Environmental Mineralogy Honours Shortcourse
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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. -
List of New Mineral Names: with an Index of Authors
415 A (fifth) list of new mineral names: with an index of authors. 1 By L. J. S~v.scs~, M.A., F.G.S. Assistant in the ~Iineral Department of the,Brltish Museum. [Communicated June 7, 1910.] Aglaurito. R. Handmann, 1907. Zeita. Min. Geol. Stuttgart, col. i, p. 78. Orthoc]ase-felspar with a fine blue reflection forming a constituent of quartz-porphyry (Aglauritporphyr) from Teplitz, Bohemia. Named from ~,Xavpo~ ---- ~Xa&, bright. Alaito. K. A. ~Yenadkevi~, 1909. BuU. Acad. Sci. Saint-P6tersbourg, ser. 6, col. iii, p. 185 (A~am~s). Hydrate~l vanadic oxide, V205. H~O, forming blood=red, mossy growths with silky lustre. Founi] with turanite (q. v.) in thct neighbourhood of the Alai Mountains, Russian Central Asia. Alamosite. C. Palaehe and H. E. Merwin, 1909. Amer. Journ. Sci., ser. 4, col. xxvii, p. 899; Zeits. Kryst. Min., col. xlvi, p. 518. Lead recta-silicate, PbSiOs, occurring as snow-white, radially fibrous masses. Crystals are monoclinic, though apparently not isom0rphous with wol]astonite. From Alamos, Sonora, Mexico. Prepared artificially by S. Hilpert and P. Weiller, Ber. Deutsch. Chem. Ges., 1909, col. xlii, p. 2969. Aloisiite. L. Colomba, 1908. Rend. B. Accad. Lincei, Roma, set. 5, col. xvii, sere. 2, p. 233. A hydrated sub-silicate of calcium, ferrous iron, magnesium, sodium, and hydrogen, (R pp, R',), SiO,, occurring in an amorphous condition, intimately mixed with oalcinm carbonate, in a palagonite-tuff at Fort Portal, Uganda. Named in honour of H.R.H. Prince Luigi Amedeo of Savoy, Duke of Abruzzi. Aloisius or Aloysius is a Latin form of Luigi or I~ewis. -
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INDEX,VOLUME 59* Absorption coefficients Albite, continued attapulgite 1113 1ow-, comparison with ussingite 347 clay ninerals 11r3 nelting in nultispecies fluid 598 dickite 274 Alexandrite, chrorniumIII centers in 159 hal loysite 274 hectorite I 113 ALLAN, DAVID illite 1113 with V. Brown, and J. Stark, Rocke kaolinite 274 and Minez,als of Califowi,a; reviewed metabentonite 1113 by J. Murdoch 387 nontronite 1113 Allemontite, see stibarsen 1331 srnectite 1113 ALLMAN,MICHAEL Absorption spectra with D.F. Lawrence, Geological alexandrite, synthetic 159 Labonatony Techni.ques reviewed apophyllite 62I ; by F.H. Manley and W.R. Powers IL42 garnet 565 olivine 244 A1lophane rhodonite.. shocked t77 dehydration, DTA, infrared spectra 1094 Acmite, Ti-, phase relations of 536 Almandine Actinolite overgrowth by grossularite- spessartine 558 coexisting with hoinblende 529 in netamorphic rocks, optical Arnerican Crystallographic Association, properties 22 abstracts, Spring neeting,1974 1L27 Activity coefficients Amphiboles of coexisting pyroxenes 204 actinolite 2? 529 Al -Ca-anphibole ADMS, HERBERTG. 22 compositions 22 with L.H. Cohen, and W. Klenent, Jr.; coordination polyhedra M High-low quartz inversion : Thermal of site atons in I 083 analysis studies to 7 kbar I 099 hornblende L, 22, 529, 604 ADAMS,JOHN W. magnesioarfvedsonite (authigenic) 830 with T. Botinelly, W.N. Sharp, and refraction indices 22 K. Robinson; Murataite, a new richterite, Mg-Fe- 518 conplex oxide from E1 Paso County, AMSTUTZ,G.C. Colorado L72 with A.J. Bernard, Eds., )nes in Errata 640 Sediments; reviewed by P.B. Barton 881 Aenigmatite ANDERSEN,C.A. in volcanic conplex, composition, and X-ray data Micz,opnobeAnalysis; reviewed by A.E. -
Copper-Nickel Mixed Oxide Catalysts from Layered Double Hydroxides For
Copper-nickel mixed oxide catalysts from layered double hydroxides for the hydrogen-transfer valorisation of lignin in organosolv pulping Iqra Zubair Awan, Giada Beltrami, Danilo Bonincontro, Olinda Gimello, Thomas Cacciaguerra, Nathalie Tanchoux, Annalisa Martucci, Stefania Albonetti, Fabrizio Cavani, Francesco Di Renzo To cite this version: Iqra Zubair Awan, Giada Beltrami, Danilo Bonincontro, Olinda Gimello, Thomas Cacciaguerra, et al.. Copper-nickel mixed oxide catalysts from layered double hydroxides for the hydrogen-transfer valori- sation of lignin in organosolv pulping. Applied Catalysis A : General, Elsevier, 2021, 609, pp.117929. 10.1016/j.apcata.2020.117929. hal-03080770 HAL Id: hal-03080770 https://hal.archives-ouvertes.fr/hal-03080770 Submitted on 17 Dec 2020 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. Copper-nickel mixed oxide catalysts from layered double hydroxides for the hydrogen-transfer valorisation of lignin in organosolv pulping. Iqra Zubair AWAN,a,b,1 Giada BELTRAMI,c Danilo BONINCONTRO,a,2 Olinda GIMELLO,b Thomas CACCIAGUERRA,b -
Thermaerogenite Cual2o4 - Crystal Data: Cubic
Thermaerogenite CuAl2O4 - Crystal Data: Cubic. Point Group: 4/m 3 2/m. As octahedral crystals to 0.02 mm displaying {111} modified by {110}, sometimes skeletal. Physical Properties: Cleavage: None. Fracture: Conchoidal. Tenacity: Brittle. Hardness = ~7 D(calc.) = 4.870 Optical Properties: Transparent to translucent. Color: Brown, yellow-brown, red-brown, brown- yellow, or brown-red; gray with yellowish internal reflections in reflected light. Streak: Yellow. Luster: Vitreous. Optical Class: Isotropic. R1-R2: (400) 16.4, (420) 16.0, (440) 15.7, (460) 15.4, (470) 15.2, (480) 15.1, (500) 14.8, (520) 14.5, (540) 14.2, (546) 14.2, (560) 14.0, (580) 13.7, (589) 13.6, (600) 13.2, (620) 13.2, (640) 13.0, (650) 12.9, (660) 12.8, (680) 12.5, (700) 12.3 - Cell Data: Space Group: Fd 3 m. a = 8.093(9) Z = [8] X-ray Powder Pattern: Arsenatnaya fumarole, Tolbachik volcano, Kamchatka Peninsula, Russia. 2.451 (100), 2.873 (65), 1.438 (30), 1.565 (28), 1.660 (16), 2.033 (10), 1.865 (6) Chemistry: (1) (2) CuO 25.01 43.83 ZnO 17.45 Al2O3 39.43 56.17 Cr2O3 0.27 Fe2O3 17.96 . Total 100.12 100.00 (1) Arsenatnaya fumarole, Tolbachik volcano, Kamchatka Peninsula, Russia; average of 4 electron microprobe analyses supplemented by Raman spectroscopy; corresponds to (Cu0.62Zn0.42)Σ=1.04 3+ (Al1.52Fe 0.44Cr0.01)Σ=1.97O4. (2) CuAl2O4. Polymorphism & Series: Continuous series with gahnite, discontinuous with cuprospinel. Mineral Group: Spinel supergroup. Occurrence: In cavities and overgrown on earlier oxide minerals, often epitaxially, as sublimates around a volcanic fumarole. -
New Mineral Species and Their Crystal Structures"
Title: Editorial for Special Issue "New Mineral Species and Their Crystal Structures" Author: Irina O. Galuskina, Igor V. Pekov Citation style: Galuskina Irina O., Pekov Igor V. (2019). Editorial for Special Issue "New Mineral Species and Their Crystal Structures". "Minerals" (Vol. 9, iss. 2 (2019), art. no 106), doi 10.3390/min9020106 minerals Editorial Editorial for Special Issue “New Mineral Species and Their Crystal Structures” Irina O. Galuskina 1,* and Igor V. Pekov 2 1 Faculty of Earth Sciences, University of Silesia, B˛edzi´nska60, 41-200 Sosnowiec, Poland 2 Faculty of Geology, Moscow State University, Vorobievy Gory, Moscow 119991, Russia; [email protected] * Correspondence: [email protected] Received: 17 January 2019; Accepted: 1 February 2019; Published: 13 February 2019 Mineralogy is the oldest and one of the most important sciences of the geological cycle. Minerals, the basis of overwhelming mass of solid matter in the universe, are direct subjects of investigation in mineralogy. Minerals, or mineral species, are generally solid crystalline substances. Their definition indicates that, they are: (1) naturally occurring; (2) belonging to the distinct structural type; (3) stable, varying merely in the relatively small limits of chemical composition. If a given mineral differs from other known species in its structure (2) and/or composition (3) then it can be considered as a new mineral species. According to the data of the Commission on New Minerals, Nomenclature and Classification (CNMNC) of the International Mineralogical Association (IMA) (http://nrmima.nrm.se/), there are currently about 5600 known mineral species. The number of minerals increases steadily year by year. -
Ophiolites from the Egyptian Shield: a Case for a Possible Inter-Arc Basin Origin ,' '"'!
MITI.ÖSTERR.MINER.GES. 148( 2003) OPHIOLITES FROM THE EGYPTIAN SHIELD: A CASE FOR A POSSIBLE INTER-ARC BASIN ORIGIN 2 A. Y. Abdel Aatl, E. S. Farahatl, G. Hoinkes & M. M. EI Mahalawil l Department of Geology Minia University, El-Minia 61 l l l, Egypt 2Jnstitute of Mineralogy and Petrology University of Graz, Universitätsplatz 2, A-8010 Graz, Austria The pyroxene and whole-rock chemistry of the ophiolitic metavolcanics of Wadi Um Seleimat (WUS) and Muweilih (MU) areas in the central Eastem Desert of Egypt are presented. WUS ophiolite suite seems to be intact where it comprises (from bottom to top): serpentinites, pyro xenites, metagabbros, massive diabases and pillowed metavolcanics. MU metavolcanics, about lO km to the southeast of WUS area, consists predominantly of metabasaltic-metadiabasic pillowed and massive lava flows together with the corresponding pyroclastics. These meta volcanics, together with their associated metagabbros and serpentinites, can be considered as a part of a dismembered ophiolite sequence. The mineral assemblage in WUS rocks is: albite, chlorite, epidote, titanite, calcite and quartz, which indicates a low greenschist facies (230-320'C) metamorphism. The mineral assemblage of MU metavolcanics includes: albite, actinolite, homblende, epidote, chlorite, titanite, calcite, quartz and ilmenite that reflectsa transitional greenschist-amphibolite facies metamorphism.Few samples of WUS contain plentiful clinopyroxene phenocrysts in plagioclase-free glassy ground mass. These features aretypical of rocks of boninitic affinity. Whole-rock and pyroxene chemistry demonstrate that the metavolcanics ofboth areas are mainly andesitic basalts with tholeiitic affinity. The boninitic affinity of some samples fromWUS area is shown on Ti0z-Si02/IOO-Na20 diagram of pyroxenes (Fig. -
A Comparative Study of Jadeite, Omphacite and Kosmochlor Jades from Myanmar, and Suggestions for a Practical Nomenclature
Feature Article A Comparative Study of Jadeite, Omphacite and Kosmochlor Jades from Myanmar, and Suggestions for a Practical Nomenclature Leander Franz, Tay Thye Sun, Henry A. Hänni, Christian de Capitani, Theerapongs Thanasuthipitak and Wilawan Atichat Jadeitite boulders from north-central Myanmar show a wide variability in texture and mineral content. This study gives an overview of the petrography of these rocks, and classiies them into ive different types: (1) jadeitites with kosmochlor and clinoamphibole, (2) jadeitites with clinoamphibole, (3) albite-bearing jadeitites, (4) almost pure jadeitites and (5) omphacitites. Their textures indicate that some of the assemblages formed syn-tectonically while those samples with decussate textures show no indication of a tectonic overprint. Backscattered electron images and electron microprobe analyses highlight the variable mineral chemistry of the samples. Their extensive chemical and textural inhomogeneity renders a classiication by common gemmological methods rather dificult. Although a deinitive classiication of such rocks is only possible using thin-section analysis, we demonstrate that a fast and non-destructive identiication as jadeite jade, kosmochlor jade or omphacite jade is possible using Raman and infrared spectroscopy, which gave results that were in accord with the microprobe analyses. Furthermore, current classiication schemes for jadeitites are reviewed. The Journal of Gemmology, 34(3), 2014, pp. 210–229, http://dx.doi.org/10.15506/JoG.2014.34.3.210 © 2014 The Gemmological Association of Great Britain Introduction simple. Jadeite jade is usually a green massive The word jade is derived from the Spanish phrase rock consisting of jadeite (NaAlSi2O6; see Ou Yang, for piedra de ijada (Foshag, 1957) or ‘loin stone’ 1999; Ou Yang and Li, 1999; Ou Yang and Qi, from its reputed use in curing ailments of the loins 2001). -
Compositional Effects on the Solubility of Minor and Trace Elements In
American Mineralogist, Volume 101, pages 1360–1372, 2016 SPINELS RENAISSANCE: THE PAST, PRESENT, AND FUTURE OF THOSE UBIQUITOUS MINERALS AND MATERIALS Compositional effects on the solubility of minor and trace elements in oxide spinel minerals: Insights from crystal-crystal partition coefficients in chromite exsolution VANESSA COLÁS1,2,*, JOSÉ ALBERTO PADRÓN-NAVARTA3, JOSÉ MARÍA GONZÁLEZ-JIMÉNEZ4, WILLIAM L. GRIFFIN5, ISABEL FANLO2, SUZANNE Y. O’REILLY5, FERNANDO GERVILLA6, JOAQUÍN A. PROENZA7, NORMAN J. PEARSON5, AND MONICA P. ESCAYOLA8 1Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria, 04510 Ciudad de México, México 2Universidad de Zaragoza, Departamento de Ciencias de la Tierra, Pedro Cerbuna 12, 50009 Zaragoza, Spain 3Géosciences Montpellier, CNRS and University of Montpellier (UMR5243), 34095 Montpellier, France 4Department of Geology and Andean Geothermal Center of Excellence (CEGA), Universidad de Chile, Plaza Ercilla no. 803, Santiago, Chile 5ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS) and GEMOC National Key Centre, Department of Earth and Planetary Sciences, Macquarie University, Sydney, New South Wales 2109, Australia 6Departamento de Mineralogía y Petrología and Instituto Andaluz de Ciencias de la Tierra (Universidad de Granada-CSIC), Facultad de Ciencias, Avda. Fuentenueva s/n, 18002 Granada, Spain 7Departament de Cristal·lografia, Mineralogia i Dipòsits Minerals, Facultat de Geologia, Universitat de Barcelona, Martí i Franquès s/n, 08028 Barcelona, Spain 8IDEAN-CONICET, Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Intendente Güiraldes 2160, Ciudad Universitaria, Pabellón II-1° EP, Office 29, (1428), Buenos Aires, Argentina ABSTRACT Chromite from Los Congos and Los Guanacos in the Eastern Pampean Ranges of Córdoba (Argentin- ian Central Andes) shows homogenous and exsolution textures. -
BURMESE JADE: the INSCRUTABLE GEM by Richard W
BURMESE JADE: THE INSCRUTABLE GEM By Richard W. Hughes, Olivier Galibert, George Bosshart, Fred Ward, Thet Oo, Mark Smith, Tay Thye Sun, and George E. Harlow The jadeite mines of Upper Burma (now Myanmar) occupy a privileged place in the If jade is discarded and pearls destroyed, petty thieves world of gems, as they are the principal source of top-grade material. This article, by the first will disappear, there being no valuables left to steal. foreign gemologists allowed into these impor- — From a dictionary published during the reign of tant mines in over 30 years, discusses the his- Emperor K’ang Hsi (1662–1722 AD) , as quoted by Gump, 1962 tory, location, and geology of the Myanmar jadeite deposits, and especially current mining erhaps no other gemstone has the same aura of mys- activities in the Hpakan region. Also detailed tery as Burmese jadeite. The mines’ remote jungle are the cutting, grading, and trading of location, which has been off-limits to foreigners for jadeite—in both Myanmar and China—as P well as treatments. The intent is to remove decades, is certainly a factor. Because of the monsoon rains, some of the mystery surrounding the Orient’s this area is essentially cut off from the rest of the world for most valued gem. several months of the year, and guerrilla activities have plagued the region since 1949 (Lintner, 1994). But of equal importance is that jade connoisseurship is almost strictly a Chinese phenomenon. People of the Orient have developed jade appreciation to a degree found nowhere else in the world, but this knowledge is largely locked away ABOUT THE AUTHORS in non-Roman-alphabet texts that are inaccessible to most Mr. -
Kosmochlor-Bearing Jadeite Rocks from Kenterlau-Itmurundy (Lake Balkhash, Kazakhstan)
35th IGC 2017 – Windhoek, Namibia Poster Sessions Kosmochlor-bearing jadeite rocks from Kenterlau-Itmurundy (Lake Balkhash, Kazakhstan) Leander Franz1, Michael Krzemnicki2, Kristina Ernst3, Christian de Capitani4, George E. Harlow5, Nicolai Kouznetsov6 1Mineralogisch-Petrographisches Institut, University of Basel, Switzerland, [email protected] 2SSEF Swiss Gemmological Institute, Basel, Switzerland 3ETH Zürich, Switzerland 4Mineralogisch-Petrographisches Institut, University of Basel, Switzerland 5American Museum of Natural History, New York, U.S.A 6Jade Resources, LTD, Hong Kong Petrographic, petrologic and geochemical investigations on Cr-jadeite rocks from Kenterlau-Itmurundy near Lake Balkhash (Kazakhstan) reveal ive diferent rock groups. Jadeitites show irregular, medium-grained white sections made up of decussate jadeite crystals and ine-grained sections made up of aligned Cr-jadeite. Omphacite jadeitites show a homogeneous, pale green colour with randomly oriented jadeite crystals, which are overgrown by omphacite on their rims and along fractures. Phlogopite-analcime jadeitites show decussate, white sections made up of jadeite and foliated, partially microfolded green layers and spots consisting of Cr-jadeite. Analcime and phlogopite formed late in fractures in the jadeite-rich sections. Phlogopite-omphacite jadeitites reveal an inhomogeneous mineral dis- tribution with a dark-green matrix made up of sheaf-like aggregates of Cr-omphacite and white spots of decussate prismatic jadeite crystals. Post-crystallization deformation is evident by bent and twisted pyroxenes while phlogopite formed post-tectonically on fractures and grain boundaries. Due to the extreme textural inhomogeneity, transitions between these four groups are blurred. Kosmochlor-analcime-albite-omphacite jadeitites reveal an inhomogeneous fabric with decussate, white sections, pale-green shear bands, and dark green layers.