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L. Jahnsite, Segelerite, and Robertsite, Three New Transition Metal Phosphate Species Ll. Redefinition of Overite, an Lsotype Of
American Mineralogist, Volume 59, pages 48-59, 1974 l. Jahnsite,Segelerite, and Robertsite,Three New TransitionMetal PhosphateSpecies ll. Redefinitionof Overite,an lsotypeof Segelerite Pnur BnnN Moone Thc Departmcntof the GeophysicalSciences, The Uniuersityof Chicago, Chicago,Illinois 60637 ilt. lsotypyof Robertsite,Mitridatite, and Arseniosiderite Peur BmaN Moonp With Two Chemical Analvsesbv JUN Iro Deryrtrnent of GeologicalSciences, Haraard Uniuersity, Cambridge, Massrchusetts 02 I 38 Abstract Three new species,-jahnsite, segelerite, and robertsite,-occur in moderate abundance as late stage products in corroded triphylite-heterosite-ferrisicklerite-rockbridgeite masses, associated with leucophosphite,hureaulite, collinsite, laueite, etc.Type specimensare from the Tip Top pegmatite, near Custer, South Dakota. Jahnsite, caMn2+Mgr(Hro)aFe3+z(oH)rlPC)oln,a 14.94(2),b 7.14(l), c 9.93(1)A, p 110.16(8)", P2/a, Z : 2, specific gavity 2.71, biaxial (-), 2V large, e 1.640,p 1.658,t l.6lo, occurs abundantly as striated short to long prismatic crystals, nut brown, yellow, yellow-orange to greenish-yellowin color.Formsarec{001},a{100},il2oll, jl2}ll,ft[iol],/tolll,nt110],andz{itt}. Segeierite,CaMg(HrO)rFes+(OH)[POdz, a 14.826{5),b 18.751(4),c7.30(1)A, Pcca, Z : 8, specific gaavity2.67, biaxial (-), 2Ylarge,a 1.618,p 1.6t5, z 1.650,occurs sparingly as striated yellow'green prismaticcrystals, with c[00], r{010}, nlll0l and qll2l } with perfect {010} cleavage'It is the Feg+-analogueofoverite; a restudy on type overite revealsthe spacegroup Pcca and the ideal formula CaMg(HrO)dl(OH)[POr]r. Robertsite,carMna+r(oH)o(Hro){Ponlr, a 17.36,b lg.53,c 11.30A,p 96.0o,A2/a, Z: 8, specific gravity3.l,T,cleavage[l00] good,biaxial(-) a1.775,8 *t - 1.82,2V-8o,pleochroismextreme (Y, Z = deep reddish brown; 17 : pale reddish-pink), @curs as fibrous massesand small wedge- shapedcrystals showing c[001 f , a{1@}, qt031}. -
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 -
Uraninite, Coffinite and Ningyoite from Vein-Type Uranium Deposits of the Bohemian Massif (Central European Variscan Belt)
minerals Article Uraninite, Coffinite and Ningyoite from Vein-Type Uranium Deposits of the Bohemian Massif (Central European Variscan Belt) Miloš René 1,*, ZdenˇekDolníˇcek 2, Jiˇrí Sejkora 2, Pavel Škácha 2,3 and Vladimír Šrein 4 1 Institute of Rock Structure and Mechanics, Academy of Sciences of the Czech Republic, 182 09 Prague, Czech Republic 2 Department of Mineralogy and Petrology, National Museum, 193 00 Prague, Czech Republic; [email protected] (Z.D.); [email protected] (J.S.); [email protected] (P.Š.) 3 Mining Museum Pˇríbram, 261 01 Pˇríbram, Czech Republic 4 Czech Geological Survey, 152 00 Prague, Czech Republic; [email protected] * Correspondence: [email protected]; Tel.: +420-266-009-228 Received: 26 November 2018; Accepted: 15 February 2019; Published: 19 February 2019 Abstract: Uraninite-coffinite vein-type mineralisation with significant predominance of uraninite over coffinite occurs in the Pˇríbram, Jáchymov and Horní Slavkov ore districts and the Pot ˚uˇcky, Zálesí and Pˇredboˇriceuranium deposits. These uranium deposits are hosted by faults that are mostly developed in low- to high-grade metamorphic rocks of the basement of the Bohemian Massif. Textural features and the chemical composition of uraninite, coffinite and ningyoite were studied using an electron microprobe. Collomorphic uraninite was the only primary uranium mineral in all deposits studied. The uraninites contained variable and elevated concentrations of PbO (1.5 wt %–5.4 wt %), CaO (0.7 wt %–8.3 wt %), and SiO2 (up to 10.0 wt %), whereas the contents of Th, Zr, REE and Y were usually below the detection limits of the electron microprobe. -
Tyrrellite (Cu, Co, Ni)3Se4 C 2001-2005 Mineral Data Publishing, Version 1
Tyrrellite (Cu, Co, Ni)3Se4 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Cubic. Point Group: 4/m 32/m. Rounded grains and subhedral cubes. Physical Properties: Cleavage: {001}, poor. Fracture: Conchoidal. Tenacity: Brittle. Hardness = ∼3.5 VHN = 343–368 (100 g load). D(meas.) = n.d. D(calc.) = 6.6(2) Optical Properties: Opaque. Color: Pale bronze; pale brassy bronze in reflected light. Streak: Black. Luster: Metallic. R: (400) 41.8, (420) 42.6, (440) 43.5, (460) 44.4, (480) 45.0, (500) 45.5, (520) 45.9, (540) 46.3, (560) 46.5, (580) 46.8, (600) 47.0, (620) 47.3, (640) 47.5, (660) 47.6, (680) 47.8, (700) 48.0 Cell Data: Space Group: Fm3m. a = 10.005(4) Z = 8 X-ray Powder Pattern: Ato Bay, Canada. 1.769 (10), 2.501 (9), 2.886 (7), 3.016 (6), 1.926 (6), 5.780 (4), 3.537 (4) Chemistry: (1) (2) Cu 12.7 13.7 Co 17.7 11.6 Ni 6.9 12.0 Se 62.4 62.0 Total 99.7 99.3 (1) Beaverlodge district [sic; Goldfields district], Canada; by electron microprobe, corresponding to Cu1.01Co1.52Ni0.60Se4.00. (2) Hope’s Nose, England; by electron microprobe; corresponding to Cu1.10Ni1.04Co1.00Se4.00. Mineral Group: Linnaeite group. Occurrence: With other selenides, as the youngest hydrothermal replacements and open space fillings in sheared Precambrian rocks, which also contain uraninite deposits (Goldfields district, Canada). Association: Umangite, klockmannite, clausthalite, pyrite, hematite, chalcopyrite, chalcomenite (Ato Bay, Canada); berzelianite, eucairite, crookesite, ferroselite, bukovite, kruˇtaite, athabascaite, calcite, dolomite (Petrovice deposit, Czech Republic). -
Environmental Exposure of Thallium and Potential Health Risk in an Area of High Natural Concentrations of Thallium: Southwest Guizhou, China
Environmental Exposure and Health 367 Environmental exposure of thallium and potential health risk in an area of high natural concentrations of thallium: southwest Guizhou, China T. Xiao1, L. He1,3, J. Guha2, J. Lin1 & J. Chen1 1State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, People’s Republic of China 2Sciences de la Terre, Université du Québec à Chicoutimi, Canada 3Graduate School of Chinese Academy of Sciences, Beijing, People’s Republic of China Abstract Little is known in the literature about thallium (Tl) exposure from naturally occurring Tl contamination. This paper draws attention to the potential health risk posed by high concentrations of naturally occurring Tl in the environment. The inhabitants of a rural area of southwest Guizhou Province, China, reside within a natural Tl accumulated environment resulting from the Tl-rich sulfide mineralization, and they face a severe Tl exposure in their daily lives. The daily intake 1.9 mg Tl from the consumed food crops was estimated for a local adult inhabitant of Lanmuchang. High Tl concentrations were detected in urines of the local residents. Measured urinary Tl levels are as high as 2.51-2,668 µg/L, surpassing the accepted world urine Tl level <1 mg/L for “non-exposed” humans. However, there is a positive relationship between the extent of Tl exposure from Tl in soil and crops in the immediate environment and the levels of Tl detected in urine. This study has been able to identify that the elevated urinary Tl levels are mainly attributable to Tl accumulation in locally grown vegetables acquiring Tl from natural sources in the local soils. -
Eskebornite, Two Canadian Occurrences
ESKEBORNITE,TWO CANADIAN OCCURRENCES D.C. HARRIS* am E.A.T.BURKE *r, AssrRAcr The flnt Canadian occurrenceof eskebomitefrom Martin Lake and the Eagle Groug Lake Athabaskaare4 Northern Saskatchewanis reported.Electron microprobe agalysesshow that the formula is cuFese2.The r-ray powdet difiraction pattems are identical to that of eskebornitefrom Tilkerode, Germany,the type locality, Eskeborniteocrurs as island remnantsin, and replac'edby,'u,rnangite'which occurs in pitchblendeores in t}le basa.ltof the Martin formaiion and in granitizedmafic rocls of the Eaglegroup. The mineral can be readily synthesizedat 500"e from pure elements in evacuatedsilica glasstubes, Reflectance and micro-indentationhardness in."r*u**o are given. IlvrnonucttoN Eskebomite, a copper iron selenide, was first discovered and namd by P. Ramdohr in 1949 while studying the selenide minerals from dre Tilkerode area, Harz Mountain, Germany. The mineral has also been reported from Sierra de Cacheuta and Sierra de lJmango, Argentina (Tischendorf 1960). More recentlyo other occurrences of eskebornite have been described: by Kvadek et al. (1965) in the selenide paragenesis at the slavkovice locality in the Bohemian and Moravian Highlands, czecho- slovakia; and by Agrinier et aI. (1967) in veins of pitchblende at Cha- m6anq Puy-de-D6me, France. Earley (1950) and Tischendorf (195g, 1960) made.observations on eskebornite from the Tilkerode locality, but, even today, certain data are still lacking in the characterization of eskebomitg in particular its crystal- lographic symmetry. The purpose of this paper is to record the first occurrence of eskebomite in Canada and to present electron microprobe analyses, reflectance and micro-indentation hardness measurements. GrNsRAr. -
New Mineral Names*,†
American Mineralogist, Volume 106, pages 1360–1364, 2021 New Mineral Names*,† Dmitriy I. Belakovskiy1, and Yulia Uvarova2 1Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18 korp. 2, Moscow 119071, Russia 2CSIRO Mineral Resources, ARRC, 26 Dick Perry Avenue, Kensington, Western Australia 6151, Australia In this issue This New Mineral Names has entries for 11 new species, including 7 minerals of jahnsite group: jahnsite- (NaMnMg), jahnsite-(NaMnMn), jahnsite-(CaMnZn), jahnsite-(MnMnFe), jahnsite-(MnMnMg), jahnsite- (MnMnZn), and whiteite-(MnMnMg); lasnierite, manganflurlite (with a new data for flurlite), tewite, and wumuite. Lasnierite* the LA-ICP-MS analysis, but their concentrations were below detec- B. Rondeau, B. Devouard, D. Jacob, P. Roussel, N. Stephant, C. Boulet, tion limits. The empirical formula is (Ca0.59Sr0.37)Ʃ0.96(Mg1.42Fe0.54)Ʃ1.96 V. Mollé, M. Corre, E. Fritsch, C. Ferraris, and G.C. Parodi (2019) Al0.87(P2.99Si0.01)Ʃ3.00(O11.41F0.59)Ʃ12 based on 12 (O+F) pfu. The strongest lines of the calculated powder X-ray diffraction pattern are [dcalc Å (I%calc; Lasnierite, (Ca,Sr)(Mg,Fe)2Al(PO4)3, a new phosphate accompany- ing lazulite from Mt. Ibity, Madagascar: an example of structural hkl)]: 4.421 (83; 040), 3.802 (63, 131), 3.706 (100; 022), 3.305 (99; 141), characterization from dynamic refinement of precession electron 2.890 (90; 211), 2.781 (69; 221), 2.772 (67; 061), 2.601 (97; 023). It diffraction data on submicrometer sample. European Journal of was not possible to perform powder nor single-crystal X-ray diffraction Mineralogy, 31(2), 379–388. -
The Importance of Minerals in Coal As the Hosts of Chemical Elements: a Review
The importance of minerals in coal as the hosts of chemical elements: A review Robert B. Finkelmana,b, Shifeng Daia,c,*, David Frenchd a State Key Laboratory of Coal Resources and Safe Mining, China University of Mining and Technology, China b University of Texas at Dallas, Richardson, TX 75080, USA c College of Geoscience and Survey Engineering, China University of Mining and Technology (Beijing), Beijing 100083, China d PANGEA Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, NSW 2052, Australia *, Corresponding author: [email protected]; [email protected] Abstract Coal is a complex geologic material composed mainly of organic matter and mineral matter, the latter including minerals, poorly crystalline mineraloids, and elements associated with non- mineral inorganics. Among mineral matter, minerals play the most significant role in affecting the utilization of coal, although, in low rank coals, the non-mineral elements may also be significant. Minerals in coal are often regarded as a nuisance being responsible for most of the problems arising during coal utilization, but the minerals are also seen as a potentially valuable source of critical metals and may also, in some cases, have a beneficial effect in coal gasification and liquefaction. With a few exceptions, minerals are the major hosts of the vast majority of elements present in coal. In this review paper, we list more than 200 minerals that have been identified in coal and its low temperature ash, although the validity of some of these minerals has not been confirmed. Base on chemical compositions, minerals found in coal can be classified into silicate, sulfide and selenide, phosphate, carbonate, sulfate, oxide and hydroxide, and others. -
~Ui&£R5itt! of J\Rij!Oua
Minerals and metals of increasing interest, rare and radioactive minerals Authors Moore, R.T. Rights Arizona Geological Survey. All rights reserved. Download date 06/10/2021 17:57:35 Link to Item http://hdl.handle.net/10150/629904 Vol. XXIV, No.4 October, 1953 ~ui&£r5itt! of J\rij!oua ~ul1etiu ARIZONA BUREAU OF MINES MINERALS AND METALS OF INCREASING INTEREST RARE AND RADIOACTIVE MINERALS By RICHARD T. MOORE ARIZONA BUREAU OF MINES MINERAL TECHNOLOGY SERIES No. 47 BULLETIN No. 163 THIRTY CENTS (Free to Residents of Arizona) PUBLISHED BY ~tti£ll~r5itt! of ~rh!Omt TUCSON, ARIZONA TABLE OF CONTENTS INTRODUCTION 5 Acknowledgments 5 General Features 5 BERYLLIUM 7 General Features 7 Beryllium Minerals 7 Beryl 7 Phenacite 8 Gadolinite 8 Helvite 8 Occurrence 8 Prices and Possible Buyers ,........................................ 8 LITHIUM 9 General Features 9 Lithium Minerals 9 Amblygonite 9 Spodumene 10 Lepidolite 10 Triphylite 10 Zinnwaldite 10 Occurrence 10 Prices and Possible Buyers 10 CESIUM AND RUBIDIUM 11 General Features 11 Cesium and Rubidium Minerals 11 Pollucite ..................•.........................................................................., 11 Occurrence 12 Prices and Producers 12 TITANIUM 12 General Features 12 Titanium Minerals 13 Rutile 13 Ilmenite 13 Sphene 13 Occurrence 13 Prices and Buyers 14 GALLIUM, GERMANIUM, INDIUM, AND THALLIUM 14 General Features 14 Gallium, Germanium, Indium and Thallium Minerals 15 Germanite 15 Lorandite 15 Hutchinsonite : 15 Vrbaite 15 Occurrence 15 Prices and Producers ~ 16 RHENIUM 16 -
Near-Infrared Spectroscopy of Uranyl Arsenates of the Autunite and Metaautunite Group
Near-Infrared spectroscopy of uranyl arsenates of the autunite and metaautunite group Ray L. Frost•, Onuma Carmody, Kristy L. Erickson and Matt L. Weier Inorganic Materials Research Program, School of Physical and Chemical Sciences, Queensland University of Technology, GPO Box 2434, Brisbane Queensland 4001, Australia. Frost, Ray and Carmody, Onuma and Erickson, Kristy and Weier, Matt (2005) Near- Infrared spectroscopy of uranyl arsenates of the autunite and metaautunite group. Spectrochimica Acta, Part A: Molecular and Biomolecular Spectroscopy 61(8):1923. Copyright 2005 Elsevier Note: This is the authors’ version of the work. Abstract A suite of uranyl arsenates have been analysed by Near-infrared spectroscopy. The NIR spectra of zeunerite and metazeunerite in the first HOH fundamental overtone are different and the spectra of uranyl arsenates of different origins in the 6000 to 7500 cm-1 region are different. NIR spectroscopy provides a method of determination of the hydration of uranyl arsenates and has implications for the structure of water in the interlayer. Such a conclusion is also supported by the water OH stretching region where considerable differences are observed. NIR is an excellent technique for the study of the autunite minerals and may be used to distinguish between different autunite phases such as the partially dehydrated autunites for example zeunerite and metazeunerite. Keywords: abernathyite, autunite, heinrichite, novacekite, zeunerite, metazeunerite, near-IR spectroscopy Introduction The study of uranium minerals is important for the remediation of soils, the solution of environmental problems caused by radioactive materials and the uptake of radionuclides from aqueous systems. Among the many uranium minerals are a group of minerals which are very common worldwide known as the autunite group of minerals. -
A New Mineralspeciesfromthe Tip Top Pegmatite, Custer County, South Dakota, and Its Relationship to Robertsite'
Canadian Mineralogist Vol. 27, pp. 451-455 (1989) PARAROBERTSITE, Ca2Mn~+(P04h02.3H20, A NEW MINERALSPECIESFROMTHE TIP TOP PEGMATITE, CUSTER COUNTY, SOUTH DAKOTA, AND ITS RELATIONSHIP TO ROBERTSITE' ANDREW C. ROBERTS Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario KIA OE8 B. DARKO STURMAN Departmentof Mineralogy,Royal OntarioMuseum, Toronto, OntarioM5S 2C6 PETE J. DUNN Departmentof MineralSciences,SmithsonianInstitution,Washington,D.C. 20560,U.S.A. WILLARD L. ROBERTS* South DakotaSchoolof Minesand Technology,Rapid City, South Dakota57701,U.S.A. ABSTRACT SOMMAIRE Pararobertsite is rare, occurring as thin red transparent La pararobertsite, espece rare, se presente sous forme single plates, or clusters of plates, on whitlockite at the Tip de plaquettes isolees minces et rouge transparent, ou en Top pegmatite, Custer County, South Dakota. Associated agregats de telles plaquettes, situees sur la whitlockite dans minerals are carbonate-apatite and quartz. Individual crys- la pegmatite de Tip Top, comte de Custer, Dakota du Sud. tals are tabular on {100}, up to 0.2 mm long and are less Lui sont associes apatite carbonatee et quartz. Les plaquet- than 0.02 mm in thickness. The streak is brownish red; tes, tabulaires sur {IOO}, atteignent une longueur de 0.2 luster vitreous; brittle; cleavage on {I oo} perfect; indiscer- mm et moins de 0.02 mm en epaisseur. La rayure est rouge nible fluorescence under long- or short-wave ultraviolet brunatre, et l' eclat, vitreux; cassante; clivage {100} par- light; hardness could not be determined, but the mineral fait; fluorescence non-discernable en lumiere ultra-violette apparently is very soft; D (meas.) 3.22 (4), D (calc.) 3.22 (onde courte ou longue); la durete, quoique indeterminee, (for the empirical formula) or 3.21 g/cm3 (for the ideal- semble tres faible; Dmes 3.22(4), Deale 3.22 (formule empi- ized formula). -
Thallium Mobility in Mining Wastes at the Crven Dol Locality, Allchar Deposit, North Macedonia
EGU2020-4959, updated on 25 Sep 2021 https://doi.org/10.5194/egusphere-egu2020-4959 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Thallium mobility in mining wastes at the Crven Dol locality, Allchar deposit, North Macedonia Tamara Đorđević1, Uwe Kolitsch1,2, Petr Drahota3, Magdaléna Knappová3, Juraj Majzlan4, Stefan Kiefer4, Tomáš Mikuš5, Goran Tasev6, Todor Serafimovski6, Ivan Boev6, and Blažo Boev6 1Institut für Mineralogie und Kristallographie, Universität Wien, Althanstr. 14, A-1090 Wien, Austria 2Mineralogisch-Petrographische Abteilung, Naturhistorisches Museum, Burgring 7, A-1010 Wien, Austria 3Institute of Geochemistry, Mineralogy and Mineral Resources, Faculty of Science, Charles University, Albertov 6, 128 43 Prague 2, Czech Republic 4Institute of Geosciences, Department of Mineralogy, Friedrich-Schiller-Universität, Carl-Zeiss-Promenade 10, 07745 Jena, Germany 5Earth Science Institute, Slovak Academy of Sciences, Geological Division, Ďumbierska 1, 974 01 Banská Bystrica, Slovakia 6Department of Mineral Deposits, Faculty of Natural Sciences, University “Goce Delčev”-Štip, Goce Delčev 89, 2000 Štip, North Macedonia In order to better understand the environmental behaviour of thallium, we have chosen the abandoned As–Sb–Tl–Au Allchar deposit (North Macedonia) with unique mineral composition and high thallium grades of the ore. We used pore water analyses, selective extractions, single-crystal and powder X-ray diffraction (PXRD), SEM-EDS, electron microprobe analysis (EMPA), and Raman spectroscopy to determine the distribution and speciation of thallium in waste dump material at the Tl-rich Crven Dol locality in the northern part of the Allchar deposit. PXRD studies showed that the various solid waste samples are comprised mostly of carbonates (dolomite and calcite), gypsum, quartz, muscovite, kaolinite-group minerals followed by orpiment, realgar, pyrite, marcasite, lorandite, and various iron and calcium arsenates and iron (hydro)oxides, both amorphous and crystalline.