Empirical Models for Structural Effects of A-Site Point
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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 -
New Mineral Names*
Ameican Mineralogist, Volume 83, pages 400-403, 1998 NEW MINERAL NAMES* JouN L. JAvrsonr aNo ANonEw C. Ronnnrs2 rDepartmentof Earth Sciences,University of Waterloo, Waterloo, Ontario N2L 3Gl, Canada 'Geological Survey of Canada,601 Booth Street,Ottawa, Ontario KIA 0Gl, Canada Benyacarite* from the results of a crystal structure determination.The F Demartin, T. Pilati, H.D. Gay, C.M. Gramaccioli (1993) empirical formula on the basis of 23 anions is The crystal structureof a mineral related to paulkerrite. (Ca.ouKoo,)r. urB5O6(OH)?Cl,nn.8HrO. The mineral occurs Zeits. Kristallogr.,208, 51-7I. as micaceous grains, 0.5 x 0.25 x 0.1 mm, that form E Demartin, H.D. Gay, C.M. Gramaccioli, T. Pilati (1997) cleavablemasses up to 2 x 1 x 1 mm. Colorlessto white, Benyacarite, a new titanium-bearingphosphate mineral transparent to translucent, viffeous luster, white streak, speciesfrom Cerro Blanco, Argentina. Can. Mineral., flexible, micaceous,perfect cleavage, : 35,701-712. {010} H 5, twinned on (010),nonfluorescent, D-""" : L91(3), D.^.: Chemical data in the 1993 paper were abstractedin 1.93 glcm3 for Z : 2. The IR spectrum shows the pres- Am. Mineral., 79, p. 763, 1994.On the basisof Z : 4, ence of HrO groups and complex borate groups.Optically the empirical formula is [(HrO)orrK.o,uNfo o.], Ti(Mn2*Vor. biaxial negative, ct : 1.506(2), P : 1.527(2), 1 : Fefrl,Mgo.),(Fe3*8Ti6j8Al00,),(PO")o(OouFoo),. l4H,O, The I.532(2),2V^"",: 56(l),2V,^,.: 51.4', oientationZ : mineral occurs as euhedral tabular to almost equidimen- b, X A c : 3U in the obtuse angle B. -
New Mineral Names*
---- -- American Mineralogist, Volume 70, pages 214-221, 1985 NEW MINERAL NAMES* PETE J. DUNN, GEORGE Y. CHAO, MICHAEL FLEISCHER, JAMES A. FERRAIOLO, RICHARD H. LANGLEY, ADOLF PAaST, AND JANET A. ZILCZER Bulachlte* (RE1.7tFeij:1i5 Tho.03Po.01h:=I.80 C5.15015.95 F 1.94,(Ba2.47SrO.02Cao.06 K. Walenta (1983) Bulachite, a new aluminum arsenate mineral Nao.3s~.07h:-3.00 (RE1.63Feij~ Tho.02AIo.01h:-1.70C5.23015.ssF2.56 and (Ba2.53SrO.03CaO.t3Nao.24Ko.07h:-3.00 (REt.66 Tho.02Po.os from Neubulach in the northern Black Forest. Der Aufschluss, 34,445-451 (in German). Alo.01h:- J.70C4.96015.66F1.SS,or ideally Ba3Ce2(C03hF2' The min- erai dissolves readily in dilute HCI and in other strong inorganic Chemical analysis gave Ah03 37.2, AS205 39.1 and H20 (by acids. weight loss) 25.5, sum 101.8%, leading to the idealized formula Weissenberg photographs, four-circle single-crystal diffrac- Ah(As04)(OHh . 3H20. Bulachite is easily soluble in HCII: I, tometry and electron diffraction show the mineral to be mono- less easily in HN03 I: I. clinic, C2/m, Cm or C2, a = 21.4256, b = 5.0348, c = 13.2395A, Dimensions of the orthorhombic unit cell, as determined from (3= 94.613°. There is a pronounced rhombohedral subcell with a' an indexed X-ray powder diffraction pattern, are: a 15.53, b = 5.11, c' = 9.8A, similar to the subcell of huanghoite (Am. 17.78, c 7.03A, Z = 10, D (meas.) 2.60, (calc.) 2.55. The Mineral., 48, 1179, 1963). -
Shin-Skinner January 2018 Edition
Page 1 The Shin-Skinner News Vol 57, No 1; January 2018 Che-Hanna Rock & Mineral Club, Inc. P.O. Box 142, Sayre PA 18840-0142 PURPOSE: The club was organized in 1962 in Sayre, PA OFFICERS to assemble for the purpose of studying and collecting rock, President: Bob McGuire [email protected] mineral, fossil, and shell specimens, and to develop skills in Vice-Pres: Ted Rieth [email protected] the lapidary arts. We are members of the Eastern Acting Secretary: JoAnn McGuire [email protected] Federation of Mineralogical & Lapidary Societies (EFMLS) Treasurer & member chair: Trish Benish and the American Federation of Mineralogical Societies [email protected] (AFMS). Immed. Past Pres. Inga Wells [email protected] DUES are payable to the treasurer BY January 1st of each year. After that date membership will be terminated. Make BOARD meetings are held at 6PM on odd-numbered checks payable to Che-Hanna Rock & Mineral Club, Inc. as months unless special meetings are called by the follows: $12.00 for Family; $8.00 for Subscribing Patron; president. $8.00 for Individual and Junior members (under age 17) not BOARD MEMBERS: covered by a family membership. Bruce Benish, Jeff Benish, Mary Walter MEETINGS are held at the Sayre High School (on Lockhart APPOINTED Street) at 7:00 PM in the cafeteria, the 2nd Wednesday Programs: Ted Rieth [email protected] each month, except JUNE, JULY, AUGUST, and Publicity: Hazel Remaley 570-888-7544 DECEMBER. Those meetings and events (and any [email protected] changes) will be announced in this newsletter, with location Editor: David Dick and schedule, as well as on our website [email protected] chehannarocks.com. -
Crystallographic Studies of Selected Perovskite-Group Compounds / by Shannon Farrell
Lakehead University Knowledge Commons,http://knowledgecommons.lakeheadu.ca Electronic Theses and Dissertations Retrospective theses 1997 Crystallographic studies of selected perovskite-group compounds / by Shannon Farrell. Farrell, Shannon Patrick http://knowledgecommons.lakeheadu.ca/handle/2453/2539 Downloaded from Lakehead University, KnowledgeCommons INFORMATION TO USERS This manuscript has been reproduced from the microfihn master. UMI fîhns the text directly from the orignal or copy submitted. Thus, some thesis and dissertation copies are in typewriter &ce, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, b%inning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. Each original is also photographed in one exposure and is included in reduced form at the back of the book. Photographs included in the original manuscript have been reproduced xerographically in this copy. Higher quality 6” x 9” black and white photographic prints are available for any photographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. UMI A Bell & Howell Infonnation C o m paiy 300 North Zeeb Road, Ann Arbor MI 48106-1346 USA 313/761-4700 800/521-0600 Reproduced with permission of the copyright owner. -
Revision 2 1 2 3 Goldschmidtite, (K,REE,Sr)(Nb,Cr)O3
1 Revision 2 2 3 4 Goldschmidtite, (K,REE,Sr)(Nb,Cr)O3: a new perovskite supergroup mineral 5 found in diamond from Koffiefontein, South Africa 6 7 Nicole A. Meyer*1, Michelle D. Wenz2, James P. S. Walsh3, Steven D. Jacobsen2, 8 Andrew J. Locock1, and Jeffrey W. Harris4 9 10 *corresponding author email: [email protected] 11 1 12 1Department of Earth and Atmospheric Sciences 13 1-26 Earth Sciences Building 14 University of Alberta 15 Edmonton, Alberta, Canada, T6G 2E3 16 17 2Department of Earth and Planetary Sciences 18 Northwestern University 19 2145 Sheridan Road 20 Technological Institute 21 Evanston, Illinois, USA, 60208 22 23 3Department of Chemistry 24 Northwestern University 25 2145 Sheridan Road 26 Evanston, Illinois, USA, 60208 27 28 4School of Geographical and Earth Sciences 29 University of Glasgow 30 The Gregory Building 31 Lilybank Gardens 32 Glasgow, Scotland, United Kingdom, G12 8QQ 33 34 2 35 ABSTRACT 36 Goldschmidtite is a new perovskite-group mineral (IMA No. 2018-034) with ideal formula 37 (K,REE,Sr)(Nb,Cr)O3. A single grain of goldschmidtite with maximum dimension of ~100 m 38 was found as an inclusion in a diamond from the Koffiefontein pipe in South Africa. In addition 39 to the dark green and opaque goldschmidtite, the diamond contained a Cr-rich augite (websteritic 40 paragenesis) and an intergrowth of chromite, Mg-silicate, and unidentified K-Sr-REE-Nb-oxide. 41 Geothermobarometry of the augite indicates the depth of formation was ~170 km. The chemical 42 composition of goldschmidtite determined by electron microprobe analysis (n = 11, WDS, wt%) 43 is: Nb2O5 44.82, TiO2 0.44, ThO2 0.10, Al2O3 0.35, Cr2O3 7.07, La2O3 11.85, Ce2O3 6.18, Fe2O3 44 1.96 MgO 0.70, CaO 0.04, SrO 6.67, BaO 6.82, K2O 11.53, total 98.53. -
Aspects of the Mineralogy of the Murun Alkaline Complex, Yakutia, Russia
Aspects of the mineralogy of the Murun alkaline complex, Yakutia, Russia. by Ekaterina Reguir @ Submitted in the partial filfilment of the requirements for the degree of Master of Science Supervisor: Dr. Roger. H. Mitchell Department of Geology Lakehead University Thunder Bay, Ontario Canada April2001 Nationai Library Bibliothèque nationale 1*1 of Canada du Canada Acquisitions and Acquisitions et Bibliographie Services services bibliographiques 395 Weltington Street 395. nie Wellington Ottawa ON K1A ON4 Ottawa ON KIA ON4 Canada Canada The author has granted a non- L'auteur a accorde une licence non exclusive licence allowing the exclusive permettant à la National Lhrary of Canada to Bibliothèque nationale du Canada de reproduce, loan, distribute or sell reproduire, prêter, distribuer ou copies of this thesis in microform, vendre des copies de cette thèse sous paper or electronic formats. la fome de microfiche/film, de reproduction sur papier ou sur format électronique. The author retains ownership of the L'auteur conserve la propriété du copyright in this thesis. Neither the droit d'auteur qui protège cette thèse. thesis nor substantial extracts fiom it Ni la thése ni des extraits substantiels may be printed or otheMrise de celle-ci ne doivent être imprimés reproduced without the author's ou autrement reproduits sans son permission. autorisation. The Murun complex contains a nurnber of unusual and mineralogically unique rocks. Many of them are problematic in texms of their genesis and petrographic interpretation. These enigmatic rocks include charoite assemblages, as well as unique Ba-Sr-nch carbonatites and alkaline ultramafic dykes refmed to as lamproites or lamprophyres. Charoitites occur in about 25 localities dong the southem margin of the Little Mum intrusion. -
New Mineral Names*
American Mineralogist, Volume 69, pages 1190-1196, 1984 NEW MINERAL NAMES* PETE J. DUNN, LoUIS J. CABRI, JAMES A. FERRAIOLO, JOEL D. GRICE, JOHN L. JAMBOR, WOLFGANG MUELLER, JAMES E. SHIGLEY, JACEK PUZIEWICZ, AND DAVID A. YANKO Bismutostibiconite* mineral usually occurs as individual grains up to 200 JLm, but it is sometimes closely intergrown with polarite, sobolevskite, sper- K. Walenta (1983) Bismutostibiconite, a new mineral of the rylite and other platinum-group minerals. In galena-chalcopyrite stibiconite group from the Black Forest. Chern. Erde, 42, 77- vein ores, cassiterite and stannite are associated with cabriite. 81 (in German). The mineral has been synthesized and disorders at 200°C to Quantitative analysis (electron beam instrument with stan- form cubic (Pd,CuhSn solid solution. dardless EDS) of the mineral gave Fe203 6.9, Bh03 49.2, Sb203 In polished section the mineral is white with a slight greyish 43.9, sum 100.0%, corresponding to Fe~~4Bit3ISbi~907' a Bi (pinkish?) tinge the brightness of the pink color changes depend- and Fe containing member of the stibiconite group. ing on the host minerals. Bireflectance in air is detectable, and X-ray camera studies show the mineral to be cubic, Fd3m, a = under crossed nicols, cabriite grains are strongly anisotropic 10.38A., Z = 8, D calc. 7.38. The strongest X-ray lines (12 given) (from greyish brown to golden colors). Cabriite characteristically are 3.01(10(222), 2.60(7)(400), 1.833(7)(440), 1.565(7)(622). exhibits a shreddy-aggregate texture, and individual grains are The mineral is always anhedral and forms yellow to yellowish- poly synthetically twinned.