The Crystal Structure of Triploidite and Its Relation to the Structures of Other Minerals of the Triplite-Triploidite Group
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The Krásno Sn-W Ore District Near Horní Slavkov: Mining History, Geological and Mineralogical Characteristics
Journal of the Czech Geological Society 51/12(2006) 3 The Krásno Sn-W ore district near Horní Slavkov: mining history, geological and mineralogical characteristics Sn-W rudní revír Krásno u Horního Slavkova historie tìby, geologická a mineralogická charakteristika (47 figs, 1 tab) PAVEL BERAN1 JIØÍ SEJKORA2 1 Regional Museum Sokolov, Zámecká 1, Sokolov, CZ-356 00, Czech Republic 2 Department of Mineralogy and Petrology, National Museum, Václavské nám. 68, Prague 1, CZ-115 79, Czech Republic The tin-tungsten Krásno ore district near Horní Slavkov (Slavkovský les area, western Bohemia) belongs to the most important areas of ancient mining in the Czech Republic. The exceptionally rich and variable mineral associations, and the high number of mineral species, make this area one of the most remarkable mineralogical localities on a worldwide scale. The present paper reviews the data on geological setting of the ore district, individual ore deposits and mining history. Horní Slavkov and Krásno were known as a rich source of exquisite quality mineral specimens stored in numerous museum collections throughout Europe. The old museum specimens are often known under the German locality names of Schlaggenwald (= Horní Slavkov) and Schönfeld (=Krásno). The megascopic properties and paragenetic position of selected mineral classics are reviewed which include arsenopyrite, fluorapatite, fluorite, hübnerite, chalcopyrite, carpholite, cassiterite, quartz, molybdenite, rhodochrosite, sphalerite, topaz and scheelite. Key words: Sn-W ores; tin-tungsten mineralization; mining history; ore geology; mineralogy; Slavkovský les; Krásno, Horní Slavkov ore district; Czech Republic. Introduction valleys dissected parts of the area. In the ore district area, the detailed surface morphology is modified by large de- In the mining history of Central Europe, Bohemia and pressions caused by the collapse of old underground Moravia are known as important source of gold, silver, workings and by extensive dumps. -
Sarkinite Mn (Aso4)(OH)
2+ Sarkinite Mn2 (AsO4)(OH) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. Crystals typically thick tabular {100}, elongated, to 4 mm, short prismatic, or tabular along [010]. May be crudely spherical, granular massive. Physical Properties: Cleavage: On {100}, distinct. Fracture: Subconchoidal to uneven. Hardness = 4–5 D(meas.) = 4.08–4.18 D(calc.) = 4.20 Optical Properties: Semitransparent. Color: Flesh-red to dark blood-red, rose-red, orange, orange-brown, brown, reddish yellow to yellow; pale rose to yellow in transmitted light. Streak: Rose-red to yellow. Luster: Greasy. Optical Class: Biaxial (–). Pleochroism: Weak. Orientation: Y = b; X ∧ c = –54◦. Dispersion: r< v. Absorption: X > Z > Y. α = 1.790–1.793 β = 1.794–1.807 γ = 1.798–1.809 2V(meas.) = 83◦ Cell Data: Space Group: P 21/a. a = 12.779(2) b = 13.596(2) c = 10.208(2) β = 108◦530 Z=16 X-ray Powder Pattern: Pajsberg [Harstigen mine, near Persberg], Sweden. 3.18 (10), 3.04 (10), 3.29 (9), 3.48 (8), 2.90 (7), 2.65 (6), 6.0 (3) Chemistry: (1) (2) (3) (1) (2) (3) P2O5 0.21 ZnO 0.15 As2O5 41.60 44.09 43.23 PbO 0.25 CO2 0.76 MgO 0.98 0.19 FeO 0.13 0.02 CaO 1.40 0.29 MnO 51.60 51.77 53.38 H2O 3.06 [3.40] 3.39 CuO 0.01 insol. 0.38 Total 100.37 [99.92] 100.00 (1) Pajsberg [Harstigen mine, near Persberg], Sweden. -
1 CRYSTAL CHEMISTRY of SELECTED Sb, As and P MINERALS
Crystal Chemistry of Selected Sb, As, and P Minerals Item Type text; Electronic Dissertation Authors Origlieri, Marcus Jason Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 07/10/2021 10:49:41 Link to Item http://hdl.handle.net/10150/194240 1 CRYSTAL CHEMISTRY OF SELECTED Sb, As AND P MINERALS by Marcus Jason Origlieri ___________________________________________ A Dissertation Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY In the Graduate College THE UNIVERSITY OF ARIZONA 2005 2 THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE As members of the Dissertation Committee, we certify that we have read the dissertation prepared by Marcus Jason Origlieri entitled Crystal Chemistry of Selected Sb, As, and P Minerals and recommend that it be accepted as fulfilling the dissertation requirement for the Degree of Doctor of Philosophy _______________________________________________________________________ Date: November 15, 2005 Robert T. Downs _______________________________________________________________________ Date: November 15, 2005 M. Bonner Denton _______________________________________________________________________ Date: November 15, 2005 Mihai N. Ducea _______________________________________________________________________ Date: November 15, 2005 Charles T. Prewitt Final approval and acceptance of this dissertation is contingent upon the candidate’s submission of the final copies of the dissertation to the Graduate College. I hereby certify that I have read this dissertation prepared under my direction and recommend that it be accepted as fulfilling the dissertation requirement. -
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 -
Mineralogy and Geology of the \Vkgnerite Occurrence Co Santa Fe Mountain, Front Range, Cobrado
Mineralogy and Geology of the \Vkgnerite Occurrence co Santa Fe Mountain, Front Range, Cobrado GEOLOGICAL SURVEY PROFESSIONAL PAPER 955 Mineralogy and Geology of the Wignerite Occurance on Santa Fe Mountain, Front Range, Colorado By DOUGLAS M. SHERIDAN, SHERMAN P. MARSH, MARY E. MROSE, and RICHARD B. TAYLOR GEOLOGICAL SURVEY PROFESSIONAL PAPER 955 A detailed mineralogic study of wagnerite, a rare phosphate mineral occurring in the report area in Precambrian gneiss; this is the first recorded occurrence of wagnerite in the United States UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Main entry under title: Mineralogy and geology of the wagnerite occurrence on Santa Fe Mountain, Front Range, Colorado. (Geological Survey Professional Paper 955) Includes bibliographical references. 1. Wagnerite Colorado Santa Fe Mountain. 2. Geology Colorado Santa Fe Mountain. I. Sheridan, Douglas M., 1921- II. Series: United States Geological Survey Professional Paper 955. QE391.W3M56 549'.72 76-10335 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, B.C. 20402 Stock Number 024-001-02844-1 CONTENTS Page Metric-English equivalents .............................. Descriptive mineralogy Continued Page Abstract............................................................ 1 Wagnerite............................................... 5 Introduction.................................................... -
NEW MINERALS It Is Proposed Hereafter to Indicate In.A General Way the Classification of All New Minerals Recoided in This Department
JOURNAL MINERALOGICAL SOCIETY OF AMENICA 63 Dr. Kunz then spoke of the various city localities and the minerals found therein. He stated that the East Side, from 37 to 110 St., probably afforded the most specimens. The various tunnels and their minerals were spoken of. Capt. Miller called attention to the fine collection of Brooklyn Drift Minerals and Rocks in the collection of the Long Island Historical Society. Ife abo mentioned the occurrence of monazite and xenotime crystals, on the Speedway,Harlem River. Dr. Kunz emphasizedthe irnportance of complete records being kept of all finds. Tnou,q,s L Mrr,r,nn, SecretaryPro, Tem. NEW MINERALS It is proposed hereafter to indicate in.a general way the classification of all new minerals recoided in this department. Subdivision will be first into "families," of which nine may be recognized,as listed in the January number (Am. Min.6 (1), 12,1921). Eachfamilywillbe separatedinto "subfamilies " based on special features of composition. This arrangement is tentative and open to modification, and criticism of it will be welcome, [Eo.] FAMILY 2. SULFIDES, ETC. SosreMrr,v 3. Doust,u suLFrDEs oF METALSAND sEMr-METAr,s. I'LTRABASITE V. Rosrcxf and J. Srnnse-Btinu. Ultrabasit, ein neues Mineral aus Freiberg in Sachsen. (Ultrabasite, a new mineral from Freiberg, Saxony). Rozpr.Eeslcd Ako,il. Prag,25, No. 45, 1916;Z. Krgst. Min., 55,43H39, 1920, Neun: From its extremely basic chemical composition. Pnrsrcar, Pnopnnrrus Color black, somewhat grayish; luster metallic; streak black; cleavage none; fracture scaly, with somewhat greasy luster on the surface. H. : 5; sp. gr. -
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. -
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. -
Geology and Beryl Deposits of the Peerless Pegmatite Pennington County South Dakota
Geology and Beryl Deposits of the Peerless Pegmatite Pennington County South Dakota GEOLOGICAL SURVEY PROFESSIONAL PAPER 297-A This report concerns work done partly on behalj of the U. S. Atomic Energy Commission and is published with the permission of the , » Commission Geology and Beryl Deposits of the Peerless Pegmatite Pennington County South Dakota By DOUGLAS M. SHERllDAN, HAL G. STEPHENS, MORTIMER H. STAATZ and JAMES J. NORTON PEGMATITES AND OTHER PRECAMBRIAN ROCKS IN THE SOUTHERN BLACK HILLS GEOLOGICAL SURVEY PROFESSIONAL PAPER 297-A This report concerns work done partly on behalf of the U. S. Atomic Energy Commission and is published with the permission of the Commission UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1957 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1.50 (paper cover) CONTENTS Page Page Abstract.__________________________________________ 1 Geology Continued Introduction _______________________________________ 1 Peerless pegmatite Continued Location_____________________________________ 1 Chemical composition......____________ 17 History and production________________________ 2 Origin________ ____________________ _. 18 Past and present investigations.__________________ 3 Mineral deposits_____________________________ 21 Acknowledgments__________________________ 4 Mica__ _________ _________________________ 21 Mine workings _____________________________________ -
A New Mineral from Mn Ores of the Ushkatyn-III Deposit, 3 Central Kazakhstan and Metamorphic Rocks of the Wanni Glacier, Switzerland 4 5 Oleg S
1 Revision 1 2 Gasparite-(La), La(AsO4), a new mineral from Mn ores of the Ushkatyn-III deposit, 3 Central Kazakhstan and metamorphic rocks of the Wanni glacier, Switzerland 4 5 Oleg S. Vereshchagin*1, Sergey N. Britvin1,6, Elena N. Perova1, Aleksey I. Brusnitsyn1, 6 Yury S. Polekhovsky1, Vladimir V. Shilovskikh2, Vladimir N. Bocharov2, 7 Ate van der Burgt3, Stéphane Cuchet4, and Nicolas Meisser5 8 1Institute of Earth Sciences, St. Petersburg State University, University Emb. 7/9, 199034 St. 9 Petersburg, Russia 10 2Geomodel Centre, St. Petersburg State University, Uliyanovskaya St. 1, 198504 St. 11 Petersburg, Russia 12 3Geertjesweg 39, NL-6706EB Wageningen, The Netherlands 13 4ch. des Bruyeres 14, CH-1007 Lausanne, Switzerland 14 5Musée cantonal de géologie, Université de Lausanne, Anthropole, 1015 Lausanne, 15 Switzerland 16 6Kola Science Center, Russian Academy of Sciences, Fersman Str. 14, 184209 Apatity, 17 Murmansk Region, Russia 18 *E-mail: [email protected] 19 1 20 Abstract 21 Gasparite-(La), La(AsO4), is a new mineral (IMA 2018-079) from Mn ores of the Ushkatyn- 22 III deposit, Central Kazakhstan (type locality) and from alpine fissures in metamorphic rocks 23 of the Wanni glacier, Binn Valley, Switzerland (co-type locality). Gasparite-(La) is named 24 for its dominant lanthanide, according to current nomenclature of rare-earth minerals. 25 Occurrence and parageneses in both localities is distinct: minute isometric grains up to 15 µm 26 in size, associated with fridelite, jacobsite, pennantite, manganhumite series minerals 27 (alleghanyite, sonolite), sarkinite, tilasite and retzian-(La) are typically embedded into 28 calcite-rhodochrosite veinlets (Ushkatyn-III deposit), versus elongated crystals up to 2 mm in 29 size in classical alpine fissures in two-mica gneiss without indicative associated minerals 30 (Wanni glacier). -
Redetermination of Eveite, Mn2aso4 (OH), Based on Single-Crystal X-Ray
inorganic compounds Acta Crystallographica Section E Experimental Structure Reports Crystal data Online ˚ 3 Mn2AsO4(OH) V = 469.33 (15) A ISSN 1600-5368 Mr = 265.81 Z =4 Orthorhombic, Pnnm Mo K radiation a = 8.5478 (16) A˚ = 12.29 mmÀ1 Redetermination of eveite, b = 8.7207 (16) A˚ T = 293 K c = 6.2961 (12) A˚ 0.05 Â 0.05 Â 0.04 mm Mn2AsO4(OH), based on single-crystal X-ray diffraction data Data collection Bruker APEXII CCD area-detector 3315 measured reflections diffractometer 911 independent reflections a b c Yongbo W. Yang, * Ryan A. Stevenson, Alesha M. Siegel Absorption correction: multi-scan 849 reflections with I >2(I) and Gordon W. Downsd (SADABS; Sheldrick, 2005) Rint = 0.015 Tmin = 0.579, Tmax = 0.639 aDepartment of Chemistry and Biochemistry, University of Arizona, 1306 Refinement E. University Blvd, Tucson, Arizona 85721-0041, USA, bDepartment of 2 2 Geosciences, University of Arizona, 1040 E. 4th Street, Tucson, Arizona R[F >2(F )] = 0.021 49 parameters 2 85721-0077, USA, cDepartment of Molecular and Cellular Biology, University of wR(F ) = 0.055 All H-atom parameters refined ˚ À3 Arizona, 1007 E. Lowell Street, Tucson, Arizona 85721-0106, USA, and dUniversity S = 1.09 Ámax = 1.28 e A 911 reflections Á = À1.15 e A˚ À3 High School, 421 N. Arcadia Avenue, Tucson, Arizona 85711-3032, USA min Correspondence e-mail: [email protected] Received 16 October 2011; accepted 24 October 2011 Table 1 Hydrogen-bond geometry (A˚ , ). Key indicators: single-crystal X-ray study; T = 293 K; mean (As–O) = 0.002 A˚; R factor = 0.021; wR factor = 0.055; data-to-parameter ratio = 18.6. -
Mineral Index
Mineral Index Abhurite T.73, T.355 Anandite-Zlvl, T.116, T.455 Actinolite T.115, T.475 Anandite-20r T.116, T.45S Adamite T.73,T.405, T.60S Ancylite-(Ce) T.74,T.35S Adelite T.115, T.40S Andalusite (VoU, T.52,T.22S), T.27S, T.60S Aegirine T.73, T.30S Andesine (VoU, T.58, T.22S), T.41S Aenigmatite T.115, T.46S Andorite T.74, T.31S Aerugite (VoU, T.64, T.22S), T.34S Andradite T.74, T.36S Agrellite T.115, T.47S Andremeyerite T.116, T.41S Aikinite T.73,T.27S, T.60S Andrewsite T.116, T.465 Akatoreite T.73, T.54S, T.615 Angelellite T.74,T.59S Akermanite T.73, T.33S Ankerite T.74,T.305 Aktashite T.73, T.36S Annite T.146, T.44S Albite T.73,T.30S, T.60S Anorthite T.74,T.415 Aleksite T.73, T.35S Anorthoclase T.74,T.30S, T.60S Alforsite T.73, T.325 Anthoinite T.74, T.31S Allactite T.73, T.38S Anthophyllite T.74, T.47S, T.61S Allanite-(Ce) T.146, T.51S Antigorite T.74,T.375, 60S Allanite-(La) T.115, T.44S Antlerite T.74, T.32S, T.60S Allanite-(Y) T.146, T.51S Apatite T.75, T.32S, T.60S Alleghanyite T.73, T.36S Aphthitalite T.75,T.42S, T.60 Allophane T.115, T.59S Apuanite T.75,T.34S Alluaudite T.115, T.45S Archerite T.75,T.31S Almandine T.73, T.36S Arctite T.146, T.53S Alstonite T.73,T.315 Arcubisite T.75, T.31S Althausite T.73,T.40S Ardaite T.75,T.39S Alumino-barroisite T.166, T.57S Ardennite T.166, T.55S Alumino-ferra-hornblende T.166, T.57S Arfvedsonite T.146, T.55S, T.61S Alumino-katophorite T.166, T.57S Argentojarosite T.116, T.45S Alumino-magnesio-hornblende T.159,T.555 Argentotennantite T.75,T.47S Alumino-taramite T.166, T.57S Argyrodite (VoU,