J the Journal of L \ A, If» R

Total Page:16

File Type:pdf, Size:1020Kb

J the Journal of L \ A, If» R j The Journal of l \ A, if» r Volumemmoie 27 Noemmoiemmoi. 3 oVolum e 2 •-••^ppsgiiiWJigpy^PW 5I>us8rtlne ? '"? ^" Gansof samets Somaliland'JoiiKiliUiiKl InJ/J NlsertajJJ£i2/J:i ,WT'^ T/j'i rJ;j;j/]'iif]ü;j The cau.eof j'iüJYüCtoj/rii'ir colour of alexandrlte. The Gemmological Association and Gem Testing Laboratory of Great Britain Gemmological Association and Gem Testing Laboratory of Great Britain 27 Greville Street, London EC1N 8TN Tel: 020 7404 3334 Fax: 020 7404 8843 e-mail: [email protected] Website: www.gagtl.ac.uk/gagtl President: Professor A.T. Collins Vice-Presidents: E.M. Bruton, A.E. Farn, R.A. Howie, D.G. Kent, R.K. Mitchell Honorary Fellows: Chen Zhonghui, R.A. Howie, R.T. Liddicoat Jnr, K. Nassau Honorary Life Members: H. Bank, D.J. Callaghan, E.A. Jobbins, H. Tillander Council of Management: T.J. Davidson, N.W. Deeks, R.R. Harding, I. Mercer, J. Monnickendam, M.J. O'Donoghue, E. Stern, I. Thomson, V.P Watson Members' Council: A.J. Allnutt, P. Dwyer-Hickey, S.A. Everitt, A.G. Good, J. Greatwood, B. Jackson, L. Music, J.B. Nelson, P.G. Read, P.J. Wates, C.H. Winter Branch Chairmen: Midlands - G.M. Green, North West -1. Knight, Scottish - B. Jackson Examiners: A.J. Allnutt, M.Sc, Ph.D., FGA, L. Bartlett, B.Sc, M.Phil., FGA, DGA, E.M. Bruton, FGA, DGA, S. Coelho, B.Sc, FGA, DGA, Prof. A.T. Collins, B.Sc, Ph.D, A.G. Good, FGA, DGA, J. Greatwood, FGA, G.M. Howe, FGA, DGA, Li Li Ping, FGA, DGA, B. Jackson, FGA, DGA, G.H. Jones, B.Sc, Ph.D., FGA, M. Newton, B.Sc, D.Phil., C.J.E. Oldershaw, B.Sc (Hons), FGA, DGA, 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, S.M. Stocklmayer, B.Sc. (Hons), FGA, Prof. I. Sunagawa, D.Sc, M. Tilley, GG, FGA, CM. 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: 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 (Hildesheim), Prof. A.H. Rankin (Kingston upon Thames), Dr J.E. Shigley (Carlsbad), Prof. D.C. Smith (Paris), E. Stern (London), Prof. I. Sunagawa (Tokyo), Dr M. Superchi (Milan), CM. Woodward (London) Production Editor: M.A. Burland Vol 27, No. 3, July 2000 ISSN: 1355-4565 AA neneww finfindd ooff spessartinspessartinee garnetgarnetss iinn NigeriNigeriaa ThomaThomass LinLindd anandd UlricUlrichh HenHennn GermanGerman GemmologicalGemmological Association,Association, Idar-Oberstein,Idar-Oberstein, GermanyGermany ABSTRACT:ABSTRACT: ThThee physico-chemicaphysico-chemical l anandd microscopimicroscopicc featurefeaturess ooff spessartinspessartinee garnetgarnetss frofromm aa neneww occurrencoccurrencee iinn NigeriNigeriaa araree presentedpresented. ChemicaChemical l analyseanalysess shoshoww thathat t thesthesee garnetgarnetss havhavee aa ververyy highighh spessartinspessartinee componencomponent t ooff 89-9589-95%% witwithh varyinvaryingg smalsmall l amountamountss ooff pyroppyropee anandd almandinealmandine. VariatioVariationn ooff ththee almandinalmandinee componencomponent t betweebetweenn 11%% anandd 66%% iiss responsiblresponsiblee foforr aa variatiovariationn ooff colourcolourss betweebetweenn yellowyellow, , goldegoldenn yelloyelloww anandd brown-orangebrown-orange. AbsorptioAbsorptionn spectrspectraa ooff ththee yelloyelloww anandd goldegoldenn yelloyelloww specimenspecimenss (typ(typee aa spectraspectra)) araree ververyy similasimilarr ttoo thosthosee ooff spessartinspessartinee frofromm KunenKunenee (Namibia)(Namibia), , whilwhilee thosthosee ooff brown-orangbrown-orangee coloucolourr (typ(typee bb spectraspectra)) araree similasimilarr ttoo thosthosee frofromm RamonRamonaa (USA)(USA). ThThee maimainn inclusioninclusionss iinn ththee NigeriaNigeriann spessartinespessartiness araree healehealedd crackcrackss representinrepresentingg thithinn liquid-filleliquid-filledd cavitiecavitiess oorr fingerprint-typfingerprint-typee feathersfeathers. Keywords:Keywords: spessartinspessartinee garnetgarnet, , NigeriaNigeria, , physico-chemicaphysico-chemical l propertiesproperties, , internainternal l characteristiccharacteristicss 129 IntroductioIntroductionn spessartinspessartinee garnetsgarnets. ThesThesee gegemm garnetgarnetss werweree firsfirst t designedesignedd aass 'Kunen'Kunenee spessartinespessartine' ' afteafterr pessartinpessartinee garnetgarnetss ooff gegemm qualitqualityy araree ththee boundarboundaryy riveriverr betweebetweenn NamibiNamibiaa anandd relativelrelativelyy rarraree comparecomparedd ttoo otheotherr AngolaAngola, , bubut t becambecamee widelwidelyy knowknownn iinn ththee SSspeciespeciess ooff ththee garnegarnet t solisolidd solutiosolutionn jewellerjewelleryy industrindustryy undeunderr ththee tradtradee namnamee seriesseries. BotBothh quantitquantityy anandd qualitqualityy ooff ththee 'mandari'mandarinn garnet'garnet'. materiamaterial l frofromm differendifferent t sourcesourcess sucsuchh aass RamonRamonaa CountyCounty, , CaliforniaCalifornia, , MacoMaconn CountyCounty, , VirginiaVirginia, , MinaMinass GeraisGerais, , BrazilBrazil, , MadagascarMadagascar, , SrSrii LankLankaa anandd KenyaKenya, , havhavee beebeenn ververyy erraticerratic, , anandd thereforthereforee spessartinspessartinee garnetgarnetss havhavee beebeenn aa collector'collector'ss gemstongemstonee ratheratherr thathann aa stonstonee suitablsuitablee foforr jewellerjewelleryy industrindustryy purposespurposes. ThiThiss wholwholee picturpicturee changedchanged, , whewhenn iinn 19919922 aann occurrencoccurrencee ooff spessartinspessartinee garnegarnet t wawass discoverediscoveredd oonn ththee northernorthernn edgedgee ooff NamibiaNamibia, , neanearr ththee bordeborderr witwithh AngolAngolaa (Lin(Lindd etet ah,ah, 1993,1994)1993,1994). ThThee materiamaterial l frofromm thithiss occurrencoccurrencee iiss ooff aa finefine, , brighbright t orangorangee coloucolourr whicwhichh iiss easileasilyy FigureFigure 1:1: Cut Cut spessartinespessartine garnet garnet ofof 2.68 2.68 ctctfrom from distinguishedistinguishedd frofromm alall l hitherthithertoo knowknownn aa new new occurrenceoccurrence in in Nigeria.Nigeria. ©© Gemmologica Gemmological l AssociatioAssociationn anandd GeGemm TestinTestingg Laborator Laboratoryy oof f GreaGreat t BritaiBritainn ISSNISSN: : 1355-4561355-45655 Production from this source has been Composition continuous, and has made spessartine Garnets are a group of minerals with garnets popular among gem dealers and extended isomorphous solid solution jewellers. Unfortunately, sizes of cut stones between its end members. Although solid generally are small, and faceted gems of solution of five and more components is more than 1 ct are already relatively rare. For common, usually 80% of the crystal is built sizes of 2-3 cts and up, a regular supply up of only two or three main constituents, cannot be maintained, even at high prices. and all garnets can be broadly subdivided Recently, a new source of gem quality into the two solid solution series ugrandite garnets of fine yellow-orange colour was (with end members uvarovite, grossularite discovered in Nigeria, West Africa (Bank et and andradite) and pyralspite (with end al., 1999). The material from this new members pyrope, almandine and occurrence complements the range of sizes spessartine). available for fine orange spessartine garnets, Pyralspite garnets with spessartine being as sizes of 2-3 ct and more can now be the main component are called spessartine in supplied to jewellers (Figure 1). Table II: Microprobe analyses of spessartine garnets Refractive index and specific gravity from Nigeria. Refractive indices of 20 specimens were Hgr324 ligr325 Ugr326 Hgr327 measured using a Rayner refractometer and fluid with an RI of 1.81 and the results varied wt% between 1.801 and 1.803. Specific gravities MgO 0.67 0.99 0.96 0.85 measured using the hydrostatic method 129 varied between 4.15 and 4.22. FeO 0.62 2.77 1.44 2.44 CaO 0.27 0.09 0.19 0.35 Table I compares values of measured gemmological data for spessartine garnets MnO 40.38 37.67 39.36 37.76 from Nigeria with values for spessartine garnets from other occurrences described in 21.21 21.40 21.48 the literature. A1203 21.36 Table I: RI values and SG values for gem quality Fe203 0.00 0.00 0.00 0.00 spessartine garnets from Nigeria compared with v2o3 0.00 0.00 0.00 0.00 published work. Cr203 0.07 0.03 0.05 0.02 Locality n SG 6 Nigeria 1.801-1.803 4.15-4.22 Ti02 0.07 0.01 0.08 0.09 Rutherford Mine, 1.802(3) - Si02 36.68 37.04 36.55 37.02 Virginia1 Total 99.97 100.00 99.99 100.01 Taita Hills, Kenya2 1.795-1.809 - Minas Gerais, Brazil3 1.803-1.805 4.15 Mol% Ramona, Calif.4 >1.81 4.17 Pyrope 2.8 4.1 3.9 3.5 Kunene, Namibia5 1.801-1.803 4.15-4.22 Almandine 1.4 6.5 3.3 5.7 1. Sinkankas and Ried, 1966 Spessartine 95.0 89.1 92.1 89.7 2. Medenbach et al, 1978 3. Bank et al, 1970 Grossular 0.6 0.2 0.4 1.0 4. Tisdall, 1962 5. Lind et al, 1993,1994 Uvarovite 0.2 0.1 0.2 0.1 6. this work /. Gemm., 2000, 27, 3, 129-132 the trade. Gem-quality spessartine garnets are usually members of two mainly binary Relevant sector of ternary pyralspite diagram solid-solution series: for spessartine from Nigeria • spessartine var. sources 1. spessartine-almandine series (pyrope A spessartine Nigeria (this paper) and grossular < 10%); • spessartine Namibia (Kunene) 2. spessartine-pyrope series (almandine and grossular < 15%); Sp 100% (see Sinkankas and Ried, 1966, Bank et al, 1970, Jobbins et al, 1977, Medenbach et al, 1978, and Lind et al, 1993,1994). Compositions of spessartines
Recommended publications
  • 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]
  • Thomas, R., Rericha, A., Pohl, WL, Davidson, P
    Originally published as: Thomas, R., Rericha, A., Pohl, W. L., Davidson, P. (2018): Genetic significance of the 867 cm−1 out-of- plane Raman mode in graphite associated with V-bearing green grossular. - Mineralogy and Petrology, 112, 5, pp. 633—645. DOI: http://doi.org/10.1007/s00710-018-0563-1 1 Genetic significance of the 867 cm-1 out-of-plane Raman mode in graphite associated with V-bearing green grossular Rainer Thomasa Adolf Rerichab Walter L. Pohlc Paul Davidsond Paul Davidson [email protected] 0000-0002-6129-0748 a Helmholtz-Centre Potsdam, German Research Centre for Geoscience – GFZ, Section 4.3. Chemistry and Physics of Earth Materials, Telegrafenberg, D-14473 Potsdam, Germany b Alemannenstr. 4a, D-14612 Falkensee, Germany c Austrian Academy of Sciences, Dr. Ignaz Seipel-Platz 2, 1010 Vienna, Austria d ARC Centre of Excellence in Ore Deposits, University of Tasmania, Hobart 7001, Australia Keywords: Tsavorite Green V-grossular Graphite Raman scattering Fluid and melt inclusions Sulfur 2 Abstract SE Kenya is the world’s largest producer of green vanadium grossular gemstones (tsavorite). Samples from one of the mines near Mwatate, and of occurrences in Tanzania yielded remarkable new insights into the genesis of tsavorite. Graphite is intimately associated with V-grossular and is one of the keys to understanding its origin. In the course of this study we found five different types of graphite. Surprisingly, in one graphite type the “Raman- forbidden” and IR-active 867 cm-1 band was observed. In this communication, we attempt to find an explanation for this unusual phenomenon.
    [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]
  • Download the Scanned
    American Mineralogist, Volume 77, pages 670475, 1992 NEW MINERAL NAMES* JonN L. J,Annson CANMET, 555 Booth Street,Ottawa, Ontario KIA OGl' Canada Abswurmbachite* rutile, hollandite, and manganoan cuprian clinochlore. The new name is for Irmgard Abs-Wurmbach, in recog- T. Reinecke,E. Tillmanns, H.-J. Bernhardt (1991)Abs- her contribution to the crystal chemistry, sta- wurmbachite, Cu'?*Mnl*[O8/SiOo],a new mineral of nition of physical properties ofbraunite. Type the braunite group: Natural occurrence,synthesis, and bility relations, and crystal structure.Neues Jahrb. Mineral. Abh., 163,ll7- material is in the Smithsonian Institution, Washington, r43. DC, and in the Institut fiir Mineralogie, Ruhr-Universitlit Bochum, Germany. J.L.J. The new mineral and cuprian braunit€ occur in brown- ish red piemontite-sursassitequartzites at Mount Ochi, near Karystos, Evvia, Greece, and in similar quartzites on the Vasilikon mountains near Apikia, Andros Island, Barstowite* Greece.An electron microprobe analysis (Andros mate- C.J. Stanley,G.C. Jones,A.D. Hart (1991) Barstowite, gave SiO, 9.8, TiO, rial; one of six for both localities) 3PbClr'PbCOr'HrO, a new mineral from BoundsClifl 0.61,Al,O3 0.60, Fe'O, 3.0,MnrO. 71.3,MgO 0.04,CuO St. Endellion,Cornwall. Mineral. Mag., 55, l2l-125. 12.5, sum 97.85 wto/o,corresponding to (CuStrMn3tu- Electron microprobe and CHN analysis gavePb75.47, Mgoo,)", oo(Mn3jrFe|jrAlo orTif.[nCuStr)", nrSi' o, for eight (calc.)6.03, sum 101.46wto/o, cations,ideally CuMnuSiO'r, the Cu analogueof braunite. Cl 18.67,C l.Iz,H 0.18,O to Pb.orClrrrCr.or- The range of Cu2* substitution for Mn2' is 0-42 molo/oin which for 17 atoms corresponds The min- cuprian braunite and 52-93 molo/oin abswurmbachite.
    [Show full text]
  • Gem Wealth of Tanzania GEMS & GEMOLOGY Summer 1992 Fipe 1
    By Dona M.Dirlarn, Elise B. Misiorowski, Rosemaiy Tozer, Karen B. Stark, and Allen M.Bassett The East African nation of Tanzania has he United Republic of Tanzania, the largest of the East great gem wealth. First known by Western- 1African countries, is composed of mainland Tanzania and ers for its diamonds, Tanzania emerged in the island of Zanzibar. 1t is regarded by many as the birthplace the 1960s as a producer of a great variety of of the earliest ancestors of Homo sapiens. To the gem indus- other gems such as tanzanite, ruby, fancy- try, however, Tanzania is one of the most promising fron- colored sapphire, garnet, and tourmaline; to date, more than 50 gem species and vari- tiers, with 50 gem species and varieties identified, to date, eties have been produced. As the 1990s from more than 200 occurrences. begin, De Beers has reinstated diamond "Modem" mining started in the gold fields of Tanzania in exploration in Tanzania, new gem materials the late 1890s (Ngunangwa, 19821, but modem diamond min- such as transparent green zoisite have ing did not start until 1925, and nearly all mining of colored appeared on the market, and there is stones has taken place since 1950. Even so, only a few of the increasing interest in Tanzania's lesser- gem materials identified have been exploited to any significant known gems such as scapolite, spinel, and extent: diamond, ruby, sapphire, purplish blue zoisite (tan- zircon. This overview describes the main zanite; figure l),and green grossular [tsavorite)and other gar- gems and gem resources of Tanzania, and nets.
    [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]
  • Transfers Young, Stephanie Lynne, Chalfont St
    The Journal of Gemmology2010 / Volume 32 / Nos. 1–4 The Gemmological Association of Great Britain The Journal of Gemmology / 2009 / Volume 31 / No. 5–8 The Gemmological Association of Great Britain 27 Greville Street, London EC1N 8TN T: +44 (0)20 7404 3334 F: +44 (0)20 7404 8843 E: [email protected] W: www.gem-a.com Registered Charity No. 1109555 Registered office: Palladium House, 1–4 Argyll Street, London W1F 7LD President: Prof. A. H. Rankin Vice-Presidents: N. W. Deeks, R. A. Howie, E. A. Jobbins, M. J. O'Donoghue Honorary Fellows: R. A. Howie Honorary Life Members: H. Bank, D. J. Callaghan, T. M. J. Davidson, J. S. Harris, E. A. Jobbins, J. I. Koivula, M. J. O'Donoghue, C. M. Ou Yang, E. Stern, I. Thomson, V. P. Watson, C. H. Winter Chief Executive Officer: J. M. Ogden Council: J. Riley – Chairman, A. T. Collins, S. Collins, B. Jackson, C. J. E. Oldershaw, L. Palmer, R. M. Slater Members’ Audit Committee: A. J. Allnutt, P. Dwyer-Hickey, J. Greatwood, G. M. Green, J. Kalischer Branch Chairmen: Midlands – P. Phillips, North East – M. Houghton, North West – J. Riley, Scottish – B. Jackson, South East – V. Wetten, South West – R. M. Slater The Journal of Gemmology Editor: Dr R. R. Harding Assistant Editor: M. J. O’Donoghue Associate Editors: Dr A. J. Allnutt (Chislehurst), Dr C. E. S. Arps (Leiden), G. Bosshart (Horgen), Prof. A. T. Collins (London), J. Finlayson (Stoke on Trent), Dr J. W. Harris (Glasgow), Prof. R. A. Howie (Derbyshire), E. A. Jobbins (Caterham), Dr J.
    [Show full text]
  • TUCSON 2018 Spinel—In Pink and Lavender Hues—In Suites and Sets As Customers Found the Scarcity and High Prices of Red Spinel Prohibitive
    Contributing Editors Emmanuel Fritsch, University of Nantes, CNRS, Team 6502, Institut des Matériaux Jean Rouxel (IMN), Nantes, France (fritsch@cnrs- imn.fr) Gagan Choudhary, Gem Testing Laboratory, Jaipur, India ([email protected]) Christopher M. Breeding, GIA, Carlsbad ([email protected]) manite. Many dealers posted strong sales of pastel-colored spinel—in pink and lavender hues—in suites and sets as TUCSON 2018 customers found the scarcity and high prices of red spinel prohibitive. In a similar vein, Margit Thorndal of Madagas- Every February the gem and mineral world descends on car Imports reported strong demand for purple-lavender Tucson, transforming the downtown convention center spinel and purple sapphire from Madagascar, as well as teal and a great many of the city’s hotels into a fascinating col- hues of unheated Montana sapphire. lage of traders bearing goods from all over the planet (fig- We noted that electric blues, teals, hot pinks, hot yel- ures 1 and 2). low greens, and pastel-colored gems were quite popular. Many of the exhibitors we spoke with described 2018 Bill Larson of Pala International pointed to this trend and as the strongest year since 2008. Although traffic wasn’t showed us a number of spectacular examples from his in- especially heavy at the AGTA and GJX shows, most deal- ventory. Fine blue zircon from Cambodia was prominent, ers there enjoyed brisk sales and healthy demand for high- as was attractive sphene from Zimbabwe and Madagascar. quality goods. Some of the same trends from last year were Dave Bindra of B&B Fine Gems said his company was evident.
    [Show full text]
  • The Seven Crystal Systems
    Learning Series: Basic Rockhound Knowledge The Seven Crystal Systems The seven crystal systems are a method of classifying crystals according to their atomic lattice or structure. The atomic lattice is a three dimensional network of atoms that are arranged in a symmetrical pattern. The shape of the lattice determines not only which crystal system the stone belongs to, but all of its physical properties and appearance. In some crystal healing practices the axial symmetry of a crystal is believed to directly influence its metaphysical properties. For example crystals in the Cubic System are believed to be grounding, because the cube is a symbol of the element Earth. There are seven crystal systems or groups, each of which has a distinct atomic lattice. Here we have outlined the basic atomic structure of the seven systems, along with some common examples of each system. Cubic System Also known as the isometric system. All three axes are of equal length and intersect at right angles. Based on a square inner structure. Crystal shapes include: Cube (diamond, fluorite, pyrite) Octahedron (diamond, fluorite, magnetite) Rhombic dodecahedron (garnet, lapis lazuli rarely crystallises) Icosi-tetrahedron (pyrite, sphalerite) Hexacisochedron (pyrite) Common Cubic Crystals: Diamond Fluorite Garnet Spinel Gold Pyrite Silver Tetragonal System Two axes are of equal length and are in the same plane, the main axis is either longer or shorter, and all three intersect at right angles. Based on a rectangular inner structure. Crystal shapes include: Four-sided prisms and pyramids Trapezohedrons Eight-sided and double pyramids Icosi-tetrahedron (pyrite, sphalerite) Hexacisochedron (pyrite) Common Tetragonal Crystals: Anatase Apophyllite Chalcopyrite Rutile Scapolite Scheelite Wulfenite Zircon Hexagonal System Three out of the four axes are in one plane, of the same length, and intersect each other at angles of 60 degrees.
    [Show full text]
  • POUDRETTEITE, Knarb3si12o3e, a NEW MEMBER of the OSUMILITE GROUP from MONT SAINT-HILAIRE, OUEBEC, and ITS CRVSTAL STRUCTURE Assr
    Canadian Mineralogist Vol. 25, pp.763-166(1987) POUDRETTEITE,KNarB3Si12O3e, A NEW MEMBEROF THE OSUMILITEGROUP FROM MONT SAINT-HILAIRE,OUEBEC, AND ITS CRVSTALSTRUCTURE JOEL D. GRICE, T. SCOTT ERCIT AND JERRY VAN VELTHUIZEN Mineral SciencesDivision, National Museumof Natural Sciences,Ottawa, Ontario KIA 0M8 PETE J. DUNN Departmentof Mineral Sciences,Smithsonian Institution, Washington,D.C, 20560,U,S.A. Assrnact positionC d coordinanceXII, le sodium,la position,4d unecoordinance VI, le bore,la position72 ir coordinance Poudretteiteis a newmineral species from the Poudrette IV, le silicium,la position71 i coordinanceIV, etla posi- quarry, Mont Saint-Hilaire,Quebec. It occursin a marble tion B estvacante. xenolith includedin nephelinesyenite, associated with pec- tolite, apophyllite, quartz and minor aegirine.It forms clear, Mots-clds: poudrettdite, nouvelle espbce min6rale, groupe colorlessto very pale pink, equidimensional,subhedral del'osumilite, mont Saint-Hilaire, borosilicate, affi ne. prismsup to 5 mm. It is brittle, H about 5, with a splin- mentde Ia structure. tery fracture;Dmetr. 2.51(l) g/cml, D"6".2.53 g/cm3. Uniaxialpositive, co 1.516(l), e 1.532(l).It is-hexagonal, spacegroup P6/ mcc, a I 0.239(l), c 13.485(3)A and,Z : 2. INTRoDUcTIoN The strongestten X-ray-diffractionlines in the powderpat- tern [d in A(r\(hkDl are: 6.74(30)(002),5.13 (100)(110), The optical and physical propertiesof members 4.07(30)(r 12), 3.70(30)(202), 3.3 6e(30)(004), 3.253 ( I 00) of the osumilite group are similar to those of com- (2r r), 2.9s6(40)(3 00), 2.8 I 5(60)(I I 4), 2.686(50)(213,204) mon mineralssuch as quartz and cordierite;for this and 2.013(30)(321).An analysisby electron microprobe reason, they are probably generally overlooked.
    [Show full text]
  • Guide to Healing Uses of Crystals & Minerals
    Guide to Healing Uses of Crystals & Minerals Addiction- Iolite, amethyst, hematite, blue chalcedony, staurolite. Attraction – Lodestone, cinnabar, tangerine quartz, jasper, glass opal, silver topaz. Connection with Animals – Leopard skin Jasper, Dalmatian jasper, silver topaz, green tourmaline, stilbite, rainforest jasper. Calming – Aqua aura quartz, rose quartz, amazonite, blue lace agate, smokey quartz, snowflake obsidian, aqua blue obsidian, blue quartz, blizzard stone, blood stone, agate, amethyst, malachite, pink tourmaline, selenite, mangano calcite, aquamarine, blue kyanite, white howlite, magnesite, tiger eye, turquonite, tangerine quartz, jasper, bismuth, glass opal, blue onyx, larimar, charoite, leopard skin jasper, pink opal, lithium quartz, rutilated quartz, tiger iron. Career Success – Aqua aura quartz, ametrine, bloodstone, carnelian, chrysoprase, cinnabar, citrine, green aventurine, fuchsite, green tourmaline, glass opal, silver topaz, tiger iron. Communication – Apatite, aqua aura quartz, blizzard stone, blue calcite, blue kyanite, blue quartz, green quartz, larimar, moss agate, opalite, pink tourmaline, smokey quartz, silver topaz, septarian, rainforest jasper. www.celestialearthminerals.com Creativity – Ametrine, azurite, agatized coral, chiastolite, chrysocolla, black amethyst, carnelian, fluorite, green aventurine, fire agate, moonstone, celestite, black obsidian, sodalite, cat’s eye, larimar, rhodochrosite, magnesite, orange calcite, ruby, pink opal, blue chalcedony, abalone shell, silver topaz, green tourmaline,
    [Show full text]
  • 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,
    [Show full text]