Barytocalcite Baca(CO3)2 C 2001-2005 Mineral Data Publishing, Version 1
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Download PDF About Minerals Sorted by Mineral Name
MINERALS SORTED BY NAME Here is an alphabetical list of minerals discussed on this site. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). APATITE Crystal system: hexagonal. Fracture: conchoidal. Color: red, brown, white. Hardness: 5.0. Luster: opaque or semitransparent. Specific gravity: 3.1. Apatite, also called cellophane, occurs in peridotites in eastern and western Kentucky. A microcrystalline variety of collophane found in northern Woodford County is dark reddish brown, porous, and occurs in phosphatic beds, lenses, and nodules in the Tanglewood Member of the Lexington Limestone. Some fossils in the Tanglewood Member are coated with phosphate. Beds are generally very thin, but occasionally several feet thick. The Woodford County phosphate beds were mined during the early 1900s near Wallace, Ky. BARITE Crystal system: orthorhombic. Cleavage: often in groups of platy or tabular crystals. Color: usually white, but may be light shades of blue, brown, yellow, or red. Hardness: 3.0 to 3.5. Streak: white. Luster: vitreous to pearly. Specific gravity: 4.5. Tenacity: brittle. Uses: in heavy muds in oil-well drilling, to increase brilliance in the glass-making industry, as filler for paper, cosmetics, textiles, linoleum, rubber goods, paints. Barite generally occurs in a white massive variety (often appearing earthy when weathered), although some clear to bluish, bladed barite crystals have been observed in several vein deposits in central Kentucky, and commonly occurs as a solid solution series with celestite where barium and strontium can substitute for each other. Various nodular zones have been observed in Silurian–Devonian rocks in east-central Kentucky. -
Oil Shale, Part II: Geology and Mineralogy of the Oil Shales of the Green River Formation, Colorado, Utah and Wyoming
Article Oil shale, part II: geology and mineralogy of the oil shales of the Green River formation, Colorado, Utah and Wyoming JAFFE, Felice Reference JAFFE, Felice. Oil shale, part II: geology and mineralogy of the oil shales of the Green River formation, Colorado, Utah and Wyoming. Colorado School of Mines Mineral Industries Bulletin, 1962, vol. 5, no. 3, p. 1-16 Available at: http://archive-ouverte.unige.ch/unige:152772 Disclaimer: layout of this document may differ from the published version. 1 / 1 b ~L~ ~· () ~~ ,~Ov. (i) ~ COLORADO SCHOOL OF MIN~JT\-:-~----~1 Mi n e r a I/I nd u s t r, ie s B.u 11 e.t i n The Colorado School of Mines Mineral Industries Bulletin is published every other month by the Colorado School of Mines Research Foundation to inform those interested in the mineral industry regarding the elements of the geology and mineral resources, mining operations, metal markets, production statistics, economics, and other aspects of the mineral industry. This publication may be obtained for a yearly subscription charge af $1.00 for the six issues pub- lished from July through May of the following year. Past issues still in print may be had for 25c each. Address your order to the Department of Publica- tions, Colorado School af Mines, Golden, Colorado. Entered as second class matter at the Post Office at Golden, Colorado, under Act of Congress, July 16, 1894. Copyright 1962 by The Colorado School of Mines. All rights reserved. This publication or any part of it may not be reproduced in any form without written permission of the Colorado School af Mines. -
Barite (Barium)
Barite (Barium) Chapter D of Critical Mineral Resources of the United States—Economic and Environmental Geology and Prospects for Future Supply Professional Paper 1802–D U.S. Department of the Interior U.S. Geological Survey Periodic Table of Elements 1A 8A 1 2 hydrogen helium 1.008 2A 3A 4A 5A 6A 7A 4.003 3 4 5 6 7 8 9 10 lithium beryllium boron carbon nitrogen oxygen fluorine neon 6.94 9.012 10.81 12.01 14.01 16.00 19.00 20.18 11 12 13 14 15 16 17 18 sodium magnesium aluminum silicon phosphorus sulfur chlorine argon 22.99 24.31 3B 4B 5B 6B 7B 8B 11B 12B 26.98 28.09 30.97 32.06 35.45 39.95 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 potassium calcium scandium titanium vanadium chromium manganese iron cobalt nickel copper zinc gallium germanium arsenic selenium bromine krypton 39.10 40.08 44.96 47.88 50.94 52.00 54.94 55.85 58.93 58.69 63.55 65.39 69.72 72.64 74.92 78.96 79.90 83.79 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 rubidium strontium yttrium zirconium niobium molybdenum technetium ruthenium rhodium palladium silver cadmium indium tin antimony tellurium iodine xenon 85.47 87.62 88.91 91.22 92.91 95.96 (98) 101.1 102.9 106.4 107.9 112.4 114.8 118.7 121.8 127.6 126.9 131.3 55 56 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 cesium barium hafnium tantalum tungsten rhenium osmium iridium platinum gold mercury thallium lead bismuth polonium astatine radon 132.9 137.3 178.5 180.9 183.9 186.2 190.2 192.2 195.1 197.0 200.5 204.4 207.2 209.0 (209) (210)(222) 87 88 104 105 106 107 108 109 110 111 112 113 114 115 116 -
Selective Flotation of Witherite from Calcite Using Potassium Chromate As a Depressant
Physicochem. Probl. Miner. Process., 55(2), 2019, 565-574 Physicochemical Problems of Mineral Processing ISSN 1643-1049 http://www.journalssystem.com/ppmp © Wroclaw University of Science and Technology Received May 31, 2018; reviewed; accepted September 2, 2018 Selective flotation of witherite from calcite using potassium chromate as a depressant Yangshuai Qiu 1, Lingyan Zhang 1,2, Xuan Jiao 1, Junfang Guan 1,2, Ye Li 1,2, Yupeng Qian 1,2 1 School of Resources and Environmental Engineering, Wuhan University of Technology, Wuhan 430070, China 2 Hubei Key Laboratory of Mineral Resources Processing & Environment, Wuhan 430070, China Corresponding author: [email protected] (Lingyan Zhang) Abstract: Witherite has been widely used as an industrial and environmental source of barium, with calcite being the primary associated carbonate mineral. However, few studies have been conducted to effectively concentrate witherite from barium ores. In this work, with the treatment of potassium chromate (K2CrO4) and sodium oleate (NaOL), witherite was selectively separated from calcite through selective flotation at different pH conditions. In addition, contact angle, Zeta potential, adsorption and X-ray photoelectron spectroscopy measurements were performed to characterize the separation mechanisms. The results demonstrated that NaOL had a strong collecting ability for both witherite and calcite; nevertheless, witherite could be effectively selected from calcite with the highest recovery at pH 9 in the presence of K2CrO4. From the XPS measurements, NaOL and K2CrO4 were found to be primarily attached to the surfaces of witherite and calcite through chemisorption. The presence of K2CrO4 on the surface of calcite adversely influenced the NaOL adsorption, which could make the flotation separation efficient and successful. -
Infrare D Transmission Spectra of Carbonate Minerals
Infrare d Transmission Spectra of Carbonate Mineral s THE NATURAL HISTORY MUSEUM Infrare d Transmission Spectra of Carbonate Mineral s G. C. Jones Department of Mineralogy The Natural History Museum London, UK and B. Jackson Department of Geology Royal Museum of Scotland Edinburgh, UK A collaborative project of The Natural History Museum and National Museums of Scotland E3 SPRINGER-SCIENCE+BUSINESS MEDIA, B.V. Firs t editio n 1 993 © 1993 Springer Science+Business Media Dordrecht Originally published by Chapman & Hall in 1993 Softcover reprint of the hardcover 1st edition 1993 Typese t at the Natura l Histor y Museu m ISBN 978-94-010-4940-5 ISBN 978-94-011-2120-0 (eBook) DOI 10.1007/978-94-011-2120-0 Apar t fro m any fair dealin g for the purpose s of researc h or privat e study , or criticis m or review , as permitte d unde r the UK Copyrigh t Design s and Patent s Act , 1988, thi s publicatio n may not be reproduced , stored , or transmitted , in any for m or by any means , withou t the prio r permissio n in writin g of the publishers , or in the case of reprographi c reproductio n onl y in accordanc e wit h the term s of the licence s issue d by the Copyrigh t Licensin g Agenc y in the UK, or in accordanc e wit h the term s of licence s issue d by the appropriat e Reproductio n Right s Organizatio n outsid e the UK. Enquirie s concernin g reproductio n outsid e the term s state d here shoul d be sent to the publisher s at the Londo n addres s printe d on thi s page. -
Conservation of Coated and Specialty Papers
RELACT HISTORY, TECHNOLOGY, AND TREATMENT OF SPECIALTY PAPERS FOUND IN ARCHIVES, LIBRARIES AND MUSEUMS: TRACING AND PIGMENT-COATED PAPERS By Dianne van der Reyden (Revised from the following publications: Pigment-coated papers I & II: history and technology / van der Reyden, Dianne; Mosier, Erika; Baker, Mary , In: Triennial meeting (10th), Washington, DC, 22-27 August 1993: preprints / Paris: ICOM , 1993, and Effects of aging and solvent treatments on some properties of contemporary tracing papers / van der Reyden, Dianne; Hofmann, Christa; Baker, Mary, In: Journal of the American Institute for Conservation, 1993) ABSTRACT Museums, libraries, and archives contain large collections of pigment-coated and tracing papers. These papers are produced by specially formulated compositions and manufacturing procedures that make them particularly vulnerable to damage as well as reactive to solvents used in conservation treatments. In order to evaluate the effects of solvents on such papers, several research projects were designed to consider the variables of paper composition, properties, and aging, as well as type of solvent and technique of solvent application. This paper summarizes findings for materials characterization, degradative effects of aging, and some effects of solvents used for stain reduction, and humidification and flattening, of pigment-coated and modern tracing papers. Pigment-coated papers have been used, virtually since the beginning of papermaking history, for their special properties of gloss and brightness. These properties, however, may render coated papers more susceptible to certain types of damage (surface marring, embedded grime, and stains) and more reactive to certain conservation treatments. Several research projects have been undertaken to characterize paper coating compositions (by SEM/EDS and FTIR) and appearance properties (by SEM imaging of surface structure and quantitative measurements of color and gloss) in order to evaluate changes that might occur following application of solvents used in conservation treatments. -
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. -
Daqingshanite-(Ce) (Sr, Ca, Ba)3(Ce, La)(PO4)(CO3)3−X(OH, F)X C 2001-2005 Mineral Data Publishing, Version 1
Daqingshanite-(Ce) (Sr, Ca, Ba)3(Ce, La)(PO4)(CO3)3−x(OH, F)x c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 3m (probable). As subhedral to rounded platy crystals, may be crudely rhombohedral, to 3 mm, in aggregates. Twinning: Complex polysynthetic twinning observed in some material. Physical Properties: Cleavage: Perfect on {1011}. Fracture: Conchoidal. Hardness = n.d. VHN = 335 (20 g load). D(meas.) = 3.81 D(calc.) = 3.71 Optical Properties: Semitransparent. Color: Pale yellow to nearly white; colorless in thin section. Streak: White. Luster: Vitreous to greasy. Optical Class: Uniaxial (–). ω = 1.708 = 1.609 Cell Data: Space Group: R3m, R3m, or R32. a = 10.058–10.073 c = 9.225–9.234 Z = 3 X-ray Powder Pattern: Bayan Obo deposit, China. 3.16 (10), 2.52 (7), 3.95 (6), 2.040 (6), 1.941 (6), 2.110 (5), 1.895 (4) Chemistry: (1) (2) (1) (2) (1) (2) P2O5 11.73 10.50 Fe2O3 0.21 K2O 0.03 CO2 16.19 n.d. MnO 0.02 F 0.80 0.29 ThO2 0.04 < 0.22 MgO 0.72 < 0.12 Cl 0.10 + Al2O3 0.18 < 0.12 CaO 6.17 0.94 H2O 0.68 n.d. La2O3 7.88 10.22 SrO 26.10 41.82 −O=F2 0.34 Ce2O3 10.16 12.24 BaO 15.98 4.57 Total [99.376] RE2O3 2.696 < 3.36 Na2O 0.13 < 0.16 (1) Bayan Obo deposit, China; CO2 and H2O by gas chromatography, original total given as 99.20%; RE2O3 =Pr6O11 0.70%, Nd2O3 1.59%, Sm2O3 0.106%, Eu2O3 0.02%, Gd2O3 0.12%, Tb4O7 0.05%, Dy2O3 0.03%, Ho2O3 0.03%, Er2O3 0.01%, Tm2O3 0.01%, Yb2O3 0.02%, Lu2O3 0.01%; corresponds to (Sr1.52Ca0.67Ba0.63Mg0.11Na0.03)Σ=2.96(Ce0.37La0.29RE0.10Al0.02 3+ Fe0.02)Σ=0.80(PO4)1.00(CO3)2.23[(OH)0.46F0.26]Σ=0.72. -
NOTICE New Mineratr Names Has Been Prepared by Michael
NOTICE New Mineratr Names has been prepared by Michael Fleischer for many years with extraordinary coverage and critical evaluation, and remains one of the most important sections ol The Americon Mineral,ogist. Dr. Fleischer con- tinues to find the task enjoyable but increasingly burdensome. This is a call for volunteers to assist him in combing and reviewing the literature for clescrip- tions of new minerals and new mineral data Mineralogists interested, please contact Dr. M. Fleischer, U, S. Geological Survey, Washington 25, D. C., and specify the language(s) and journals you can ancl are willing to cover. Es- pecially helpful would be the services of three good mineralogists to cover Minerologicol Magazine, Bulletin Soci.6t6 Franqaise Minlralogie, and Neues Jahrbuch J* Minerologie etc., Monatshefte NEW MINERAL NAMES Farringtonite E. R' DurnnsNa aNo s. K. Rov. A new phosphate mineral from the springwater pallasite: Geocltim.et Cosmocltim.Acta,24, 198 205 (1961). The mineral was found in the springn'ater pallasite, from near Springwater, Sas- katchewan. rt occurs as colorless to wax-white to yellon' material peripheral to olivine nodules. The meteorite also contains metallic iron (kamacite) ancl troilite. Spectrographic analyses were made on two 25 mg. samples; the first rn'ascleaned magnetically, the second by gravity separation in a centrifuge as we1l. These gave: pror 37.6+0.6,49.7 + 1.0;MgO 49.2+O.2,4t.6I1.3; SiO, 11.1+0.2,2.9 +0.1; Fe 5.4+0.1,3.7 ,,quite +0.2ok. The final content of metallic iron in the samples was negligible,,; the Fe reported must be present as FeO or FezO: or both. -
Fluid Inclusions in Fibrous and Octahedrally-Grown Diamonds
FLUID INCLUSIONS IN FIBROUS AND OCTAHEDRALLY-GROWN DIAMONDS by Evan Mathew Smith A THESIS SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in The Faculty of Graduate and Postdoctoral Studies (Geological Sciences) THE UNIVERSITY OF BRITISH COLUMBIA (Vancouver) March 2014 © Evan Mathew Smith, 2014 Abstract My thesis puts forth new models for diamond formation that explain the difference between octahedral and fibrous diamond growth, as well as the difference between octahedral diamond growth in the lithospheric and the sublithospheric mantle. Diamond growth in the mantle involves reactions between carbon-bearing fluid and the host rocks it infiltrates. This fluid is sometimes included in diamond. Fluids in dendritically-grown, fibrous diamonds from Wawa, Superior craton, were analysed in a novel way, using transmission X-ray diffraction. The technique allows bulk analysis of daughter minerals within fluid inclusions. The mineralogy, major and trace elements, Sr isotopes, volatiles, and nitrogen characteristics of the hydrous saline–high-Mg carbonatitic fluid in these Archean diamonds strongly resemble those of Phanerozoic fibrous diamonds. This implies that some mantle processes, including the formation of fibrous diamonds, can be extended unvaryingly back to 2.7 Ga. Fluid equilibrated with octahedrally-grown diamonds from the Siberian, Kaapvaal, and Congo cratons is trapped in healed fractures in the diamonds. They contain anhydrous CO2–N2 fluid inclusions with 40±4 mol% N2 and inclusions of former silicate melt that had an original N2 content of ~0.1 wt%, as shown by Raman, electron microprobe, and microthermometry analyses. The liberation of N2 from the convecting mantle is proposed to be controlled by increasing oxygen fugacity that destabilizes host phases. -
List of Abbreviations
List of Abbreviations Ab albite Cbz chabazite Fa fayalite Acm acmite Cc chalcocite Fac ferroactinolite Act actinolite Ccl chrysocolla Fcp ferrocarpholite Adr andradite Ccn cancrinite Fed ferroedenite Agt aegirine-augite Ccp chalcopyrite Flt fluorite Ak akermanite Cel celadonite Fo forsterite Alm almandine Cen clinoenstatite Fpa ferropargasite Aln allanite Cfs clinoferrosilite Fs ferrosilite ( ortho) Als aluminosilicate Chl chlorite Fst fassite Am amphibole Chn chondrodite Fts ferrotscher- An anorthite Chr chromite makite And andalusite Chu clinohumite Gbs gibbsite Anh anhydrite Cld chloritoid Ged gedrite Ank ankerite Cls celestite Gh gehlenite Anl analcite Cp carpholite Gln glaucophane Ann annite Cpx Ca clinopyroxene Glt glauconite Ant anatase Crd cordierite Gn galena Ap apatite ern carnegieite Gp gypsum Apo apophyllite Crn corundum Gr graphite Apy arsenopyrite Crs cristroballite Grs grossular Arf arfvedsonite Cs coesite Grt garnet Arg aragonite Cst cassiterite Gru grunerite Atg antigorite Ctl chrysotile Gt goethite Ath anthophyllite Cum cummingtonite Hbl hornblende Aug augite Cv covellite He hercynite Ax axinite Czo clinozoisite Hd hedenbergite Bhm boehmite Dg diginite Hem hematite Bn bornite Di diopside Hl halite Brc brucite Dia diamond Hs hastingsite Brk brookite Dol dolomite Hu humite Brl beryl Drv dravite Hul heulandite Brt barite Dsp diaspore Hyn haiiyne Bst bustamite Eck eckermannite Ill illite Bt biotite Ed edenite Ilm ilmenite Cal calcite Elb elbaite Jd jadeite Cam Ca clinoamphi- En enstatite ( ortho) Jh johannsenite bole Ep epidote -
Barite–Celestine Geochemistry and Environments of Formation Jeffrey S
Barite–Celestine Geochemistry and Environments of Formation Jeffrey S. Hanor Department of Geology and Geophysics Louisiana State University Baton Rouge, Louisiana 70803 INTRODUCTION Minerals in the barite (BaSO4)–celestine (SrSO4) solid solution series, (Ba,Sr)SO4, occur in a remarkably diverse range of sedimentary, metamorphic, and igneous geological environments which span geological time from the Early Archean (~3.5 Ga) to the present. The purpose of this chapter is to review: (1) the controls on the chemical and isotopic composition of barite and celestine and (2) the geological environments in which these minerals form. Some health risks are associated with barite, and these are discussed near the end of this chapter. Although complete solid solution exists between BaSO4 and SrSO4 most representa- tives of the series are either distinctly Ba-rich or Sr-rich. Hence, it is convenient to use the term barite to refer to not only the stochiometric BaSO4 endmember but also to those (Ba,Sr)SO4 solid solutions dominated by Ba. Similarly, the term celestine will refer here not only to the stoichiometric SrSO4 endmember but to solid solutions dominated by Sr. Such usage is in accord with standard mineral nomenclature. The Committee on Mineral Names and Nomenclature of the International Mineralogical Association recognizes “celestine” as the official name for SrSO4. However, the name “celestite” is still commonly used in the literature. Geological significance of barite and celestine Most of the barite which exists in the Earth’s crust has formed through the mixing of fluids, one containing Ba leached from silicate minerals, and the other an oxidized shallow fluid, such as seawater, which contains sulfate.