Distinction of Taaffeite and Musgravite

Total Page:16

File Type:pdf, Size:1020Kb

Distinction of Taaffeite and Musgravite The Journal of Gemmology Volume 26 No. 3 July 1998 The Gemmological Association and Gem Testing Laboratory of Great Britain Gemmological Association and Gem Testing Laboratory of Great Britain 27 Greville Street, London EC1N 8SU Tel: 0171 404 3334 Fax: 0171 404 8843 e-mail: [email protected] Website: www.gagtl.ac.uk/gagtl President: Professor R.A. Howie Vice-Presidents: E.M. Bruton, A.E. Farn, D.G. Kent, R.K. Mitchell Honorary Fellows: R.A. Howie, R.T. Liddicoat Jnr, K. Nassau Honorary Life Members: D.J. Callaghan, E.A. Jobbins, H. Tillander Council of Management: C.R. Cavey, T.J. Davidson, N.W. Deeks, R.R. Harding, I. Thomson, V.P. Watson Members' Council: A.J. Allnutt, P. Dwyer-Hickey, S.A. Everitt, R. Fuller, A.G. Good, J. Greatwood, B. Jackson, J. Kessler, J. Monnickendam, L. Music, J.B. Nelson, P.G. Read, R. Shepherd, P.J. Wates, C.H. Winter Branch Chairmen: Midlands - G.M. Green, North West - I. Knight, Scottish - B. Jackson Examiners: A.J. Allnutt, M.Sc., Ph.D., FGA, S.M. Anderson, B.Sc. (Hons), FGA, L. Bartlett, B.Sc., MPhil., FGA, DGA, E.M. Bruton, FGA, DGA, C.R. Cavey, FGA, S. Coelho, B.Sc., FGA, DGA, Prof. A.T. Collins, B.Sc., Ph.D, A.G. Good, FGA, DGA, G.M. Howe, FGA, DGA, G.H. Jones, B.Sc., Ph.D., FGA, M. Newton, B.Sc., D.Phil., CJ.E. Oldershaw, B.Sc. (Hons), FGA, H.L. Plumb, B.Sc., FGA, DGA, R.D. Ross, B.Sc., FGA, DGA, P.A. Sadler, B.Sc., FGA, DGA, E. Stern, FGA, DGA, Prof. I. Sunagawa, D.Sc., M. Tilley, GG, FGA, C.M. Woodward, B.Sc., FGA, DGA The Journal of Gemmology Editor: Dr R.R. Harding Assistant Editors: M.J. O'Donoghue, P.G. Read Associate Editors: S.M. Anderson (Perth), Dr C.E.S. Arps (Leiden), G. Bosshart (Zurich), Prof. A.T. Collins (London), Dr J.W. Harris (Glasgow), Prof. R.A. Howie (Derbyshire), Dr J.M. Ogden (Cambridge), Prof. A.H. Rankin (Kingston upon Thames), Dr J.E. Shigley (Carlsbad), Prof. D.C. Smith (Paris), E. Stern (London), Prof. 1. Sunagawa (Tokyo), Dr M. Superchi (Milan), C.M. Woodward (London) Production Editor: M.A. Burland Vol 26, No. 3, July 1998 ISSN: 1355-4565 The colour of Igmerald: I.G. Farbenindustrie flux-grown synthetic emerald Dr Karl Schmetzer1 and Dr Lore Kiefert2 1. Marbacher Strasse 22b, D-85238 Petershausen, Germany 2. SSEF Swiss Gemmological Institute, CH-4001 Basel Switzerland ABSTRACT: Seven samples of I.G. Farbenindustrie flux-grown synthetic emerald were examined. The synthetic emeralds were grown between 1929 and 1942 at Bitterfeld, Germany in a lithium molybdate solvent. Gemmological, chemical and spectroscopic properties are given. The colour of the samples is caused by minor amounts of chromium and nickel and, thus, the secret ingredient mentioned by Espig (1960) is identified as a nickel-bearing compound. Introduction Webster, 1952, 1955, 1958; Wiegand, 1952; 145 Gübelin 1953; Eppler, 1958a,b). Regarding the Historical background growth technology used, there was only he first emerald synthesis which speculation until three more or less detailed produced facetable crystals above one papers of one of the inventors of the Tcentimetre in size was performed by I.G. Farbenindustrie process were published I.G. Farbenindustrie (literally I.G. Dye Trust) (Espig, 1960, 1961, 1962). Before this at Bitterfeld, Germany Facetable material information was available, the synthetic had been grown since 1929 (Schiebold, 1935; emeralds were considered as hydrothermally Espig, I960), but samples were released to grown (Webster, 1955,1958; Wilke 1956). the public only after the first announcement to the press in February 1935 (Anonymous, Growth technology 1935). Gemmological descriptions of this synthetic emerald were published in the Espig reported that the first attempts to same year (Eppler, 1935; Jaeger and Espig, grow synthetic emeralds at Bitterfeld started 1935; Anderson, 1935) and mineralogical in 1911 and that he was involved in these investigations of the synthetic emerald experiments from 1924. Crystal growth in the crystals, e.g. by X-ray powder diffraction, final stage of the technical development was were also performed (Schiebold, 1935; Espig, performed in platinum crucibles with 1935; Anderson, 1935). Gemmological lithium molybdate as the solvent. A properties of these synthetic emeralds were schematic drawing of the growth conditions examined later by various authors and their (Figure 1) which followed closely the results were summarized and compared descriptions of Espig was published by with the features of the first synthetic Recker (1973). A nutrient of BeO and A1203 emeralds produced in the United States by with lithium Chromate as colour-causing Chatham in different articles in the '50s (e.g. dopant was placed at the bottom of a © Gemmological Association and Gem Testing Laboratory of Great Britain ISSN: 1355-4565 2 ~~-H~~~~---8 ur~~~ l~~~~~1-ffif/~~-6 ~~~~~~~~~~---9 1~+-+-.,4--- 4 146 146 Figure 1: Schematic diagram diagram of ofthe the process process applied applied to fluX to fluxgrowth growth of synthetic of synthetic emerald emerald by I.G. by I.G. Farbenindustrie at at Bitterfeld, Bitterfeld, Germany, Germany, from from 1929 1929to 1942; to 1942;Key: 1 Key: = platinum 1 = platinum crucible, crucible,2 = platinum 2 = platinum lid, 3 = insulation,insulation, 4 4= = heating heating system, system, 5 = 5 central = central platinum platinum tube tubefor the for addition the addition of material of material to the to the nutrient, 6 = baffle,baffle, 7 7= = nutrient, nutrient, 8 =8 quartz= quartz plates, plates, 9 = 9 growing = growing crystals, crystals, 10 = 10lithium = lithium molybdate molybdate solvent (adapted(adapted from from Recker, Kecker, 1973). 1973). platinuplatinumm crucible.crucible. Subsequently,Subsequently, ththee cruciblecrucible 2 oror 3 emcm inin lengthlength (Espig,(Espig, 1960,1960, 1961,1961 , 1962).1962) . wawass fillefilledd witwithh lithiulithiumm molybdatemolybdate andand FaceteFacetedd stonesstones upup toto 1 ctct inin weightweight measuringmeasuring emeraldemerald seedsseeds werweree positionedpositioned belobeloww a 5 toto 6 mmmm werewere cutcut fromfrom thethe rough.rough. platinumplatinum baffle.baffle. AbovAbovee thithiss bafflebaffle,, quartzquartz EmeraldEmeraldss werweree produceproducedd atat BitterfelBitterfeldd fromfrom platesplates ofof 8 toto 1010 mmmm inin thicknessthickness werewere 19291929 untiluntil 19421942 in in 12 12 furnaces furnaces (Espig, (Espig ,1960), 1960) but, bu t arranged.arranged. TheseThese quartzquartz platesplates floatedfloated oonn toptop ofof duedue toto thethe marketmarket situationsituation forfor naturalnatural ththee meltmelt afterafter heatinheatingg thethe furnacefurnace toto a constantconstant emeraldsemeralds andand ththee relativelrelativelyy highighh coscostt ofof crystalcrystal temperaturetemperature ofof aboutabout 800°e.800°C ThisThis temperaturetemperature growth,growth, thertheree waswas nono large-scalelarge-scale industrialindustrial wawass kepkeptt atat a constantconstant levellevel overover a growthgrowth productioproductionn ooff syntheticsynthetic emeraldsemeralds atat thethe I.GLG.. periodperiod ooff 2020 days,days, butbut newnew nutrientnutrient waswas addedadded FarbenindustriFarbenindustrie(Anonymous,e (Anonymous, 1952;VV1egand,1952; Wiegand, everyevery secondsecond dayday bbyy meansmeans ofof a centralcentral 1952).1952). AsAs aa result,result, thethe syntheticsynthetic emeraldsemeralds werewere platinuplatinumm tubetube ttoo ththee materialmaterial atat thethe bottombottom ooff nevernever soldsold commerciallycommercially onon ththee freefree market.market. ththee crucible.crucible. AfteAfterr eacheach growthgrowth periodperiod,, thethe TheThe materialmaterial waswas namednamed Igmerald,Igmerald, standingstanding syntheticsynthetic emeraldemerald crystalscrystals werewere examinedexamined andand forfor I.GI.G.. emerald,emerald, andand waswas used forfor publicpublic extremelyextremely impureimpure layerslayers ofof syntheticsynthetic emeraldemerald relationsrelations purposepurposess ofof thethe I.G.LG. Farbenindustrie.Farbenindustrie. materiamateriall werewere removed.removed. TheThe largestlargest crystalscrystals ooff InIn 1945,1945, thethe completecomplete platinuplatinumm growthgrowth prismaticprismatic habithabit whichwhich werewere obtainedobtained iinn aboutabout facilitiesfacilities werweree lostlost andand productioproductionn waswas notnot 1818 growthgrowth periodsperiods duringduring oneone yearyear measuredmeasured resumedresumed afterafter thethe war.war. J.J. Gemm.,Gemm .• 1998,26,3,145-1551998, 26, 3, 145-155 Colour of of Igmerald Igmeral d 1980;1980; NassauNassau andand Nassau,Nassau, 1980).1980). ThisThis AlthoughAlthough thethe basibasicc technologytechnology ofof emeraldemerald assumptionassumption wawass acceptedaccepted byby otherother scientistsscientists productioproductionn hahass beenbeen availableavailable toto ththee publicpublic (see(see e.g.e.g. Elwell,Elwell, 1979)1979) andand seemsseems reasonable,reasonable, sincesince 1960,I960, a fewfew sentencessentences inin thethe firstfirst ofof thethe becausebecause syntheticsynthetic greengreen 'emeralds''emeralds' whichwhich threethree paperspapers byby EspiEspigg ledled toto somesome speculation:speculation: werewere colouredcoloured bbyy vanadiumvanadium hadhad alreadyalready 'Zwar'Zwar stehtsteht iinn allenallen Lehrbiichern,Lehrbüchern, daISdaß beenbeen mentionedmentioned inin 19261926 bbyy BernauerBernauer (in(in a SmaragdSmaragd durehdurch ChromoyxdChromoyxd gefarbtgefärbt istist unundd inin paperpaper dealingdealing withwith trapichtrapichee emeraldsemeralds fromfrom derder
Recommended publications
  • Amber with Mite Inclusion
    Editor Nathan Renfro Contributing Editors Elise A. Skalwold and John I. Koivula The purpose of this new quarterly column in Gems & may seem elusive, even daunting. Continual practice, care- Gemology is to encourage the appreciation of inclusions ful observation, and patience will refine both technique and in forensic gemology and to help build the observational interpretive prowess for both new and experienced inclu- skill set of the practicing gemologist. By providing concise sionists. Observation through the microscope serves as the information and vividly clear photomicrographs and pho- very foundation for many conclusions drawn on a speci- tomacrographs of new or otherwise interesting inclusion men. This can include identification, treatment detection, specimens, the column aims to narrow the knowledge gap separation of natural and synthetic materials, and geo- between advanced inclusionists and gemologists working graphic origin—even secrets of a gem’s genesis and the se- in mainstream general practice. crets of the earth’s depths may ultimately be revealed. The micro-world of gems lies at the very core of gemol- In building proficiency of the micro-world through this ogy. Sometimes its nature contributes to the allure of a column, readers will also expand their personal knowledge gem, as is the case with such coveted gems as sunstones, base and ability with a microscope. Mastery of microscopy, star sapphires, and cat’s-eye chrysoberyls. At other times combined with at least a basic grasp of mineralogy, is es- that world may seem a dreadful distraction to an otherwise sential for understanding the nature of gems and the geo- beautiful, marketable specimen.
    [Show full text]
  • 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
    [Show full text]
  • Taaffeite, a New Beryllium Mineral, Found As a Cut Gem- Stone.I
    765 Taaffeite, a new beryllium mineral, found as a cut gem- stone.I By B. W. ANDERSON,B.Sc., F.C.S., C. J. PAYNE, B.Sc. Laboratory of the Diamond, Pearl, and Precious Stone Trade Section of the London Chamber of Commerce. and G. F. CLARINGBULL,B.Sc., Ph.D., F.G.S. With microchemical analysis by M. H. HEY, M.A., D.Sc. Department of Mineralogy, British Museum. [Read June 7, 1951.] ------ N October 1945 Count Taaffe,2 a brilliant if unorthodox Dublin I gemmologist, in the course of examining a motley collection of gem- stones, came across a small mauve stone which puzzled him greatly. The stone had the appearance, and most of the characters, of spinel, but afforded clear evidence of double refraction. As recounted below, this stone was later found to belong to an entirely new mineral species-the only c~se hitherto known where a mineral has been first encountered as a faceted gem. Since the precise circumstances of such a discovery have both human and technical interest, it seemed best to obtain from Count Taaffe his own account of the event. This is accordingly given below before pro- ceeding to the more formal presentation of the data on the new mineral, which has been named taaffeite in honour of its discoverer. On one of my rounds in search of gems I came to Mr. Robert Dobbie, watchmaker and working jeweller in Fleet Street, Dublin; he allowed me in his genial way to go through all his boxes in which he kept stones, to pick out any that were real-most of them were glass-and to make him an offer for them.
    [Show full text]
  • Alphab Etical Index
    ALPHAB ETICAL INDEX Names of authors are printed in SMALLCAPITALS, subjects in lower-case roman, and localities in italics; book reviews are placed at the end. ABDUL-SAMAD, F. A., THOMAS, J. H., WILLIAMS, P. A., BLASI, A., tetrahedral A1 in alkali feldspar, 465 and SYMES, R. F., lanarkite, 499 BORTNIKOV, N. S., see BRESKOVSKA, V. V., 357 AEGEAN SEA, Santorini I., iron oxide mineralogy, 89 Boulangerite, 360 Aegirine, Scotland, in trachyte, 399 BRAITHWAITE, R. S. W., and COOPER, B. V., childrenite, /~kKERBLOM, G. V., see WILSON, M. R., 233 119 ALDERTON, D. H. M., see RANKIN, A. H., 179 Braunite, mineralogy and genesis, 506 Allanite, Scotland, 445 BRESKOVSKA, V. V., MOZGOVA, N. N., BORTNIKOV, N. S., Aluminosilicate-sodalites, X-ray study, 459 GORSHKOV, A. I., and TSEPIN, A. I., ardaite, 357 Amphibole, microstructures and phase transformations, BROOKS, R. R., see WATTERS, W. A., 510 395; Greenland, 283 BULGARIA, Madjarovo deposit, ardaite, 357 Andradite, in banded iron-formation assemblage, 127 ANGUS, N. S., AND KANARIS-SOTIRIOU, R., autometa- Calcite, atomic arrangement on twin boundaries, 265 somatic gneisses, 411 CANADA, SASKATCHEWAN, uranium occurrences in Cree Anthophyllite, asbestiform, morphology and alteration, Lake Zone, 163 77 CANTERFORD, J. H., see HILL, R. J., 453 Aragonite, atomic arrangements on twin boundaries, Carbonatite, evolution and nomenclature, 13 265 CARPENTER, M. A., amphibole microstructures, 395 Ardaite, Bulgaria, new mineral, 357 Cassiterite, SW England, U content, 211 Arfvedsonite, Scotland, in trachyte, 399 Cebollite, in kimberlite, correction, 274 ARVlN, M., pumpellyite in basic igneous rocks, 427 CHANNEL ISLANDS, Guernsey, meladiorite layers, 301; ASCENSION ISLAND, RE-rich eudialyte, 421 Jersey, wollastonite and epistilbite, 504; mineralization A TKINS, F.
    [Show full text]
  • Sugilite in Manganese Silicate Rocks from the Hoskins Mine and Woods Mine, New South Wales, Australia
    Sugilite in manganese silicate rocks from the Hoskins mine and Woods mine, New South Wales, Australia Y. KAWACHI Geology Department, University of Otago, P.O.Box 56, Dunedin, New Zealand P. M. ASHLEY Department of Geology and Geophysics, University of New England, Armidale, NSW 2351, Australia D. VINCE 1A Ramsay Street, Essendon, Victoria 3040, Australia AND M. GOODWIN P.O.Bo• 314, Lightning Ridge, NSW 2834, Australia Abstract Sugilite relatively rich in manganese has been found at two new localities, the Hoskins and Woods mines in New South Wales, Australia. The occurrences are in manganese-rich silicate rocks of middle to upper greenschist facies (Hoskins mine) and hornblende hornfels facies (Woods mine). Coexisting minerals are members of the namansilite-aegirine and pectolite-serandite series, Mn-rich alkali amphiboles, alkali feldspar, braunite, rhodonite, tephroite, albite, microcline, norrishite, witherite, manganoan calcite, quartz, and several unidentified minerals. Woods mine sugilite is colour-zoned with pale mauve cores and colourless rims, whereas Hoskins mine sugilite is only weakly colour-zoned and pink to mauve. Within single samples, the chemical compositions of sugilite from both localities show wide ranges in A1 contents and less variable ranges of Fe and Mn, similar to trends in sugilite from other localities. The refractive indices and cell dimensions tend to show systematic increases progressing from Al-rich to Fe- Mn-rich. The formation of the sugilite is controlled by the high alkali (especially Li) and manganese contents of the country rock, reflected in the occurrences of coexisting high alkali- and manganese- bearing minerals, and by high fo2 conditions. KEYWORDS: sugilite, manganese silicate rocks, milarite group, New South Wales, Australia Introduction Na2K(Fe 3 +,Mn 3 +,Al)2Li3Sit2030.
    [Show full text]
  • Petrology of Nepheline Syenite Pegmatites in the Oslo Rift, Norway: Zr and Ti Mineral Assemblages in Miaskitic and Agpaitic Pegmatites in the Larvik Plutonic Complex
    MINERALOGIA, 44, No 3-4: 61-98, (2013) DOI: 10.2478/mipo-2013-0007 www.Mineralogia.pl MINERALOGICAL SOCIETY OF POLAND POLSKIE TOWARZYSTWO MINERALOGICZNE __________________________________________________________________________________________________________________________ Original paper Petrology of nepheline syenite pegmatites in the Oslo Rift, Norway: Zr and Ti mineral assemblages in miaskitic and agpaitic pegmatites in the Larvik Plutonic Complex Tom ANDERSEN1*, Muriel ERAMBERT1, Alf Olav LARSEN2, Rune S. SELBEKK3 1 Department of Geosciences, University of Oslo, PO Box 1047 Blindern, N-0316 Oslo Norway; e-mail: [email protected] 2 Statoil ASA, Hydroveien 67, N-3908 Porsgrunn, Norway 3 Natural History Museum, University of Oslo, Sars gate 1, N-0562 Oslo, Norway * Corresponding author Received: December, 2010 Received in revised form: May 15, 2012 Accepted: June 1, 2012 Available online: November 5, 2012 Abstract. Agpaitic nepheline syenites have complex, Na-Ca-Zr-Ti minerals as the main hosts for zirconium and titanium, rather than zircon and titanite, which are characteristic for miaskitic rocks. The transition from a miaskitic to an agpaitic crystallization regime in silica-undersaturated magma has traditionally been related to increasing peralkalinity of the magma, but halogen and water contents are also important parameters. The Larvik Plutonic Complex (LPC) in the Permian Oslo Rift, Norway consists of intrusions of hypersolvus monzonite (larvikite), nepheline monzonite (lardalite) and nepheline syenite. Pegmatites ranging in composition from miaskitic syenite with or without nepheline to mildly agpaitic nepheline syenite are the latest products of magmatic differentiation in the complex. The pegmatites can be grouped in (at least) four distinct suites from their magmatic Ti and Zr silicate mineral assemblages.
    [Show full text]
  • Chemical Composition and Petrogenetic Implications of Eudialyte-Group Mineral in the Peralkaline Lovozero Complex, Kola Peninsula, Russia
    minerals Article Chemical Composition and Petrogenetic Implications of Eudialyte-Group Mineral in the Peralkaline Lovozero Complex, Kola Peninsula, Russia Lia Kogarko 1,* and Troels F. D. Nielsen 2 1 Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, 119991 Moscow, Russia 2 Geological Survey of Denmark and Greenland, 1350 Copenhagen, Denmark; [email protected] * Correspondence: [email protected] Received: 23 September 2020; Accepted: 16 November 2020; Published: 20 November 2020 Abstract: Lovozero complex, the world’s largest layered peralkaline intrusive complex hosts gigantic deposits of Zr-, Hf-, Nb-, LREE-, and HREE-rich Eudialyte Group of Mineral (EGM). The petrographic relations of EGM change with time and advancing crystallization up from Phase II (differentiated complex) to Phase III (eudialyte complex). EGM is anhedral interstitial in all of Phase II which indicates that EGM nucleated late relative to the main rock-forming and liquidus minerals of Phase II. Saturation in remaining bulk melt with components needed for nucleation of EGM was reached after the crystallization about 85 vol. % of the intrusion. Early euhedral and idiomorphic EGM of Phase III crystalized in a large convective volume of melt together with other liquidus minerals and was affected by layering processes and formation of EGM ore. Consequently, a prerequisite for the formation of the ore deposit is saturation of the alkaline bulk magma with EGM. It follows that the potential for EGM ores in Lovozero is restricted to the parts of the complex that hosts cumulus EGM. Phase II with only anhedral and interstitial EGM is not promising for this type of ore.
    [Show full text]
  • Asbestos Fibers and Other Elongate Mineral Particles: State of the Science and Roadmap for Research
    CURRENT INTELLIGENCE BULLETIN 62 Asbestos Fibers and Other Elongate Mineral Particles: State of the Science and Roadmap for Research Revised Edition DEPARTMENT OF HEALTH AND HUMAN SERVICES Centers for Disease Control and Prevention National Institute for Occupational Safety and Health Cover Photograph: Transitional particle from upstate New York identified by the United States Geological Survey (USGS) as anthophyllite asbestos altering to talc. Photograph courtesy of USGS. CURRENT INTELLIGENCE BULLETIN 62 Asbestos Fibers and Other Elongate Mineral Particles: State of the Science and Roadmap for Research DEPARTMENT OF HEALTH AND HUMAN SERVICES Centers for Disease Control and Prevention National Institute for Occupational Safety and Health This document is in the public domain and may be freely copied or reprinted. Disclaimer Mention of any company or product does not constitute endorsement by the Na- tional Institute for Occupational Safety and Health (NIOSH). In addition, citations to Web sites external to NIOSH do not constitute NIOSH endorsement of the spon- soring organizations or their programs or products. Furthermore, NIOSH is not responsible for the content of these Web sites. Ordering Information To receive NIOSH documents or other information about occupational safety and health topics, contact NIOSH at Telephone: 1–800–CDC–INFO (1–800–232–4636) TTY: 1–888–232–6348 E-mail: [email protected] or visit the NIOSH Web site at www.cdc.gov/niosh. For a monthly update on news at NIOSH, subscribe to NIOSH eNews by visiting www.cdc.gov/niosh/eNews. DHHS (NIOSH) Publication No. 2011–159 (Revised for clarification; no changes in substance or new science presented) April 2011 Safer • Healthier • PeopleTM ii Foreword Asbestos has been a highly visible issue in public health for over three decades.
    [Show full text]
  • New Minerals Approved Bythe Ima Commission on New
    NEW MINERALS APPROVED BY THE IMA COMMISSION ON NEW MINERALS AND MINERAL NAMES ALLABOGDANITE, (Fe,Ni)l Allabogdanite, a mineral dimorphous with barringerite, was discovered in the Onello iron meteorite (Ni-rich ataxite) found in 1997 in the alluvium of the Bol'shoy Dolguchan River, a tributary of the Onello River, Aldan River basin, South Yakutia (Republic of Sakha- Yakutia), Russia. The mineral occurs as light straw-yellow, with strong metallic luster, lamellar crystals up to 0.0 I x 0.1 x 0.4 rnrn, typically twinned, in plessite. Associated minerals are nickel phosphide, schreibersite, awaruite and graphite (Britvin e.a., 2002b). Name: in honour of Alia Nikolaevna BOG DAN OVA (1947-2004), Russian crys- tallographer, for her contribution to the study of new minerals; Geological Institute of Kola Science Center of Russian Academy of Sciences, Apatity. fMA No.: 2000-038. TS: PU 1/18632. ALLOCHALCOSELITE, Cu+Cu~+PbOZ(Se03)P5 Allochalcoselite was found in the fumarole products of the Second cinder cone, Northern Breakthrought of the Tolbachik Main Fracture Eruption (1975-1976), Tolbachik Volcano, Kamchatka, Russia. It occurs as transparent dark brown pris- matic crystals up to 0.1 mm long. Associated minerals are cotunnite, sofiite, ilin- skite, georgbokiite and burn site (Vergasova e.a., 2005). Name: for the chemical composition: presence of selenium and different oxidation states of copper, from the Greek aA.Ao~(different) and xaAxo~ (copper). fMA No.: 2004-025. TS: no reliable information. ALSAKHAROVITE-Zn, NaSrKZn(Ti,Nb)JSi401ZJz(0,OH)4·7HzO photo 1 Labuntsovite group Alsakharovite-Zn was discovered in the Pegmatite #45, Lepkhe-Nel'm MI.
    [Show full text]
  • Articles Devoted to Silicate Minerals from Fumaroles of the Tol- Bachik Volcano (Kamchatka, Russia)
    Eur. J. Mineral., 32, 101–119, 2020 https://doi.org/10.5194/ejm-32-101-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Unusual silicate mineralization in fumarolic sublimates of the Tolbachik volcano, Kamchatka, Russia – Part 1: Neso-, cyclo-, ino- and phyllosilicates Nadezhda V. Shchipalkina1, Igor V. Pekov1, Natalia N. Koshlyakova1, Sergey N. Britvin2,3, Natalia V. Zubkova1, Dmitry A. Varlamov4, and Eugeny G. Sidorov5 1Faculty of Geology, Moscow State University, Vorobievy Gory, 119991 Moscow, Russia 2Department of Crystallography, St Petersburg State University, University Embankment 7/9, 199034 St. Petersburg, Russia 3Kola Science Center of Russian Academy of Sciences, Fersman Str. 14, 184200 Apatity, Russia 4Institute of Experimental Mineralogy, Russian Academy of Sciences, Academica Osypyana ul., 4, 142432 Chernogolovka, Russia 5Institute of Volcanology and Seismology, Far Eastern Branch of Russian Academy of Sciences, Piip Boulevard 9, 683006 Petropavlovsk-Kamchatsky, Russia Correspondence: Nadezhda V. Shchipalkina ([email protected]) Received: 19 June 2019 – Accepted: 1 November 2019 – Published: 29 January 2020 Abstract. This is the initial paper in a pair of articles devoted to silicate minerals from fumaroles of the Tol- bachik volcano (Kamchatka, Russia). These papers contain the first systematic data on silicate mineralization of fumarolic genesis. In this article nesosilicates (forsterite, andradite and titanite), cyclosilicate (a Cu,Zn- rich analogue of roedderite), inosilicates (enstatite, clinoenstatite, diopside, aegirine, aegirine-augite, esseneite, “Cu,Mg-pyroxene”, wollastonite, potassic-fluoro-magnesio-arfvedsonite, potassic-fluoro-richterite and litidion- ite) and phyllosilicates (fluorophlogopite, yanzhuminite, “fluoreastonite” and the Sn analogue of dalyite) are characterized with a focus on chemistry, crystal-chemical features and occurrence.
    [Show full text]
  • MINERALOGY for PETROLOGISTS Comprising a Guidebook and a Full Color CD-ROM, This Reference Set Offers Illustrated Essentials to Study Mineralogy, Applied to Petrology
    MINERALOGY for PETROLOGISTS for MINERALOGY Comprising a guidebook and a full color CD-ROM, this reference set offers illustrated essentials to study mineralogy, applied to petrology. While there are some excellent reference works available on this subject, this work is unique for its data richness and its visual character. MINERALOGY for PETROLOGISTS With a collection of images that excels both in detail and aesthetics, 151 minerals are presented in more than 400 plates. Different facies and paragenesis, both in natural polarized light, are shown for every mineral and optical data, sketches of the crystal habitus, chemical composition, occurrence and a brief description are Optics, Chemistry and Occurrences included. The accompanying user guide gives a general introduction to microscope mineral observation, systematic mineralogy, mineral chemistry, occurrence, of Rock-Forming Minerals stability, paragenesis, structural formula calculation and its use in petrology. This compact set will serve as a field manual to students, researchers and Michel Demange professionals in geology, geological, mining, and mineral resources engineering to observe and determine minerals in their studies or field work. Dr. Michel Demange has devoted his career to regional geology and tectonics of metamorphic and magmatic terranes and to ore deposits. Graduated from the École Nationale Supérieure des Mines de Paris and holding a Docteur-es-Sciences from the University Pierre et Marie Curie, Paris VI, he has been active in a rich variety of geological projects and investigations around the world. In combination with his teaching and research activities at the École des Mines in Paris, France, he headed various research studies. This book benefits from the great experience in field M.
    [Show full text]
  • A Comparative Study of Jadeite, Omphacite and Kosmochlor Jades from Myanmar, and Suggestions for a Practical Nomenclature
    Feature Article A Comparative Study of Jadeite, Omphacite and Kosmochlor Jades from Myanmar, and Suggestions for a Practical Nomenclature Leander Franz, Tay Thye Sun, Henry A. Hänni, Christian de Capitani, Theerapongs Thanasuthipitak and Wilawan Atichat Jadeitite boulders from north-central Myanmar show a wide variability in texture and mineral content. This study gives an overview of the petrography of these rocks, and classiies them into ive different types: (1) jadeitites with kosmochlor and clinoamphibole, (2) jadeitites with clinoamphibole, (3) albite-bearing jadeitites, (4) almost pure jadeitites and (5) omphacitites. Their textures indicate that some of the assemblages formed syn-tectonically while those samples with decussate textures show no indication of a tectonic overprint. Backscattered electron images and electron microprobe analyses highlight the variable mineral chemistry of the samples. Their extensive chemical and textural inhomogeneity renders a classiication by common gemmological methods rather dificult. Although a deinitive classiication of such rocks is only possible using thin-section analysis, we demonstrate that a fast and non-destructive identiication as jadeite jade, kosmochlor jade or omphacite jade is possible using Raman and infrared spectroscopy, which gave results that were in accord with the microprobe analyses. Furthermore, current classiication schemes for jadeitites are reviewed. The Journal of Gemmology, 34(3), 2014, pp. 210–229, http://dx.doi.org/10.15506/JoG.2014.34.3.210 © 2014 The Gemmological Association of Great Britain Introduction simple. Jadeite jade is usually a green massive The word jade is derived from the Spanish phrase rock consisting of jadeite (NaAlSi2O6; see Ou Yang, for piedra de ijada (Foshag, 1957) or ‘loin stone’ 1999; Ou Yang and Li, 1999; Ou Yang and Qi, from its reputed use in curing ailments of the loins 2001).
    [Show full text]