Shigaite Namn Al3(SO4)
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Metamorphism of Sedimentary Manganese Deposits
Acta Mineralogica-Petrographica, Szeged, XX/2, 325—336, 1972. METAMORPHISM OF SEDIMENTARY MANGANESE DEPOSITS SUPRIYA ROY ABSTRACT: Metamorphosed sedimentary deposits of manganese occur extensively in India, Brazil, U. S. A., Australia, New Zealand, U. S. S. R., West and South West Africa, Madagascar and Japan. Different mineral-assemblages have been recorded from these deposits which may be classi- fied into oxide, carbonate, silicate and silicate-carbonate formations. The oxide formations are represented by lower oxides (braunite, bixbyite, hollandite, hausmannite, jacobsite, vredenburgite •etc.), the carbonate formations by rhodochrosite, kutnahorite, manganoan calcite etc., the silicate formations by spessartite, rhodonite, manganiferous amphiboles and pyroxenes, manganophyllite, piedmontite etc. and the silicate-carbonate formations by rhodochrosite, rhodonite, tephroite, spessartite etc. Pétrographie and phase-equilibia data indicate that the original bulk composition in the sediments, the reactions during metamorphism (contact and regional and the variations and effect of 02, C02, etc. with rise of temperature, control the mineralogy of the metamorphosed manga- nese formations. The general trend of formation and transformation of mineral phases in oxide, carbonate, silicate and silicate-carbonate formations during regional and contact metamorphism has, thus, been established. Sedimentary manganese formations, later modified by regional or contact metamorphism, have been reported from different parts of the world. The most important among such deposits occur in India, Brazil, U.S.A., U.S.S.R., Ghana, South and South West Africa, Madagascar, Australia, New Zealand, Great Britain, Japan etc. An attempt will be made to summarize the pertinent data on these metamorphosed sedimentary formations so as to establish the role of original bulk composition of the sediments, transformation and reaction of phases at ele- vated temperature and varying oxygen and carbon dioxide fugacities in determin- ing the mineral assemblages in these deposits. -
Speciation of Manganese in a Synthetic Recycling Slag Relevant for Lithium Recycling from Lithium-Ion Batteries
metals Article Speciation of Manganese in a Synthetic Recycling Slag Relevant for Lithium Recycling from Lithium-Ion Batteries Alena Wittkowski 1, Thomas Schirmer 2, Hao Qiu 3 , Daniel Goldmann 3 and Ursula E. A. Fittschen 1,* 1 Institute of Inorganic and Analytical Chemistry, Clausthal University of Technology, Arnold-Sommerfeld Str. 4, 38678 Clausthal-Zellerfeld, Germany; [email protected] 2 Department of Mineralogy, Geochemistry, Salt Deposits, Institute of Disposal Research, Clausthal University of Technology, Adolph-Roemer-Str. 2A, 38678 Clausthal-Zellerfeld, Germany; [email protected] 3 Department of Mineral and Waste Processing, Institute of Mineral and Waste Processing, Waste Disposal and Geomechanics, Clausthal University of Technology, Walther-Nernst-Str. 9, 38678 Clausthal-Zellerfeld, Germany; [email protected] (H.Q.); [email protected] (D.G.) * Correspondence: ursula.fi[email protected]; Tel.: +49-5323-722205 Abstract: Lithium aluminum oxide has previously been identified to be a suitable compound to recover lithium (Li) from Li-ion battery recycling slags. Its formation is hampered in the presence of high concentrations of manganese (9 wt.% MnO2). In this study, mock-up slags of the system Li2O-CaO-SiO2-Al2O3-MgO-MnOx with up to 17 mol% MnO2-content were prepared. The man- ganese (Mn)-bearing phases were characterized with inductively coupled plasma optical emission spectrometry (ICP-OES), X-ray diffraction (XRD), electron probe microanalysis (EPMA), and X-ray absorption near edge structure analysis (XANES). The XRD results confirm the decrease of LiAlO2 phases from Mn-poor slags (7 mol% MnO2) to Mn-rich slags (17 mol% MnO2). -
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. -
Compositional Characteristics of Kinoshitatite from the Sausar Group
American Mineralogist, Volume 74, pages 200-202, 1989 Compositionalcharacteristics of kinoshitatite from the SausarGroup, India SoNrN,q.rHD,c.scuprA., Slun Crr,cxRAnonrr, Puul.r SnNcurra, P. K. BnarrAcHARyA! H. BlNrn"rnn Centre of Advanced Study in Economic Geology, Department of Geological Sciences,Jadavpur University, Calcutta-700 032, India M. Furuoxe Department of Geology, Kyushu University, Fukuoka, Japan Anstnlcr Ba-rich and Ba-poor micas with varying Mn and Mg content in octahedralsites coexist in isolated pockets in braunite-bixbyite-hausmanniteores that have been invaded by late silicic pegmatite and carbonateveins in the SausarGroup, India. The micas are secondary in nature and are pseudomorphsafter carbonatesand alkali feldspars.One of the micas approachesclosely synthetic end-memberkinoshitalite, BaMgrAlrSirO,o(OH)..The present study shows a complete solid solution between the K (phlogopite) and Ba (kinoshitalite) end-members.Compositional diversities in these micas are attributable to the different minerals that the micas replaced. INlnolucrroN lites. Micas havedeveloped in manganeseoxide-rich rocks Krnoshitalite, BaMg.AlrSirOr0(OH)r, was defined by wherethe latter have beeninvaded by late silicic pegmatite Yoshii et al. (1973a)as the Ba and Mg trioctahedralbrit- and carbonateveins. In thesepockets, the manganeseox- tle mica. As an end-member, it is known only as a syn- ide-rich rocks exhibit the following mineral assemblage: thetic phase obtained hydrothermally at 600 "C and 2 braunite * hausmannite + bixbyite * Ba-bearingmica kbar (Frondel and Ito, 1967). Naturally occurring ki- + alkali feldspar + hematite * calcite + dolomite + noshitalite has been reported with considerableamounts qtrartz. The oxides collectively account for over 800/oof of K and Mn (Yoshii et al., l9l3b; Yoshii and Maeda, the rock. -
The Picking Table Volume 27, No. 1 – Spring 1986
TABLE JOURNAL of the FRANKLIN-OGDENSBURG MINERALOGICAL SOCIETY, INC. SPRING. 1986 VOLUME 27, NO.l The contents of The Picking Table are licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. F.QM.S. Notes prise a spectacular fluorescent display. For PRESIDENT'S MESSAGE years the Gerstmann Mineral Museum has displayed the collection for the delight and With the melting of the snow, the rocks of education of amateur and professional mineralo- the Buckwheat Dump emerge from their white gists alike. The Franklin Mineral Museum mantle, and the seismic tremors rumble through is most grateful to Arthur and Harriet Mitteldorf the souls of the collector community. Whatever for this most generous donation and to Ewald Spring may mean to the average mortal, to Gerstmann for its accumulation and for his FOMS members it brings a special appeal to sponsorship of the Franklin Mineral Museum dig in the dirt, not to plant, but to explore as the recipient. Transfer of the collection again the crystalline mysteries of Nature. will be effected as soon as suitable space is available to house it. Let us not lose sight of the fact that we are a community, however widespread, dedicated JLB to a great common interest and purpose: the expansion and preservation of knowledge about the world's most remarkable mineral location. ABOUT THE COVER SKETCH Like all great enterprises, this demands the efforts and participation of many. To the Located Sphalerite Occurrences—Franklin Mine extent that we share our knowledge, our time, and our interest with each other and the world, It is suggested that you refer to this hand Franklin lives. -
MINERALS and MINERAL VARIETIES from METAMORPHOSED Mn DEPOSITS of BISTRITA MOUNTAINS, ROMANIA
Acta Mineralogica-Petrographica, Abstract Series 1, Szeged, 2003 MINERALS AND MINERAL VARIETIES FROM METAMORPHOSED Mn DEPOSITS OF BISTRITA MOUNTAINS, ROMANIA HÎRTOPANU, P.1 & SCOTT, P.2 1 Geological Institute of Romania, Caransebeş 1, RO-78344 Bucharest, Romania. E-mail: [email protected] 2 Camborne School of Mines, Redruth, Cornwall, United Kingdom. The Bistrita Mountains belong to the Crystalline Meso- mation of some amphiboles and some pyroxenes into other zoic Zone of the East Carpathians, which consists of super- phases, there are drastical transformations of pyroxenes into posed Variscan and Alpine Nappes, overthrusted eastwards pyroxenoids (johannsenite into rhodonite), pyroxenoids into over the Flysch Zone. The manganese ore is contained by pyroxenoids (pyroxmangite into rhodonite), pyroxmangite Tulghes Group (Tg2 level) of the Variscan Putna Nappe, into manganogrunerite, garnets into garnets (spessartine- situated over the Pietrosu Bistritei Nappe and supporting the calderite into spessartine, spessartine into anisotropic spes- thrusting of the Rebra Nappe. All these Variscan nappes sartine-andradite-grossular), calderite into pyroxmangite- constitute the Alpine Sub-Bucovinian Nappe localised be- magnetite, etc. are the best evidences of continuous variation tween Alpine Infrabucovinian Nappe in the East and the of formation conditions. Alpine Bucovinian Nappe in the West. The Mn ore have a predominant carbonate rather than The mineralogy of Mn metamorphosed deposits from silicate mineralogical composition, which means a great CO2 Bistrita Mts. includes 328 minerals and mineral varieties. fluid control in the carbonation and dehydration processes They may count among the mineralogically the most com- along the many stages of the whole history of the ore and the plex deposits of the world. -
Thirty-Fourth List of New Mineral Names
MINERALOGICAL MAGAZINE, DECEMBER 1986, VOL. 50, PP. 741-61 Thirty-fourth list of new mineral names E. E. FEJER Department of Mineralogy, British Museum (Natural History), Cromwell Road, London SW7 5BD THE present list contains 181 entries. Of these 148 are Alacranite. V. I. Popova, V. A. Popov, A. Clark, valid species, most of which have been approved by the V. O. Polyakov, and S. E. Borisovskii, 1986. Zap. IMA Commission on New Minerals and Mineral Names, 115, 360. First found at Alacran, Pampa Larga, 17 are misspellings or erroneous transliterations, 9 are Chile by A. H. Clark in 1970 (rejected by IMA names published without IMA approval, 4 are variety because of insufficient data), then in 1980 at the names, 2 are spelling corrections, and one is a name applied to gem material. As in previous lists, contractions caldera of Uzon volcano, Kamchatka, USSR, as are used for the names of frequently cited journals and yellowish orange equant crystals up to 0.5 ram, other publications are abbreviated in italic. sometimes flattened on {100} with {100}, {111}, {ill}, and {110} faces, adamantine to greasy Abhurite. J. J. Matzko, H. T. Evans Jr., M. E. Mrose, lustre, poor {100} cleavage, brittle, H 1 Mono- and P. Aruscavage, 1985. C.M. 23, 233. At a clinic, P2/c, a 9.89(2), b 9.73(2), c 9.13(1) A, depth c.35 m, in an arm of the Red Sea, known as fl 101.84(5) ~ Z = 2; Dobs. 3.43(5), D~alr 3.43; Sharm Abhur, c.30 km north of Jiddah, Saudi reflectances and microhardness given. -
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. -
Kinoshitalite (Ba,K)(Mg,Mn,Al)3Si2al2o10(OH)2
Kinoshitalite (Ba; K)(Mg; Mn; Al)3Si2Al2O10(OH)2 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Monoclinic. Point Group: 2=m: Forms small scales, < 1 mm. Physical Properties: Cleavage: 001 , perfect. Tenacity: Brittle. Hardness = 2.5{3 D(meas.) = 3.30 D(calc.) = 3.33 f g Optical Properties: Semitransparent. Color: Yellow-brown to colorless; light yellow to colorless in thin section. Luster: Vitreous. Optical Class: Biaxial ({). Pleochroism: X = very light yellow to light yellow; Y = Z = light yellow with brownish tinge. Absorption: Y Z > X. ® = 1.619 ¯ = 1.628{1.633 ° = 1.635 ' 2V(meas.) = 23± Cell Data: Space Group: C2=m: a = 5.345(3) b = 9.250(4) c = 10.256(8) ¯ = 99:99(6)± Z = 2 X-ray Powder Pattern: Noda-Tamagawa mine, Japan. 3.37 (100), 2.52 (55), 2.020 (55), 5.05 (50), 10.1 (45), 1.684 (15), 3.16 (5) Chemistry: (1) (2) (1) (2) SiO2 24.58 23.43 BaO 17.85 27.60 TiO2 0.16 Na2O 0.68 0.11 Al2O3 22.06 19.25 K2O 3.30 0.24 Fe2O3 0.71 1.87 F 0.21 + Mn2O3 3.24 H2O 2.90 FeO 0.04 H2O¡ 0.20 MnO 7.38 2.62 H2O 3.50 MgO 16.60 21.95 O = F 0.09 ¡ 2 CaO 0.05 0.05 Total 99.87 100.62 2+ (1) Noda-Tamagawa mine, Japan; corresponds to (Ba0:58K0:35Na0:11Ca0:01)§=1:05(Mg2:06Mn0:52 3+ 3+ Al0:22Mn0:21Fe0:04Ti0:01)§=3:06Si2:05Al1:94O10[(OH)1:62O0:33F0:06]§=2:01: (2) Netra, India; by electron microprobe, total Fe as Fe2O3; corresponding to (Ba0:93K0:03Na0:02Ca0:01)§=0:99 (Mg2:80Mn0:19Fe0:08)§=3:07Si2:01(Al1:94Fe0:05)§=1:99O10(OH)2: Polymorphism & Series: 1M, 2M1 polytypes. -
Aspects of the Petrology, Mineralogy, and Geochemistry of the Granitic Rocks Associated with Questa Caldera, Northern New Mexico
DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Aspects of the Petrology, Mineralogy, and Geochemistry of the Granitic Rocks Associated with Questa Caldera, Northern New Mexico By Brigitte Dillet and Gerald K. Czamanske Open-file Report 87-258 lU.S. Geological Survey, 345 Middlefield Rd., Menlo Park, California. This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards (and stratigraphic nomenclature). (Any use of trade names is for descriptive purposes only and does not imply endorsement by the USGS.) Aspects of the Petrology, Mineralogy, and Geochemistry of the Granitic Rocks Associated with Questa Caldera, Northern New Mexico By Brigitte Dillet and Gerald K. Czamanske, U.S. Geological Survey This report consists largely of the Ph.D. thesis prepared by Brigitte Dillet and defended at the University of Clermont-Ferrand, France, in February, 1987. From December, 1983 through December, 1985 Ms. Dillet was supported by a grant from the French Government to carry out this thesis study at the offices of the U.S. Geological Survey in Menlo Park, California, under the guidance of Gerald Czamanske. Expenses for field work and part of 1986 were contributed by the U.S. Geological Survey as part of a comprehensive study of the volcanic and plutonic rocks associated with Questa caldera Appendices B through L have been added to the thesis to provide accurate sample locations, supplemental major- and minor-element data, and electron microprobe analyses obtained by G.K.C. for allanite, apatite, chevkinite, feldspars, and sphene in the Questa granitoids. NOTES: 1. Because early pagination is used in the thesis, pages 8, 9, ^, 3P, 179, and 185 do not exist. -
Gatehouseite Mn (PO4)2(OH)4
2+ Gatehouseite Mn5 (PO4)2(OH)4 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 222. As bladelike crystals, with prominent {001}, {110}, {102}, elongated along [010], to 100 µm, in radiating to divergent groups and overgrowths on arsenoclasite. Twinning: On {001}, contact twins. Physical Properties: Cleavage: On {010}, distinct. Fracture: Splintery. Hardness = ∼4 D(meas.) = n.d. D(calc.) = 3.74 Optical Properties: Transparent. Color: Pale brownish orange to yellow or pale yellow. Streak: Pale yellow. Luster: Adamantine. Optical Class: Biaxial. Pleochroism: Distinct; brown to nearly colorless. Orientation: Parallel extinction; length-slow. α = 1.74(1) β = n.d. γ = 1.76(1) 2V(meas.) = n.d. Cell Data: Space Group: P 212121 (probable). a = 9.097(2) b = 5.693(2) c = 18.002(10) Z=4 X-ray Powder Pattern: Iron Monarch quarry, Australia. 2.90 (100), 2.702 (80), 2.853 (70), 2.802 (50), 2.022 (15), 1.608 (15), 4.483 (10) Chemistry: (1) (2) (3) SO3 0.10 P2O5 22.18 23.05 26.65 As2O5 3.58 3.32 V2O5 0.38 Al2O3 0.10 FeO 0.19 0.32 MnO 64.42 63.34 66.59 CuO 0.03 0.04 ZnO 0.03 PbO 0.05 0.05 H2O [6.44] [6.43] 6.76 Total [97.40] [96.65] 100.00 (1) Iron Monarch quarry, Australia; by electron microprobe, total Mn as MnO, total Fe as FeO, H2O calculated for 4(OH); corresponds to Mn5.09Fe0.01Al0.01[(P0.87As0.08V0.01)Σ=0.96O4]2(OH)4.