Mineral Ecology and Network Analysis of Chromium, Platinum
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Coulsonite Fev2o4—A Rare Vanadium Spinel Group Mineral in Metamorphosed Massive Sulfide Ores of the Kola Region, Russia
minerals Article Coulsonite FeV2O4—A Rare Vanadium Spinel Group Mineral in Metamorphosed Massive Sulfide Ores of the Kola Region, Russia Alena A. Kompanchenko Geological Institute of the Federal Research Centre “Kola Science Centre of the Russian Academy of Sciences”, 14 Fersman Street, 184209 Apatity, Russia; [email protected]; Tel.: +7-921-048-8782 Received: 24 August 2020; Accepted: 21 September 2020; Published: 24 September 2020 Abstract: This work presents new data on a rare vanadium spinel group mineral, i.e., coulsonite FeV2O4 established in massive sulfide ores of the Bragino occurrence in the Kola region, Russia. Coulsonite in massive sulfide ores of the Bragino occurrence is one of the most common vanadium minerals. Three varieties of coulsonite were established based on its chemical composition, some physical properties, and mineral association: coulsonite-I, coulsonite-II, and coulsonite-III. Coulsonite-I forms octahedral crystal clusters of up to 500 µm, and has a uniformly high content of 2 Cr2O3 (20–30 wt.%), ZnO (up to 4.5 wt.%), and MnO (2.8 wt.%), high microhardness (743 kg/mm ) and coefficient of reflection. Coulsonite-II was found in relics of quartz–albite veins in association with other vanadium minerals. Its features are a thin tabular shape and enrichment in TiO2 of up to 18 wt.%. Coulsonite-III is the most common variety in massive sulfide ores of the Bragino occurrence. Coulsonite-III forms octahedral crystals of up to 150 µm, crystal clusters, and intergrowths with V-bearing ilmenite, W-V-bearing rutile, Sc-V-bearing senaite, etc. Chemical composition of coulsonite-III is characterized by wide variation of the major compounds—Fe, V, Cr. -
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 -
Chromite Crystal Structure and Chemistry Applied As an Exploration Tool
Western University Scholarship@Western Electronic Thesis and Dissertation Repository February 2015 Chromite Crystal Structure and Chemistry applied as an Exploration Tool Patrick H.M. Shepherd The University of Western Ontario Supervisor Dr. Roberta L. Flemming The University of Western Ontario Graduate Program in Geology A thesis submitted in partial fulfillment of the equirr ements for the degree in Master of Science © Patrick H.M. Shepherd 2015 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Geology Commons Recommended Citation Shepherd, Patrick H.M., "Chromite Crystal Structure and Chemistry applied as an Exploration Tool" (2015). Electronic Thesis and Dissertation Repository. 2685. https://ir.lib.uwo.ca/etd/2685 This Dissertation/Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. Western University Scholarship@Western University of Western Ontario - Electronic Thesis and Dissertation Repository Chromite Crystal Structure and Chemistry Applied as an Exploration Tool Patrick H.M. Shepherd Supervisor Roberta Flemming The University of Western Ontario Follow this and additional works at: http://ir.lib.uwo.ca/etd Part of the Geology Commons This Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in University of Western Ontario - Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. Chromite Crystal Structure and Chemistry Applied as an Exploration Tool (Thesis format: Integrated Article) by Patrick H.M. -
Synthesis, Properties and Uses of Chromium-Based Pigments from The
Synthesis, properties and uses of chromium-based pigments from the Manufacture de Sèvres Louisiane Verger, Olivier Dargaud, Mathieu Chassé, Nicolas Trcera, Gwenaëlle Rousse, Laurent Cormier To cite this version: Louisiane Verger, Olivier Dargaud, Mathieu Chassé, Nicolas Trcera, Gwenaëlle Rousse, et al.. Syn- thesis, properties and uses of chromium-based pigments from the Manufacture de Sèvres. Journal of Cultural Heritage, Elsevier, 2018, 30, pp.26 - 33. 10.1016/j.culher.2017.09.012. hal-01777923 HAL Id: hal-01777923 https://hal.sorbonne-universite.fr/hal-01777923 Submitted on 25 Apr 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Synthesis, Properties and Uses of Chromium-Based Pigments from the Manufacture de Sèvres Louisiane Verger1,2, Olivier Dargaud2, Mathieu Chassé1, Nicolas Trcera3, Gwenaëlle Rousse4,5, Laurent Cormier1 1. Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Sorbonne Universités, UPMC Univ Paris 06, CNRS UMR 7590, Muséum national d'Histoire naturelle, IRD UMR 206, 4 place Jussieu, F-75005 Paris, France 2. Cité de la céramique - Sèvres et Limoges, 2 Place de la Manufacture, 92310 Sèvres, France 3. Synchrotron Soleil, 91190 Saint-Aubin 4 .Collège de France, Chimie du Solide et de l’Energie, UMR 8260, 11 place Marcelin Berthelot, 75231 Paris Cedex 05, France. -
Wickenburgite Pb3caal2si10o27² 3H2O
Wickenburgite Pb3CaAl2Si10O27 ² 3H2O c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Hexagonal. Point Group: 6=m 2=m 2=m: Tabular holohedral crystals, dominated by 0001 and 1011 , to 1.5 mm. As spongy aggregates of small, highly perfect f g f g individuals; as subparallel aggregates or rosettes; granular. Physical Properties: Cleavage: 0001 , indistinct. Tenacity: Brittle but tough. Hardness = 5 D(meas.) = 3.85 D(cfalc.) g= 3.88 Fluoresces dull orange under SW UV. Optical Properties: Transparent to translucent. Color: Colorless to white; rarely salmon-pink. Luster: Vitreous. Optical Class: Uniaxial ({). Dispersion: r < v; moderate. ! = 1.692 ² = 1.648 Cell Data: Space Group: P 63=mmc: a = 8.53 c = 20.16 Z = 2 X-ray Powder Pattern: Near Wickenburg, Arizona, USA. 10.1 (100), 3.26 (80), 3.93 (60), 3.36 (40), 2.639 (40), 5.96 (30), 5.04 (30) Chemistry: (1) (2) SiO2 42.1 40.53 Al2O3 7.6 6.88 PbO 44.0 45.17 CaO 3.80 3.78 H2O 3.77 3.64 Total 101.27 100.00 (1) Near Wickenburg, Arizona, USA. (2) Pb3CaAl2Si10O24(OH)6: [needsnew??formula] Occurrence: In oxidized hydrothermal veins, carrying galena and sphalerite, in quartz and °uorite gangue (near Wickenburg, Arizona, USA). Association: Phoenicochroite, mimetite, cerussite, willemite, crocoite, duftite, hemihedrite, alamosite, melanotekite, luddenite, ajoite, shattuckite, vauquelinite, descloizite, laumontite. Distribution: In the USA, in Arizona, at several localities south of Wickenburg, Maricopa Co., including the Potter-Cramer property, Belmont Mountains, and the Moon Anchor mine; on dumps at a Pb-Ag-Cu prospect in the Artillery Peaks area, Mohave Co.; and in the Dives (Padre Kino) mine, Silver district, La Paz Co. -
Chemistry, Geochemistry, and Geology of Chromium and Chromium Compounds
L1608_C02.fm Page 23 Thursday, July 15, 2004 6:57 PM 2 Chemistry, Geochemistry, and Geology of Chromium and Chromium Compounds William E. Motzer and Todd Engineers CONTENTS 2.1 Chromium Chemistry .................................................................................24 2.1.1 Background ......................................................................................24 2.1.2 Elemental/Metallic Chromium Characteristics .........................25 2.1.3 Ionic Radii ........................................................................................29 2.1.4 Oxidation States...............................................................................30 2.1.5 Stable and Radioactive Isotopes ...................................................31 2.1.6 Characteristics of Chromium Compounds.................................34 2.2 Natural Chromium Concentrations..........................................................34 2.2.1 Mantle ...............................................................................................46 2.2.2 Chromium Minerals........................................................................46 2.2.3 Chromium Ore Deposits................................................................46 2.2.3.1 Stratiform Mafic-Ultramafic Chromite Deposits .........62 2.2.3.2 Podiform- or Alpine-Type Chromite Deposits ............63 2.2.4 Crude Oil, Tars and Pitch, Asphalts, and Coal..........................63 2.2.5 Rock ...................................................................................................64 -
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. -
Italian Type Minerals / Marco E
THE AUTHORS This book describes one by one all the 264 mi- neral species first discovered in Italy, from 1546 Marco E. Ciriotti was born in Calosso (Asti) in 1945. up to the end of 2008. Moreover, 28 minerals He is an amateur mineralogist-crystallographer, a discovered elsewhere and named after Italian “grouper”, and a systematic collector. He gradua- individuals and institutions are included in a pa- ted in Natural Sciences but pursued his career in the rallel section. Both chapters are alphabetically industrial business until 2000 when, being General TALIAN YPE INERALS I T M arranged. The two catalogues are preceded by Manager, he retired. Then time had come to finally devote himself to his a short presentation which includes some bits of main interest and passion: mineral collecting and information about how the volume is organized related studies. He was the promoter and is now the and subdivided, besides providing some other President of the AMI (Italian Micromineralogical As- more general news. For each mineral all basic sociation), Associate Editor of Micro (the AMI maga- data (chemical formula, space group symmetry, zine), and fellow of many organizations and mine- type locality, general appearance of the species, ralogical associations. He is the author of papers on main geologic occurrences, curiosities, referen- topological, structural and general mineralogy, and of a mineral classification. He was awarded the “Mi- ces, etc.) are included in a full page, together cromounters’ Hall of Fame” 2008 prize. Etymology, with one or more high quality colour photogra- geoanthropology, music, and modern ballet are his phs from both private and museum collections, other keen interests. -
To Volume 55, 1970
THE AMERICAN MINERALOGIST. VOL, 55. NOVEMtsER.DECEMBER. 1970 INDEX TO VOLUME 55, 1970 The index for this volume attempts to combine the advantages of the content of the traditional subject index, with the computer storage and retrieval possibilities of the KWIC index that was used for volumes 52-54. This index is processed and printed from the input to the Bibli.ography and Iniler oJ Geology,under a contract arrangement with the American Geological Institute. Thanks are due them for their excellent cooperation in this initial venture. The content and layout of this index, and in particular the choice of sub- ject headings, and subheadings, is still evolving. General cornments and specific suggestions from users will be welcomed, and should be addressed to the Editor oI The American Mineralogisl. 2147 AUTHOR INDEX TO VOLUME 55 7-8 1440 Adams. John W. A convenient nonoxidizing heating method for metamict minerals tt-12 2141 Ahmed, E. F. R. (ed.) Crystallographiccomputing [book review] 7-8 1302 Akizuki, Mizuhiko. Slip structureof heated sphalerite 3-4 491 Albee, Arden L. Semiquantitative electron microprobe determination of Fer1 /Fer t and Mn:r /Mnr' in oxides and silicatesand its applicationto petrologicproblems 9-r0 1772 Alberti, Alberto. variation in diffractometer profiles of powder with a gaussian dispersionof the chemical composition t-2 299 Allmann, Rudolf. How to recognize O OH-and H:O in crystal structures determined by x-rays [abstr.] Allmann, Rudolf. How to recognize O: , OH', and H:O in crystal structures 5-6 1003 determined by x-rays Anderson, C. P. The crystal structuresof the humite minerals;ll, Chondrodite 7-8 1182 Anderson, Charles A. -
Anomalous Elastic Behavior of Phase Egg, Alsio3(OH), at High Pressures
American Mineralogist, Volume 104, pages 130–139, 2019 Anomalous elastic behavior of phase egg, AlSiO3(OH), at high pressures MAINAK MOOKHERJEE1,*, WENDY R. PANERO2, BERND WUNDER3, AND SANDRO JAHN4 1Earth, Ocean and Atmospheric Sciences, Florida State University, Tallahassee, Florida 32306, U.S.A. 2School of Earth Sciences, Ohio State University, Columbus, Ohio 43210, U.S.A. 3Deutsches GeoForschungsZentrum GFZ, Telegrafenberg, 14473 Potsdam, Germany 4Institut für Geologie und Mineralogie, Zülpicher Str. 49b, Universität zu Köln, 50674 Cologne, Germany ABSTRACT Phase egg, [AlSiO3(OH)], is an aluminosilicate hydrous mineral that is thermodynamically stable in lithological compositions represented by Al2O3-SiO2-H2O (ASH) ternary, i.e., a simplified ternary for the mineralogy of subducted sediments and continental crustal rocks. High-pressure and high-temperature experiments on lithological compositions resembling hydrated sedimentary layers in subducting slabs show that phase egg is stable up to pressures of 20–30 GPa, which translates to the transition zone to lower mantle depths. Thus, phase egg is a potential candidate for transporting water into the Earth’s mantle transition zone. In this study, we use first-principles simulations based on density functional theory to explore the pressure dependence of crystal structure and how it influences energetics and elasticity. Our results indicate that phase egg exhibits anomalous behavior of the pressure dependence of the elasticity at mantle transition zone depths (~15 GPa). Such anomalous behavior in the elastic- ity is related to changes in the hydrogen bonding O-H···O configurations, which we delineate as a transition from a low-pressure to a high-pressure structure of phase egg. -
1 #4771 REVISION 1 1 Revised January 13, 2014 2 Original
1 #4771 REVISION 1 2 Revised January 13, 2014 3 Original manuscript submitted October 15, 2013 4 5 MANTLE-DERIVED GUYANAITE IN A Cr-OMPHACITITE XENOLITH FROM MOSES 6 ROCK DIATREME, UTAH 7 8 Daniel J. Schulze 9 Department of Earth Sciences and Department of Chemical and Physical Sciences, 10 University of Toronto, Mississauga, Ontario, Canada L5L 1C6 11 Roberta L. Flemming 12 Department of Earth Sciences, Western University, London, Ontario, Canada N6A 5B7 13 Patrick H.M. Shepherd 14 Department of Earth Sciences, Western University, London, Ontario, Canada N6A 5B7 15 Herwart Helmstaedt 16 Department of Geological Sciences and Geological Engineering, Queen’s University, 17 Kingston, Ontario, Canada K7L 3N6 18 19 20 21 1 22 Abstract 23 Guyanaite, naturally occurring β-CrOOH, has been identified in a xenolith of Cr-rich 24 omphacitite from the Moses Rock diatreme in the Navajo Volcanic Field of the southwestern 25 United States. It occurs as the dominant phase in small clusters of accessory minerals, 26 intergrown with kosmochlor-rich omphacite, zincian chromite, eskolaite and carmichaelite. The 27 assemblage is interpreted as the result of metasomatism of chromite-bearing serpentinite by slab- 28 derived fluids during subduction of the Farallon Plate in Laramide time. At the time of 29 entrainment of the xenolith, the rock was undergoing prograde metamorphism, with guyanaite 30 dehydrating to eskolaite plus water. This reaction, and the coeval dehydration of the inferred 31 accompanying host serpentinites (which would have been much more volumetrically 32 significant), provided water for hydration of the subcontinental upper mantle, contributing to 33 uplift of the Colorado Plateau. -
Volume 116 No. 6 June 2016
VOLUME 116 NO. 6 JUNE 2016 The Southern African Institute of Mining and Metallurgy )) ) )) ) ) *Deceased * H. Simon (1957–1958) * W. Bettel (1894–1895) * M. Barcza (1958–1959) !! * A.F. Crosse (1895–1896) * R.J. Adamson (1959–1960) Mike Teke * W.R. Feldtmann (1896–1897) * W.S. Findlay (1960–1961) President, Chamber of Mines of South Africa * C. Butters (1897–1898) D.G. Maxwell (1961–1962) * J. Loevy (1898–1899) * J. de V. Lambrechts (1962–1963) ! !! * J.R. Williams (1899–1903) * J.F. Reid (1963–1964) Mosebenzi Zwane * S.H. Pearce (1903–1904) * D.M. Jamieson (1964–1965) Minister of Mineral Resources, South Africa * W.A. Caldecott (1904–1905) * H.E. Cross (1965–1966) * W. Cullen (1905–1906) * D. Gordon Jones (1966–1967) Rob Davies * E.H. Johnson (1906–1907) * P. Lambooy (1967–1968) Minister of Trade and Industry, South Africa * J. Yates (1907–1908) * R.C.J. Goode (1968–1969) Naledi Pandor * R.G. Bevington (1908–1909) * J.K.E. Douglas (1969–1970) Minister of Science and Technology, South Africa * A. McA. Johnston (1909–1910) * V.C. Robinson (1970–1971) * J. Moir (1910–1911) * D.D. Howat (1971–1972) * C.B. Saner (1911–1912) J.P. Hugo (1972–1973) !! * W.R. Dowling (1912–1913) * P.W.J. van Rensburg R.T. Jones * A. Richardson (1913–1914) (1973–1974) * G.H. Stanley (1914–1915) * R.P. Plewman (1974–1975) !!! * J.E. Thomas (1915–1916) * R.E. Robinson (1975–1976) C. Musingwini * J.A. Wilkinson (1916–1917) * M.D.G. Salamon (1976–1977) * G. Hildick-Smith (1917–1918) * P.A. Von Wielligh (1977–1978) ! !! * H.S.