered as pathfinder minerals for gold as they are intimately associated with gold-bearing ores. -
Entropy Principle and Recent Results in Non-Equilibrium Theories
Entropy 2014, 16, 1756-1807; doi:10.3390/e16031756 OPEN ACCESS entropy ISSN 1099-4300 www.mdpi.com/journal/entropy Article Entropy Principle and Recent Results in Non-Equilibrium Theories Vito Antonio Cimmelli 1;*, David Jou 2, Tommaso Ruggeri 3 and Péter Ván 4;5;6 1 Department of Mathematics, Computer Science and Economics, University of Basilicata, Potenza 85100, Italy 2 Departament de Física, Universitat Autònoma de Barcelona, Bellaterra, and Institut d’Estudis Catalans, Barcelona, Catalonia 08193, Spain; E-Mail: [email protected] 3 Department of Mathematics and Research Center of Applied Mathematics, University of Bologna, Bologna 40123, Italy; E-Mail: [email protected] 4 Department of Theoretical Physics, Wigner Research Centre for Physics, Institute for Particle and Nuclear Physics, Budapest 1121, Hungary; E-Mail: [email protected] 5 Department of Energy Engineering, BME, Budapest 1111, Hungary 6 Montavid Thermodynamic Research Group, Budapest 1112 , Hungary * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +39-097-120-5885; Fax: +39-097-120-5896. Received: 30 December 2013; in revised form: 27 January 2014 / Accepted: 7 March 2014 / Published: 24 March 2014 Abstract: We present the state of the art on the modern mathematical methods of exploiting the entropy principle in thermomechanics of continuous media. A survey of recent results and conceptual discussions of this topic in some well-known non-equilibrium theories (Classical irreversible thermodynamics CIT, Rational thermodynamics RT, Thermodynamics of irreversible processes TIP, Extended irreversible thermodynamics EIT, Rational Extended thermodynamics RET) is also summarized. Keywords: continuum thermodynamics; entropy principle; rational thermodynamics; classical irreversible thermodynamics; extended irreversible thermodynamics; rational extended thermodynamics; exploitation of second law PACS Classification: 03.50.-z, 05.70.Ln, 05.70.Ce Entropy 2014, 16 1757 1. -
Chrisstanleyite Ag2pd3se4 C 2001-2005 Mineral Data Publishing, Version 1
Chrisstanleyite Ag2Pd3Se4 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m or 2. Anhedral crystals, to several hundred µm, aggregated in grains. Twinning: Fine polysynthetic and parquetlike, characteristic. Physical Properties: Tenacity: Slightly brittle. Hardness = ∼5 VHN = 371–421, 395 average (100 g load), D(meas.) = n.d. D(calc.) = 8.30 Optical Properties: Opaque. Color: Silvery gray. Streak: Black. Luster: Metallic. Optical Class: Biaxial. Pleochroism: Slight; pale buff to slightly gray-green buff. Anisotropism: Moderate; rose-brown, gray-green, pale bluish gray, dark steel-blue. Bireflectance: Weak to moderate. R1–R2: (400) 35.6–43.3, (420) 36.8–44.2, (440) 37.8–45.3, (460) 39.1–46.7, (480) 40.0–47.5, (500) 41.1–48.0, (520) 42.1–48.5, (540) 42.9–48.7, (560) 43.5–49.1, (580) 44.1–49.3, (600) 44.4–49.5, (620) 44.6–49.6, (640) 44.5–49.3, (660) 44.4–49.2, (680) 44.2–49.1, (700) 44.0–49.0 Cell Data: Space Group: P 21/m or P 21. a = 6.350(6) b = 10.387(4) c = 5.683(3) β = 114.90(5)◦ Z=2 X-ray Powder Pattern: Hope’s Nose, England. 2.742 (100), 1.956 (100), 2.688 (80), 2.868 (50b), 2.367 (50), 1.829 (30), 2.521 (20) Chemistry: (1) (2) (3) Pd 37.64 35.48 37.52 Pt 0.70 Hg 0.36 Ag 25.09 24.07 25.36 Cu 0.18 2.05 Se 36.39 38.50 37.12 Total 99.30 101.16 100.00 (1) Hope’s Nose, England; by electron microprobe, average of 26 analyses; corresponding to (Ag2.01Cu0.02)Σ=2.03Pd3.02Se3.95. -
European Journal of Mineralogy
Title Grundmannite, CuBiSe<SUB>2</SUB>, the Se-analogue of emplectite, a new mineral from the El Dragón mine, Potosí, Bolivia Authors Förster, Hans-Jürgen; Bindi, L; Stanley, Christopher Date Submitted 2016-05-04 European Journal of Mineralogy Composition and crystal structure of grundmannite, CuBiSe2, the Se-analogue of emplectite, a new mineral from the El Dragόn mine, Potosí, Bolivia --Manuscript Draft-- Manuscript Number: Article Type: Research paper Full Title: Composition and crystal structure of grundmannite, CuBiSe2, the Se-analogue of emplectite, a new mineral from the El Dragόn mine, Potosí, Bolivia Short Title: Composition and crystal structure of grundmannite, CuBiSe2, Corresponding Author: Hans-Jürgen Förster Deutsches GeoForschungsZentrum GFZ Potsdam, GERMANY Corresponding Author E-Mail: [email protected] Order of Authors: Hans-Jürgen Förster Luca Bindi Chris J. Stanley Abstract: Grundmannite, ideally CuBiSe2, is a new mineral species from the El Dragόn mine, Department of Potosí, Bolivia. It is either filling small shrinkage cracks or interstices in brecciated kruta'ite−penroseite solid solutions or forms independent grains in the matrix. Grain size of the anhedral to subhedral crystals is usually in the range 50−150 µm, but may approach 250 µm. Grundmannite is usually intergrown with watkinsonite and clausthalite; other minerals occasionally being in intimate grain-boundary contact comprise quartz, dolomite, native gold, eskebornite, umangite, klockmannite, Co-rich penroseite, and three unnamed phases of the Cu−Bi−Hg−Pb−Se system, among which is an as-yet uncharacterizedspecies with the ideal composition Cu4Pb2HgBi4Se11. Eldragόnite and petrovicite rarely precipitated in the neighborhood of CuBiSe2. Grundmannite is non-fluorescent, black and opaque with a metallic luster and black streak. -
Mineralogy of Zn–Hg–S and Hg–Se–S Series Minerals in Carbonate-Hosted Mercury Deposits in Western Hunan, South China
minerals Article Mineralogy of Zn–Hg–S and Hg–Se–S Series Minerals in Carbonate-Hosted Mercury Deposits in Western Hunan, South China Jianping Liu 1,2, Yanan Rong 1 and Shugen Zhang 1,* 1 Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083, China; [email protected] (J.L.); [email protected] (Y.R.) 2 Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510460, China * Correspondence: [email protected]; Tel.: +86-731-888-30616 Academic Editor: Radostina Atanassova Received: 10 May 2017; Accepted: 12 June 2017; Published: 15 June 2017 Abstract: Among the Zn–Hg–S and Hg–Se–S series minerals, Hg-bearing sphalerite and metacinnabar are uncommon in ore deposits, but they are useful indicators of temporal variation of ore forming fluids, as well as presenting metallurgical implications for Hg-bearing deposits. To understand the Hg–Zn–Se mineralization system of the Tongren–Fenghuang Hg Belt (TFHB), the Zn–Hg–S and Hg–Se–S series minerals of the Chashula Hg–Zn and Dongping Hg–Ag–Se carbonate-hosted deposits were studied by microscopic observation, electron-probe microanalysis, and X-ray diffraction analysis. Observations show that the Chashula and Dongping deposits experienced two stages of mineralization (Stages 1 and 2). The pyrite, sphalerite I (Hg-poor sphalerite), and quartz formed in Stage 1, while the Zn-bearing cinnabar, sphalerite II (Hg-bearing sphalerite), cinnabar, selenium metacinnabar, and Ag minerals formed in Stage 2. The Hg-bearing sphalerite, containing 13.36–22.26 wt % Hg (average 18.73 wt % Hg), replaces sphalerite I (0.00–1.31 wt % Hg). -
General Index Vols. XLI-L, Third Series
GENERAL INDEX OF VOLUMES XLI-L OF THE THIRD SERIES. WInthe references to volumes xli to I, only the numerals i to ir we given. NOTE.-The names of mineral8 nre inaerted under the head ol' ~~IBERALB:all ohitllary notices are referred to under OBITUARY. Under the heads BO'PANY,CHK~I~TRY, OEOLO~Y, Roo~s,the refereuces to the topics in these department8 are grouped together; in many cases, the same references appear also elsewhere. Alabama, geological survey, see GEOL. REPORTSand SURVEYS. Abbe, C., atmospheric radiation of Industrial and Scientific Society, heat, iii, 364 ; RIechnnics of the i. 267. Earth's Atmosphere, v, 442. Alnska, expedition to, Russell, ii, 171. Aberration, Rayleigh, iii, 432. Albirnpean studies, Uhler, iv, 333. Absorption by alum, Hutchins, iii, Alps, section of, Rothpletz, vii, 482. 526--. Alternating currents. Bedell and Cre- Absorption fipectra, Julius, v, 254. hore, v, 435 ; reronance analysis, ilcadeiny of Sciences, French, ix, 328. Pupin, viii, 379, 473. academy, National, meeting at Al- Altitudes in the United States, dic- bany, vi, 483: Baltimore, iv, ,504 : tionary of, Gannett, iv. 262. New Haven, viii, 513 ; New York, Alum crystals, anomalies in the ii. 523: Washington, i, 521, iii, growth, JIiers, viii, 350. 441, v, 527, vii, 484, ix, 428. Aluminum, Tvave length of ultra-violet on electrical measurements, ix, lines of, Runge, 1, 71. 236, 316. American Association of Chemists, i, Texas, Transactions, v, 78. 927 . Acoustics, rrsearchesin, RIayer, vii, 1. Geological Society, see GEOL. Acton, E. H., Practical physiology of SOCIETYof AMERICA. plants, ix, 77. Nuseu~nof Sat. Hist., bulletin, Adams, F. -
Mineral Formation on Metallic Copper in A'future Repository Site
riVI n L no *7 SE9800146 SKI Report 98:7 Mineral Formation on Metallic Copper in a "Future Repository Site Environment": Textural Considerations Based on Natural Analogs Orjan Amcoff January 1998 ISSN 1104-1374 ISRN SKI-R-9/7-SE • / STATENS KARNKRAFTINSPEKTION v;"- Swedish Nuclear Power Inspectorate SKI Report 98:7 Mineral Formation on Metallic Copper in a "Future Repository Site Environment7': Textural Considerations Based on Natural Analogs Orjan Amcoff University of Uppsala, Institute of Earth Sciences, Norbyvagen 18B, SE-752 36 Uppsala, Sweden January 1998 SKI Project Number 95112 This report concerns a study which has been conducted for the Swedish Nuclear Powei Inspectorate (SKI). The conclusions and viewpoints presented in the report are those of the author and do not necessarily coincide with those of the SKI. Norstedts Tryckeri AB Stockholm 1998 TABLE OF CONTENTS 1 INTRODUCTION 4 2 ORE MINERAL TEXTURES 5 2.1 GENERAL 5 2.2 SPECIFIC TEXTURES 6 2.2.1 The eutectoid texture 6 2.2.2 Exsolution textures 7 2.2.3 Textures formed during growth of new minerals in a pre-existing rock matrix 8 2.2.4 Dendritic textures 10 2.3 SPECIFIC TEXTURES IN THE LOW-TEMPERATURE ENVIRONMENT 11 2.4 SPECIFIC MINERAL TEXTURES 12 2.4.1 Native copper 13 2.4.2 Chalcocite 13 2.4.3 Bornite 14 2.4.4 Covellite 14 2.4.5 Chalcopyrite 15 2.4.6 Bornite 15 2.4.7 Tenorite 15 2.4.8 Malachite and Azurite 16 3 LOW-TEMPERATURE COPPER ORE DEPOSITS 16 3.1 FORMATION OF ORE MINERALS: GENERAL PRINCIPLES 16 3.2 DEPOSITS WITH NATIVE COPPER 18 3.2.1 Low-temperature primary sulphide ores of the Red Bed type 21 4 DISCUSSION 23 4.1 NATURAL ANALOGS 23 4.2 COPPER-MINERAL INTERACTIONS ON THE CANISTERS: TEXTURAL AND CHEMICAL CONSIDERATIONS 25 4.2.1 Halogens in copper phases at the repository 30 5 CONCLUDING REMARKS 30 6 REFERENCES 33 7 FIGURE LEGENDS 38 SUMMARY. -
Selenium Minerals and the Recovery of Selenium from Copper Refinery Anode Slimes by C
http://dx.doi.org/10.17159/2411-9717/2016/v116n6a16 Selenium minerals and the recovery of selenium from copper refinery anode slimes by C. Wang*, S. Li*, H. Wang*, and J. Fu* and genesis of native selenium from Yutangba, #65'272 Enshi City, Hubei Province, China in 2004, and pointed out, from the different forms of native Since it was first identified in 1817, selenium has received considerable Se, that selenium can be interest. Native selenium and a few selenium minerals were discovered several decades later. With the increasing number of selenium minerals, activated,transformed, remobilized, and the occurrence of selenium minerals became the focus of much research. A enriched at sites such as in the unsaturated great number of selenium deposits were reported all over the world, subsurface zone or in the saturated zone (Zhu although few independent selenium deposits were discovered. Selenium is et al., 2005). The transport and deposition of obtained mainly as a byproduct of other metals, and is produced primarily selenium in felsic volcanic-hosted massive from the anode mud of copper refineries. This paper presents a compre- sulphide deposits of the Yukon Territory, hensive review of selenium minerals, as well as the treatment of copper Canada was studied and reported by Layton- refinery anode slimes for the recovery of selenium. Our focus is on the Matthews et al. (2005). selenium minerals, including their discovery and occurrence, and the Selenium is a comparatively rare and distribution of selenium resources. In addition, the main methods of greatly dispersed element. The average recovering selenium from copper anode slimes are summarized.