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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 -
Newsletter June 2006
w NEWSLETTER INTERNATIONAL TUNGSTEN INDUSTRY ASSOCIATION Rue Père Eudore Devroye 245, 1150 Brussels, Belgium Tel: +32 2 770 8878 Fax: + 32 2 770 8898 E-mail: [email protected] Web: www.itia.info The programme will begin on Tuesday Toxicologic Assessment for the Production and 19th evening with a Reception in the hotel jointly Mechanical Processing of Materials containing hosted by Tiberon Minerals and ITIA. Tungsten Heavy Metal. Not least will be an introduction to the formation of a Consortium to deal Working sessions will be held on Wednesday Annual with the implications of REACH on behalf of the and Thursday mornings and papers will tungsten industry, both legal and financial. include: General Readers will recall that REACH will place an obligation ▼ HSE work programme on individual companies to submit a technical dossier and register any chemical substance Meeting ▼ Ganzhou’s Tungsten Industry and Its Progress manufactured or imported into the EU in quantities ▼ Geostatistics in the mid and long-term planning for of more than 1 tonne. the Panasqueira deposit (Nuno Alves, Beralt Tin Tuesday 26 to and Wolfram) In order to assist companies with the registration process, the Commission recommends the creation ▼ Thursday 28 Paper by Zhuzhou Cemented Carbide of industry Consortia. These Consortia will enable the ▼ Update on Tiberon’s Development of Tungsten joint development, submission and sharing of September 2006 Mining in Vietnam information with the aim of reducing the compliance burden on individual companies and preventing ▼ Update on China’s Tungsten Industry Hyatt Regency Hotel, unnecessary additional animal testing. ▼ Update on US Tungsten Market (Dean Schiller, Boston, USA OsramSylvania Products) Both members and non-members will be equally ▼ Review of Trends in 2006 (Nigel Tunna, Metal-Pages) welcome to join the Consortium, saving themselves considerable amounts of money and time by so doing. -
Khomyakovite and Manganokhomyakovite, Two
893 TheCanadian Mineralogist Vol. 37,pp. 893-899 (1999) KHOMYAKOVITEAND MANGANOKHOMYAKOVITE, TWO NEW MEMBERS OF THEEUDIALYTE GROUP FROM MONT SAINT.HILAIRE, QUEBEC, CANADA OLE JOHNSEN Geological Museum, University of Copenhagen,Oster Voldgade 5-7, DK-L350 Copenhagen,Denmark ROBERT A. GAULT, JOEL D. GRICE AND T. SCOTT ERCIT Research Division, Canadian Museum of Nature, P O. Box 3143, Station D, Ottawa, Ontario Kl P 6P4, Canaela Aesrnacr Khomyakovite, ideally Nal2Sr3Ca6Fe3Zr3W(Si25O73)(O,OH,H2O)3(OH,Cl)zand manganokhomyakovite, ideally Na12Sr3Ca6N4n3Zr3W(Si25O7r(O,OH,H2O)3(OH,Cl)2are two new members of the eudialyte group from Mont Saint-Hilaire, Quebec. They occur as orange to orange-red,pseudo-octahedral crystals ranging in size from 0.5 mm (khomyakovite) to 5 mm (manganokhomyakovite).Associated minerals include, for khomyakovite: analcime, annite, calcite, natrolite, pyrite, and titanite, and for manganokhomyakovite:aegirine, albite, analcime,annite, cerussite, galena, kupletskite, microcline, molybdenite, natrolite, pyrite, pyrrhotite, sodalite, sphalerite, titanite, wohlerite and zircon. Both minerals are transparentto translucent, with a vitreous luster and white streak They are brittle, with a hardnessof 5-6 (Mohs scale). They have no cleavage,no parting and an uneven fractue. They are uniaxial negative, for khomyakovire: a = 1.62'19(5) and e = I.6254(5), and for manganokhomyakovite: = o -= 1.629(1) and e 1.626(2).They are trigonal, spacegroup R3n. For kho-myakovitg.a 14.2959(8),c 30.084(3) A,V 5324.6('l) A3, and for manganokhomyakovi -
Mitteilungen Der Osterreichischen Mineralogischen Gesellschaft
Mitteilungen der II Osterreichischen Mineralogischen Gesellschaft Band 146 2001 Herausgegeben von der Österreichischen Mineralogischen Gesellschaft für das Vereinsjahr 2000 Eigenverlag Mitteilungen der Österreichischen Mineralogischen Gesellschaft Band 146 2001 Vereinsjahr 2000 Gefördert aus Mitteln des Bundesministeriums für Wissenschaft und Verkehr in Wien. Impressum: Eigentümer, Herausgeber und Verleger: Österreichische Mineralogische Gesellschaft p.A. Mineralogisch-Petrographische Abteilung, Naturhistorisches Museum Wien Burgring 7, A- 1014 Wien Homepage: http://www.univie.ac.at/Mineralogie/Oemg.htm ISSN 1609-0144 Redaktion: Friedrich Koller, Institut für Petrologie, Universität Wien Geozentrum, Althanstraße 14, A-1090 Wien Anton Beran, Institut für Mineralogie & Kristallographie, Universität Wien Geozentrum, Althanstraße 14, A-1090 Wien Richard Tessadri, Institut für Mineralogie & Petrographie, Universität Innsbruck lnnrain 52, A-6020 Innsbruck Gestaltung und Layout: R. Tessadri (Innsbruck) Für den Inhalt sind die Autoren selbst verantwortlich. Druck: Anton Riegelnik,Piaristengasse 19, A-1080 Wien Printed in Austria MITI.ÖSTERR.MINER.GES. 146(2001) INHALT MinPet 2001, 24.-26. September 2001, Vienna, Geocenter Anniversary Meeting Österreichische Mineralogische Gesellschaft (ÖMG) 1901-2001 Abart R., BadertscherN., Bernhard F., Burkhard M., Koller F. & Povoden E.: Syn-deformative fluidcirculation at the Glarus Thrust, E-Switzerland S. 13 Adamovic J., Melka K. & Ulrych J.: Fe-oxyhydroxide cementation in cretaceous sandstones, northern Bohemia: relation to young volvanic activity S. 16 Akinin V. V .. NtaflosTh. & Richter W.: Augite megacrysts from Enmelen volcanoes (Bering Sea basalt province) S. 18 AndrutM. & Wildner M.: Lumineszenzspektroskopische Identifizierungspin verbotener Übergänge von CrJ+ als Voraussetzung zur Anwendung des "Superposition Model" (SM) auf Uwarowite S. 21 Andrut M., Hammer V M. F., Lengauer C. L., NtaflosT. & Redhammer G. J.: Untersuchungen zur Farbe des Lazuliths S. -
GEUS No 190.Pmd
G E O L O G Y O F G R E E N L A N D S U R V E Y B U L L E T I N 1 9 0 · 2 0 0 1 The Ilímaussaq alkaline complex, South Greenland: status of mineralogical research with new results Edited by Henning Sørensen Contributions to the mineralogy of Ilímaussaq, no. 100 Anniversary volume with list of minerals GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF THE ENVIRONMENT 1 Geology of Greenland Survey Bulletin 190 Keywords Agpaite, alkaline, crystallography, Gardar province, geochemistry, hyper-agpaite, Ilímaussaq, mineralogy, nepheline syenite, peral- kaline, Mesoproterozoic, rare-element minerals, South Greenland. Cover Igneous layering in kakortokites in the southern part of the Ilímaussaq alkaline complex, South Greenland. The central part of the photograph shows the uppermost part of the layered kakortokite series and the overlying transitional kakortokites and aegirine lujavrite on Laksefjeld (680 m), the dark mountain in the left middle ground of the photograph. The cliff facing the lake in the right middle ground shows the kakortokite layers + 4 to + 9. The kakortokite in the cliff on the opposite side of the lake is rich in xenoliths of roof rocks of augite syenite and naujaite making the layering less distinct. On the skyline is the mountain ridge Killavaat (‘the comb’), the highest peak 1216 m, which is made up of Proterozoic granite which was baked and hardened at the contact to the intrusive complex. The lake (987 m) in the foreground is intensely blue and clear because it is practically devoid of life. -
CM37 893.Pdf
893 TheCanadian Mineralogist Vol. 37,pp. 893-899 (1999) KHOMYAKOVITEAND MANGANOKHOMYAKOVITE, TWO NEW MEMBERS OF THEEUDIALYTE GROUP FROM MONT SAINT.HILAIRE, QUEBEC, CANADA OLE JOHNSEN Geological Museum, University of Copenhagen,Oster Voldgade 5-7, DK-L350 Copenhagen,Denmark ROBERT A. GAULT, JOEL D. GRICE AND T. SCOTT ERCIT Research Division, Canadian Museum of Nature, P O. Box 3143, Station D, Ottawa, Ontario Kl P 6P4, Canaela Aesrnacr Khomyakovite, ideally Nal2Sr3Ca6Fe3Zr3W(Si25O73)(O,OH,H2O)3(OH,Cl)zand manganokhomyakovite, ideally Na12Sr3Ca6N4n3Zr3W(Si25O7r(O,OH,H2O)3(OH,Cl)2are two new members of the eudialyte group from Mont Saint-Hilaire, Quebec. They occur as orange to orange-red,pseudo-octahedral crystals ranging in size from 0.5 mm (khomyakovite) to 5 mm (manganokhomyakovite).Associated minerals include, for khomyakovite: analcime, annite, calcite, natrolite, pyrite, and titanite, and for manganokhomyakovite:aegirine, albite, analcime,annite, cerussite, galena, kupletskite, microcline, molybdenite, natrolite, pyrite, pyrrhotite, sodalite, sphalerite, titanite, wohlerite and zircon. Both minerals are transparentto translucent, with a vitreous luster and white streak They are brittle, with a hardnessof 5-6 (Mohs scale). They have no cleavage,no parting and an uneven fractue. They are uniaxial negative, for khomyakovire: a = 1.62'19(5) and e = I.6254(5), and for manganokhomyakovite: = o -= 1.629(1) and e 1.626(2).They are trigonal, spacegroup R3n. For kho-myakovitg.a 14.2959(8),c 30.084(3) A,V 5324.6('l) A3, and for manganokhomyakovi -
1 Geological Association of Canada Mineralogical
GEOLOGICAL ASSOCIATION OF CANADA MINERALOGICAL ASSOCIATION OF CANADA 2006 JOINT ANNUAL MEETING MONTRÉAL, QUÉBEC FIELD TRIP 4A : GUIDEBOOK MINERALOGY AND GEOLOGY OF THE POUDRETTE QUARRY, MONT SAINT-HILAIRE, QUÉBEC by Charles Normand (1) Peter Tarassoff (2) 1. Département des Sciences de la Terre et de l’Atmosphère, Université du Québec À Montréal, 201, avenue du Président-Kennedy, Montréal, Québec H3C 3P8 2. Redpath Museum, McGill University, 859 Sherbrooke Street West, Montréal, Québec H3A 2K6 1 INTRODUCTION The Poudrette quarry located in the East Hill suite of the Mont Saint-Hilaire alkaline complex is one of the world’s most prolific mineral localities, with a species list exceeding 365. No other locality in Canada, and very few in the world have produced as many species. With a current total of 50 type minerals, the quarry has also produced more new species than any other locality in Canada, and accounts for about 25 per cent of all new species discovered in Canada (Horváth 2003). Why has a single a single quarry with a surface area of only 13.5 hectares produced such a mineral diversity? The answer lies in its geology and its multiplicity of mineral environments. INTRODUCTION La carrière Poudrette, localisée dans la suite East Hill du complexe alcalin du Mont Saint-Hilaire, est l’une des localités minéralogiques les plus prolifiques au monde avec plus de 365 espèces identifiées. Nul autre site au Canada, et très peu ailleurs au monde, n’ont livré autant de minéraux différents. Son total de 50 minéraux type à ce jour place non seulement cette carrière au premier rang des sites canadiens pour la découverte de nouvelles espèces, mais représente environ 25% de toutes les nouvelles espèces découvertes au Canada (Horváth 2003). -
New Data on Minerals
RUSSIAN ACADEMY OF SCIENCES FERSMAN MINERALOGICAL MUSEUM volume 43 New Data on Minerals FOUNDED IN 1907 MOSCOW 2008 ISSN 5900395626 New Data on Minerals. Volume 43. Мoscow: Аltum Ltd, 2008. 176 pages, 250 photos, and drawings. Editor: Margarita I. Novgorodova, Doctor in Science, Professor. Publication of Institution of Russian Academy of Sciences – Fersman Mineralogical Museum RAS This volume contains articles on new mineral species and new finds of rare minerals, among them – Nalivkinite, a new mineral of the astrophyllite group; new finds of Dzhalindite, Mo-bearing Stolzite and Greenockite in ores of the Budgaya, Eastern Transbaikalia; new finds of black Powellite in molybdenum-uranium deposit of Southern Kazakhstan. Corundum-bearing Pegmatite from the Khibiny massif and Columbite-Tantalite group minerals of rare- metal tantalum-bearing amazonite-albite granites from Eastern Transbaikalia and Southern Kazakhstan are described. There is also an article on mineralogical and geochemical features of uranium ores from Southeastern Transbaikalia deposits. New data on titanium-rich Biotite and on polymorphs of anhydrous dicalcium orthosilicate are published. “Mineralogical Museums and Collections” section contains articles on collections and exhibits of Fersman Mineralogical Museum RAS: on the collection of mining engineer I.N. Kryzhanovsky; on Faberge Eggs from the funds of this museum (including a describing of symbols on the box with these eggs); on the exhibition devoted to A.E. Fersman’s 125th anniversary and to 80 years of the first edition of his famous book “Amuzing Mineralogy” and the review of Fersman Mineralogical Museum acquisitions in 2006–2008. This section includes also some examples from the history of discovery of national deposits by collection’s specimens. -
The Picking Table Volume 41, No. 2 – Fall 2000
ICKIHIE The ABLE JOURNAL OF THE FRANKLIN-OGDENSBURG MiNERALOGICAL SOCIETY /olume 41, No. 2 - Fall 2000 $10.00 U.S. Mid range Ultraviolet Responses Palache's Contributions to the Mineralogy of Sterling Hill New Species: Synchysite Schedule of Activities Thorutite FOMS News The contents of The Picking Table are licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. THE 44TH ANNUAL Franklin-Sterling Hill Mineral and Gem Show Proudly Presented By FRANKLIN THE FRANKLIN MINERAL MUSEUM FRANKLIN M M September 23 & 24, 2000 U N s E Saturday: 9:00 AM - 6:00 PM E R U A Sunday: 10:00 AM - 5:00 PM M L i * FREE PARKING * FRANKLIN SCHOOL - WASHINGTON AVE. off Buckwheat Rd by way of Franklin Ave. FRANKLIN, NEW JERSEY * DEALERS * GEMS * JEWELRY * MINERALS * FOSSILS * *WIRE WRAPPING * JEWELRY REPAIR * RING SIZING * * STONE CARVINGS * STONE MOUNTING * * LECTURES * LITERATURE * FLUORESCENT MINERAL EXHIBITS* * PRIVATE AND INSTITUTIONAL EXHIBITORS * * MINERAL COLLECTING AT THE BUCKWHEAT DUMP * MUSEUM TOURS * NEARBY RESTAURANTS* DOOR PRIZES THE TRADITIONAL "POND" OUTDOOR SWAP/SELL HOURS: SEPT23, SAT 6:30 AM - 6 PM SEPT 24, SUN. 8 AM- 5 PM !!! A FUN DA Y FOR THE ENTIRE FAMIL Y!!! For information: The Franklin Mineral Museum Evans Street, Box 54 Franklin, NJ 07416 (973) 827-3481 COME VISIT US! Daily Admission: Adults: $4.00 Two Days: $7.00 Children: $2.00 $3.00 Admission covers the show, outdoor swap,and admission to the Franklin Mineral Museum. The Franklin Mineral Museum is a nonprofit, educational institution. The contents of The Picking Table are licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. -
New Data on the Isomorphism in Eudialyte-Group Minerals. 2
minerals Review New Data on the Isomorphism in Eudialyte-Group Minerals. 2. Crystal-Chemical Mechanisms of Blocky Isomorphism at the Key Sites Ramiza K. Rastsvetaeva 1 and Nikita V. Chukanov 2,3,* 1 Shubnikov Institute of Crystallography of Federal Scientific Research Centre “Crystallography and Photonics”, Russian Academy of Sciences, Leninskiy Prospekt 59, 119333 Moscow, Russia; [email protected] 2 Institute of Problems of Chemical Physics, Russian Academy of Sciences, Chernogolovka, 142432 Moscow, Russia 3 Faculty of Geology, Moscow State University, Vorobievy Gory, 119991 Moscow, Russia * Correspondence: [email protected] Received: 24 July 2020; Accepted: 14 August 2020; Published: 17 August 2020 Abstract: The review considers various complex mechanisms of isomorphism in the eudialyte-group minerals, involving both key positions of the heteropolyhedral framework and extra-framework components. In most cases, so-called blocky isomorphism is realized when one group of atoms and ions is replaced by another one, which is accompanied by a change in the valence state and/or coordination numbers of cations. The uniqueness of these minerals lies in the fact that they exhibit ability to blocky isomorphism at several sites of high-force-strength cations belonging to the framework and at numerous sites of extra-framework cations and anions. Keywords: eudialyte group; crystal chemistry; blocky isomorphism; peralkaline rocks 1. Introduction Eudialyte-group minerals (EGMs) are typical components of some kinds of agpaitic igneous rocks and related pegmatites and metasomatic assemblages. Crystal-chemical features of these minerals are important indicators reflecting conditions of their formation (pressure, temperature, fugacity of oxygen and volatile species, and activity of non-coherent elements [1–9]). -
IMA–CNMNC Approved Mineral Symbols
Mineralogical Magazine (2021), 85, 291–320 doi:10.1180/mgm.2021.43 Article IMA–CNMNC approved mineral symbols Laurence N. Warr* Institute of Geography and Geology, University of Greifswald, 17487 Greifswald, Germany Abstract Several text symbol lists for common rock-forming minerals have been published over the last 40 years, but no internationally agreed standard has yet been established. This contribution presents the first International Mineralogical Association (IMA) Commission on New Minerals, Nomenclature and Classification (CNMNC) approved collection of 5744 mineral name abbreviations by combining four methods of nomenclature based on the Kretz symbol approach. The collection incorporates 991 previously defined abbreviations for mineral groups and species and presents a further 4753 new symbols that cover all currently listed IMA minerals. Adopting IMA– CNMNC approved symbols is considered a necessary step in standardising abbreviations by employing a system compatible with that used for symbolising the chemical elements. Keywords: nomenclature, mineral names, symbols, abbreviations, groups, species, elements, IMA, CNMNC (Received 28 November 2020; accepted 14 May 2021; Accepted Manuscript published online: 18 May 2021; Associate Editor: Anthony R Kampf) Introduction used collection proposed by Whitney and Evans (2010). Despite the availability of recommended abbreviations for the commonly Using text symbols for abbreviating the scientific names of the studied mineral species, to date < 18% of mineral names recog- chemical elements -
New Mineral Names*
American Mineralogist, Volume 85, pages 873–877, 2000 NEW MINERAL NAMES* JOHN L. JAMBOR1, VLADIMIR A. KOVALENKER2, AND ANDREW C. ROBERTS3 1Department of Earth and Ocean Sciences, University of British Columbia, Vancouver, British Columbia V6T 1Z4, Canada 2IGREM RAN, Russian Academy of Sciences, Moscow 10917, Staromonetnii 35, Russia 3Geological Survey of Canada, 601 Booth Street, Ottawa K1A 0E8, Canada Bariosincosite* Cobaltolotharmeyerite* A. Pring, U. Kolitsch, W.D. Birch, B.D. Beyer, P. Elliott, P. W. Krause, H. Effenberger, H.-J. Bernhardt, M. Martin (1999) Ayyappan, A. Ramanan (1999) Bariosincosite, a new hydrated Cobaltolotharmeyerite, Ca(Co,Fe,Ni)2(AsO4)2(OH,H2O)2, a barium vanadium phosphate, from the Spring Creek Mine, new mineral from Schneeberg, Germany. Neues Jahrb. Min- South Australia. Mineral. Mag., 63, 735–741. eral. Mon., 505–517. The mineral occurs as irregular clusters of radiating to diver- Electron microprobe analysis of the mineral from the type gent platy crystals, each crystal up to 250 µm across and 5 µm in locality gave a mean and range (16 analyses) of CaO 12.18 thickness, on cuprite or native copper within cavities in a quartz- (11.94–12.43), NiO 5.76 (4.04–7.28), CoO 15.70 (14.24– goethite host. Electron microprobe analysis gave BaO 23.20, SrO 16.50), Fe2O3 11.53 (10.21–12.25), As2O5 49.36 (45.52–51.02), 4.19, CaO 0.36, VO2 31.55, Fe2O3 0.20, Al2O3 0.50, P2O5 28.15, H2O (calc.) 6.39, sum 100.92 wt%, corresponding to H2O (calc.) 13.93, sum 102.08 wt%, corresponding to Ca1.01(Co0.97Fe0.67Ni0.36)Σ2.00(AsO4)2.00[(OH)0.69(H2O)1.31]Σ2.00.