X"^ the Journal of "I Y Volume 27 No

Total Page:16

File Type:pdf, Size:1020Kb

X GAGTL EDU GemmolosX"^ The Journal of "I y Volume 27 No. 8 October 2001 tj J Cultured Cat's-eyes and Nephrite Synthetic pearls star stones jade moissanite 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 President: Professor A.T. Collins Vice-Presidents: 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, R.R. Harding, I. Mercer, J. Monnickendam, M.J. O'Donoghue, E. Stern, I. Thomson, J-P. van Doren, V.P. Watson Members' Council: A.J. Allnutt, S. Burgoyne, P. Dwyer-Hickey, S.A. Everitt, 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 - I. Knight, Scottish - B. Jackson, South West - R.M. Slater Examiners: A.J. Allnutt, M.Sc, Ph.D., FGA, L. Bartlett, B.Sc, M.Phil., 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, S. Hue Williams MA, FGA, DGA, B. Jackson, FGA, DGA, G.H. Jones, B.Sc, Ph.D., FGA, Li Li Ping, FGA, DGA, 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. 8, October 2001 ISSN: 1355-4565 Cultured pearls and colour-changed cultured pearls: Raman spectra Li Liping and Chen Zhonghui Gemmological Institute, China University of Geosciences, Wuhan 430074, P.R. China ABSTRACT: The numbers of coloured pearls on the market have grown over the past few years and include dyed pearls, irradiated pearls and so-called 'lasered' pearls. In this study, different pearl samples have been experimentally dyed or irradiated. Their Raman spectra have been obtained and found to be useful in identifying the colour origin of pearls. Keywords: colour origin, dyed pearl, irradiated pearl, natural coloured pearl, Raman spectrum Introduction coloured freshwater cultured pearls. Our research work has shown that the so-called ver the years, the range of coloured Tasered' freshwater cultured pearls are actu­ freshwater cultured pearls generally ally dyed(1). Our studies have confirmed that Oavailable has increased significantly colour features, colour distribution, internal 451 and includes black, peacock green, dark characteristics, ultra-violet fluorescence, and purple and bronze varieties. Some are dyed, chemical tests are useful in identifying some some are irradiated freshwater cultured dyed or irradiated pearls (op. cit.). However, pearls, and some are even labelled as many treated cultured pearls do not show Tasered'. These are in addition to naturally any distinctive features. Furthermore, when #•% i Figure 1: Some of the pearl samples studied: dyed cultured pearls (left) and irradiated cultured pearls (right). © Gemmological Association and Gem Testing Laboratory of Great Britain ISSN: 1355-4565 Table I: Chemical data for five pearls. Sample Freshwater pearls Tahiti pearl white orange purple di/erf rfarfc Element purple at.% F-l F-2 F-3 FA F-6 Ca 37.98 37.78 37.91 38.17 38.12 Na 0.26 0.26 0.28 0.27 0.75 ppm Mg 39 25 48 40 79 Si 840 790 1800 1300 1600 P 210 220 190 170 170 Al 9 8 13 24 14 K 56 52 69 238 238 Sr 394 332 402 373 900 Ba 410 550 390 330 190 Fe 5 36 11 21 49 Mn 286 323 643 241 1 451 Cu 1 1 1 1 2 Zn 4 3 4 4 5 Ni 1 1 2 <1 <1 Co <1 <1 <1 <1 <1 Cr <1 <1 <1 <1 <1 N.B.: Results obtained from Hitchi 180-70 atomic absorption spectrometer. a pearl is mounted, identification of its green line (514.5 nm) of an Ar-ion laser colour origin is made more difficult. as excitation. In order to obtain comparable Raman spectra, the power and exposure For this study, some of the samples were times were kept constant for all the samples. obtained directly from the market and others were treated by dyeing or irradiation The chemical compositions of natural- (Figure 1). Some of the cultured pearls were coloured and dyed pearls were obtained by dyed black by immersion over a twelve day dissolving small samples of pearl and period in either 0.025N silver nitrate, or in analysing the solutions with a Hitachi 180-70 silver nitrate diluted with ammonia atomic absorption spectrometer; the results (Figure 2). Some were treated by electron are shown in Table I. accelerator. Eighteen samples were tested In this study, all the freshwater cultured using the Renishaw MK1-1000 laser Raman pearls are non-nucleated and all the spectrometer at room temperature with the seawater cultured pearls are nucleated. /. Gemm., 2001, 27, 8, 449-455 Figure 2: Cultured pearls dyed with AgN03 only (left) and pearls dyed using AgN03 diluted by ammonia (right). Results and discussion The black Tahiti cultured pearl samples show very strong fluorescence under the Naturally-coloured cultured pearls green laser, and in the Raman spectrum Naturally-coloured freshwater cultured (Figure 4) there is a broad low peak at 1605 pearls are usually white, orange or purple as cm4 beside the typical sharp peaks at 1083 shown in Figure 3. It is easy to distinguish and 702 cm1 of aragonite. As can be seen naturally-coloured freshwater cultured from the chemical analysis (Table I, column pearls from black Tahiti cultured pearls F-6) the Tahiti pearl contains very small (whether nucleated or non-nucleated) on quantities of minor elements, which proba­ colour alone. However, the lighter grey bly would have little influence on the colour. Tahiti cultured pearls may prove to be more The peak at 1605 cm4 is relatively low and difficult to differentiate. comparatively wide, indicating that it may 451451 451 Figure 3: Naturally-coloured Chinese freshwater cultured pearls. Cultured pearls and colour-changed cultured pearls: Raman spectra '083 25000 1605 20000 ~ 15000 0 II 10000 702 5000 '600 '400 ' 200 '000 800 600 400 200 Ramanshift (cm-t) fi gure 4: Raman spectrum of Tahiti cultured pearl. 1084 '5000 10000 1524 452 5000 3046 2650 ~ 1132 A 226 1 151 JU ' 90 :r 27' 3500 3000 2500 2000 ' 500 1000 500 Raman shift (em-I) f igure 5: Raman spectrum of naturally-colouredorangefres hwatercultured pearl. 6000 1083 6000 1510 15 19 1127 00 C 4000 263 1 5 3730 3024 II 2000 '295 1017 702 3500 3000 2500 2000 1500 1000 500 Raman shift (cm-r) Figure 6: Raman spectrum of naturally-coloured purplefreshwater cultured pearl. J. Gemm., 2001, 27, 8, 449-455 12000 1579 10000 8000 ~ 6000 6 0 4000 2000 3500 3000 2500 2000 1500 1000 500 Raman shift (cm-t) Figure 7: Ramanspectrum offreshwater culturedpearl dyed black by silvernitrate. be caused by a substance of low crystalline Dyed pearls structure, which would include organic Many freshwater and saltwater cultured materials. It has been suggested by other pearls are dyed various colours. The dyed researchers (e.g. see(2)) that pigments such as black cultured pearls often show very good porphyrin seem to be the cause of colour in iridescence. The iridescent peacock green and Tahiti cultured pearls. purple colours associated with the highly For naturally-coloured orange freshwater valued natural-coloured black Tahiti cul­ 453 cultured pearls, the Raman spectrum tured pearls can also be seen in the so-called (Figure 5) is very different to that seen in 'Iasered' freshwater cultured pearls. The Tahiti cultured pearls. In addition to the colour distribution in both types is quite sharp and strong peaks of aragonite at 1084 even. The 'lasered' freshwater cultured and 702 cm', there are sharp peaks at 1524 pearls are actually dyed - the process and 1132 cm' and also some weak peaks at involves immersion for about one year in a 2650 and 2261 cm'. The sharp peaks indicate new organic dye. that the impurities are in the crystal structure. All the dyed cultured pearl samples show The chemical analyses for the orange fresh­ very different Raman spectra to the naturally­ water cultured pearls reveal iron (Table I, F-2) coloured cultured pearl samples. The three being present in a comparatively high black cultured pearls dyed by silver nitrate enough concentration to be a possible methods produced differing colour satura­ contributory cause of the orange colour. tions, but similar Raman spectra. The Further research is needed to establish if this absorption peaks of aragonite are commonly is the cause of colour. present but, compared with Raman spectra The naturally-coloured purple freshwa­ of undyed cultured pearls, what was also ter cultured pearls show a complicated found were peaks relating to carbon as seen Raman spectrum, with sharp peaks at 1127, in the likes of jet'3) (Figure 7).
Recommended publications
  • Black Pearls
    Number 22 The Journal of the AMERICAN BOTANI CAL COUNCU.. and the HERB RESEARCH FOUNDATION Hawthorn -A Literature Review Special Report: Black Pearls - Prescription Drugs Masquerade as Chinese Herbal Arthritis Formula FROM THE EDITOR In This Issue his issue of HerbalGram offers some good news and some herbal combination for use in rheumatoid arthritis and related bad news. First the good news. Our Legal and Regulatory inflammatory conditions, this product has been tested repeatedly Tsection is devoted to a recent clarification by the Canadian and shown positive for the presence of unlabeled prescription drugs. Health Protection Branch (Canada's counterpart to our FDA)of its Herb Research Foundation President Rob McCaleb and I have willingness to grant "Traditional Medicine" status to many medici­ spent several months researching the latest resurgence in sales of nal herb products sold in Canada under the already existing approval this and related products. We have made every attempt to follow up process for over-the-counter remedies. This announcement has on many avenues to determine whether these products contain un­ been hailed as a positive step by almost everyone with whom we labeled drugs, and whether or not they are being marketed fraudu­ have talked, both in academia and in the herb industry. lently. Herb marketers and consumers alike should be concerned More good news is found in the literature review on Hawthorn. whenever prescription drugs are presented for sale as "natural" and Steven Foster has joined Christopher Hobbs in preparing a compre­ "herbal." You will find our report on page 4. hensive view of a plant with a long history of use as both food and In addition, we present the usual array of interesting blurbs, medicine.
    [Show full text]
  • L. Jahnsite, Segelerite, and Robertsite, Three New Transition Metal Phosphate Species Ll. Redefinition of Overite, an Lsotype Of
    American Mineralogist, Volume 59, pages 48-59, 1974 l. Jahnsite,Segelerite, and Robertsite,Three New TransitionMetal PhosphateSpecies ll. Redefinitionof Overite,an lsotypeof Segelerite Pnur BnnN Moone Thc Departmcntof the GeophysicalSciences, The Uniuersityof Chicago, Chicago,Illinois 60637 ilt. lsotypyof Robertsite,Mitridatite, and Arseniosiderite Peur BmaN Moonp With Two Chemical Analvsesbv JUN Iro Deryrtrnent of GeologicalSciences, Haraard Uniuersity, Cambridge, Massrchusetts 02 I 38 Abstract Three new species,-jahnsite, segelerite, and robertsite,-occur in moderate abundance as late stage products in corroded triphylite-heterosite-ferrisicklerite-rockbridgeite masses, associated with leucophosphite,hureaulite, collinsite, laueite, etc.Type specimensare from the Tip Top pegmatite, near Custer, South Dakota. Jahnsite, caMn2+Mgr(Hro)aFe3+z(oH)rlPC)oln,a 14.94(2),b 7.14(l), c 9.93(1)A, p 110.16(8)", P2/a, Z : 2, specific gavity 2.71, biaxial (-), 2V large, e 1.640,p 1.658,t l.6lo, occurs abundantly as striated short to long prismatic crystals, nut brown, yellow, yellow-orange to greenish-yellowin color.Formsarec{001},a{100},il2oll, jl2}ll,ft[iol],/tolll,nt110],andz{itt}. Segeierite,CaMg(HrO)rFes+(OH)[POdz, a 14.826{5),b 18.751(4),c7.30(1)A, Pcca, Z : 8, specific gaavity2.67, biaxial (-), 2Ylarge,a 1.618,p 1.6t5, z 1.650,occurs sparingly as striated yellow'green prismaticcrystals, with c[00], r{010}, nlll0l and qll2l } with perfect {010} cleavage'It is the Feg+-analogueofoverite; a restudy on type overite revealsthe spacegroup Pcca and the ideal formula CaMg(HrO)dl(OH)[POr]r. Robertsite,carMna+r(oH)o(Hro){Ponlr, a 17.36,b lg.53,c 11.30A,p 96.0o,A2/a, Z: 8, specific gravity3.l,T,cleavage[l00] good,biaxial(-) a1.775,8 *t - 1.82,2V-8o,pleochroismextreme (Y, Z = deep reddish brown; 17 : pale reddish-pink), @curs as fibrous massesand small wedge- shapedcrystals showing c[001 f , a{1@}, qt031}.
    [Show full text]
  • Alteration of Spodumene, Montebrasite and Lithiophilite In
    American Mineralogist, Volume 67, pages 97-113, 1982 Alteration of spodumene,montebrasite and lithiophilite in pegmatites of the White PicachoDistrict, Arizona Davrp Lor.rooxrnNo DoNer-uM. Bunr Department of Geology Arizona State University Tempe, Arizona 85281 Abstract The crystallization sequence and metasomatic alteration of spodumene (LiAlSizOe), montebrasite(LiAIPO4(OH,F)), and lithiophilite (Li(Mn,Fe)PO+)are describedfor nine zoned lithium pegmatitesin the White Picacho district, Arizona. The observedcrystalliza- tion trends suggesta progressiveincrease in the activities of lithium species(spodumene follows microcline as the principal alkali aluminosilicate), as well as an increase in the activities of the acidic volatiles phosphorus and fluorine (montebrasite succeedsspodu- mene as the stableprimary lithium phase).Much of the lithiophilite occurs with columbite, apatite, beryl, zircon, and tourmaline in cleavelanditecomplexes that formed in part at the expenseof quartz-spodumenepegmatite. Fracture-controlledpseudomorphic alteration of the primary lithium minerals is widespread and apparently is the result of subsolidus reactionswith residualpegmatitic fluids. Spodumenehas been replacedby eucryptite, albite, and micas. Alteration products of montebrasite include low-fluorine secondary montebrasite,crandallite (tentative), hydroxylapatite, muscovite, brazilianite, augelite (tentative),scorzalite, kulanite, wyllieite, and carbonate-apatite.Secondary phases identi- fied in altered lithiophilite include hureaulite, triploidite, eosphorite,
    [Show full text]
  • Mineralogy and Geochemistry of Nephrite Jade from Yinggelike Deposit, Altyn Tagh (Xinjiang, NW China)
    minerals Article Mineralogy and Geochemistry of Nephrite Jade from Yinggelike Deposit, Altyn Tagh (Xinjiang, NW China) Ying Jiang 1, Guanghai Shi 1,* , Liguo Xu 2 and Xinling Li 3 1 State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China; [email protected] 2 Geological Museum of China, Beijing 100034, China; [email protected] 3 Xinjiang Uygur Autonomous Region Product Quality Supervision and Inspection Institute, Xinjiang 830004, China; [email protected] * Correspondence: [email protected]; Tel.: +86-010-8232-1836 Received: 6 April 2020; Accepted: 6 May 2020; Published: 8 May 2020 Abstract: The historic Yinggelike nephrite jade deposit in the Altyn Tagh Mountains (Xinjiang, NW China) is renowned for its gem-quality nephrite with its characteristic light-yellow to greenish-yellow hue. Despite the extraordinary gemological quality and commercial significance of the Yinggelike nephrite, little work has been done on this nephrite deposit, due to its geographic remoteness and inaccessibility. This contribution presents the first systematic mineralogical and geochemical studies on the Yinggelike nephrite deposit. Electron probe microanalysis, X-ray fluorescence (XRF) spectrometry, inductively coupled plasma mass spectrometry (ICP-MS) and isotope ratio mass spectrometry were used to measure the mineralogy, bulk-rock chemistry and stable (O and H) isotopes characteristics of samples from Yinggelike. Field investigation shows that the Yinggelike nephrite orebody occurs in the dolomitic marble near the intruding granitoids. Petrographic studies and EMPA data indicate that the nephrite is mainly composed of fine-grained tremolite, with accessory pargasite, diopside, epidote, allanite, prehnite, andesine, titanite, zircon, and calcite. Geochemical studies show that all nephrite samples have low bulk-rock Fe/(Fe + Mg) values (0.02–0.05), as well as low Cr (0.81–34.68 ppm), Co (1.10–2.91 ppm), and Ni (0.52–20.15 ppm) contents.
    [Show full text]
  • Crystal Chemistry of the Monazite and Xenotime Structures Yuxxnnc Nr
    American Mineralogist, Volume 80, pages2I-26, 1995 Crystal chemistry of the monazite and xenotime structures YuxxnNc Nr, JonN M. Hucnns Department of Geology, Miami University, Oxford, Ohio 45056' U.S.A. ANrrrotvv N. M.q'nr,lNo 48 PageBrook Road, Carlisle, Massachusetts01741' U.S.A. Arsrnlcr Monazite and xenotime, the RE(PO,) dimorphs, are the most ubiquitous rare earth (RE) minerals, yet accuratestructure studiesof the natural phaseshave not been reported. Here we report the results of high-precision structure studies of both the natural phasesand the synthetic RE(PO4)phases for all individual stable rare earth elements. Monazite is monoclinic, P2r/n, and xenotime is isostructural with zircon (spacegroup 14r/amd)- Both atomic arrangementsare basedon [001] chains of intervening phosphate tetrahedra and RE polyhedra, with a REO, polyhedron in xenotime that accommodates the heavy lanthanides(Tb-Lu in the synthetic phases)and a REO, polyhedron in monazite that preferentially incorporatesthe larger light rare earth elements(Ia-Gd). As the struc- ture "transforms" from xenotime to monazite, the crystallographic properties are com- parable along the [001] chains, with structural adjustments to the different sizes of RE atoms occurring principally in (001). There are distinct similarities betweenthe structuresthat are evident when their atomic arrangementsare projected down [001]. In that projection, the chains exist i! (100) planes, with two planes per unit cell. In monazite the planes are offset by 2.2 A along [010], relative to those in xenotime, in order to accommodate the larger light RE atoms. The shift of the planes in monazite allows the RE atom in that phaseto bond to an additional 02' atom to complete the REO' polyhedron.
    [Show full text]
  • OK PASSOVER PRODUCTS FOOD GUIDE 2020 ALCOHOLIC BEVERAGES Aluminum 10" Round Pan Multipeel (O) Barkan Wine Cellars Ltd
    OK PASSOVER PRODUCTS FOOD GUIDE 2020 ALCOHOLIC BEVERAGES Aluminum 10" Round Pan Multipeel (O) Barkan Wine Cellars Ltd. Aluminum 3lb Large Oval Bakin Nalo Faser / Fibrous- cellulose Givon Vodka Aluminum 4 4/5" Round Pan casings with paper (O) Courvoisier SAS Aluminum 5lb X-large Oval Bak Nalo Ferm (O) XO Cognac Courvoisier Size: Aluminum 8" Angel Tube Pan Nalo Kranz-pure cellulose casings 700ml Lot: L9162JCG01, Aluminum 8" Round Pan (O) L6202JCG05 Aluminum Medium Oval Baking Nalo ML-pure cellulose casings Le Cognac de Napoleon P (O) XO Cognac Courvoisier Size: Nicole Home Collection Nalo M-pure cellulose casings 700ml Lot: L9162JCG01, (O) 8" Square Cake Pan Aluminum L6202JCG05 Nalo Net-fibrous casing with net 9" Square Deep Cake Pan- Matar Winery (O) alumin Arak Nalo Schmal / Cellulose- pure Aluminum 10" Angel Tube Royal Wine Corporation cellulose casings (O) Pan Alfasi - Mistico (MV) Nalo Top - cellulose casings with Aluminum 10" Round Pan ALUMINUM WRAP PRODUCTS paper (O) Aluminum 3lb Large Oval Bakin Betty Crocker NaloFashion (O) Aluminum 4 4/5" Round Pan 25Sq ft Aluminum Foil (O) OSKUDA 2101 (O) Aluminum 5lb X-large Oval Bak 37.5Sq ft Aluminum Foil (O) Pergament (O) Aluminum 8" Angel Tube Pan 75Sq ft Aluminum Foil (O) Rona (O) Aluminum 8" Round Pan Formula Brands Inc. Ronet (O) Aluminum Medium Oval Baking 25Sq ft Aluminum Foil (O) Rotex (O) P 37.5Sq ft Aluminum Foil (O) Texdalon (O) AROMATIC CHEMICALS 75Sq ft Aluminum Foil (O) Texdalon KSB - Semi Finished Crown Chemicals Pvt. Ltd. Guangzhou Huafeng Aluminum (O) Piperonal Foil Technologies Co Ltd.
    [Show full text]
  • With a Short Neck and Angular Should
    LOW HIGH Lot Description Estimate Estimate Chinese archaistic bronze wine vessel (pou), with a short neck and angular shoulder with 1 three ram's head form handles, the body with taotie on a dense ground, raised on a tall foot, 8"h $ 300 - 500 (lot of 2) Chinese archaistic bronzes, the first a pouring vessel on tripod supports with taotie 2 pattern, body with inscription; the other an ox form guang lidded vessel, with a bird motif on the body,10.75"w $ 300 - 500 (lot of 3) Asian bronze items, consisting of a Himalayan ritual dagger (purba) and a ghanta 3 (bell); together with a Chinese archaistic bronze bell, with raised bosses, with wood stand, bell: 8.25"h $ 300 - 500 (lot of 5) Chinese hardstone plaques, consisting of two butterflies; one floral roundel; one 4 fan and one of bird-and-flowers, 2.75"w $ 150 - 250 5 Chinese hardstone bangle, reticulated with bats and tendrils, 2.5"w $ 300 - 500 (lot of 2) Chinese hardstone pebbles, the first carved of a bamboo stalk; the second, of a 6 mouse and sack, largest: 2"w $ 400 - 600 7 (lot of 2) Chinese hardstone figural carvings, featuring one young attendant; and the other of an immortal with a lion on his shoulder, with wood stands, carving: 3.125"h $ 300 - 500 Chinese bronze zoomorph, featuring a recumbent beast with a reticulated body with a bird 8 pattern, 4"w $ 200 - 400 Chinese patinated bronze censer of ding-form, the rim flanked by upright handles and the 9 body cast with floral scrolls, raised on tall tripod supports, with wood stand and lid, censer: 5"h $ 300 - 500 (lot of 5) Chinese
    [Show full text]
  • The Secondary Phosphate Minerals from Conselheiro Pena Pegmatite District (Minas Gerais, Brazil): Substitutions of Triphylite and Montebrasite Scholz, R.; Chaves, M
    The secondary phosphate minerals from Conselheiro Pena Pegmatite District (Minas Gerais, Brazil): substitutions of triphylite and montebrasite Scholz, R.; Chaves, M. L. S. C.; Belotti, F. M.; Filho, M. Cândido; Filho, L. Autor(es): A. D. Menezes; Silveira, C. Publicado por: Imprensa da Universidade de Coimbra URL persistente: URI:http://hdl.handle.net/10316.2/31441 DOI: DOI:http://dx.doi.org/10.14195/978-989-26-0534-0_27 Accessed : 2-Oct-2021 20:21:49 A navegação consulta e descarregamento dos títulos inseridos nas Bibliotecas Digitais UC Digitalis, UC Pombalina e UC Impactum, pressupõem a aceitação plena e sem reservas dos Termos e Condições de Uso destas Bibliotecas Digitais, disponíveis em https://digitalis.uc.pt/pt-pt/termos. Conforme exposto nos referidos Termos e Condições de Uso, o descarregamento de títulos de acesso restrito requer uma licença válida de autorização devendo o utilizador aceder ao(s) documento(s) a partir de um endereço de IP da instituição detentora da supramencionada licença. Ao utilizador é apenas permitido o descarregamento para uso pessoal, pelo que o emprego do(s) título(s) descarregado(s) para outro fim, designadamente comercial, carece de autorização do respetivo autor ou editor da obra. Na medida em que todas as obras da UC Digitalis se encontram protegidas pelo Código do Direito de Autor e Direitos Conexos e demais legislação aplicável, toda a cópia, parcial ou total, deste documento, nos casos em que é legalmente admitida, deverá conter ou fazer-se acompanhar por este aviso. pombalina.uc.pt digitalis.uc.pt 9 789892 605111 Série Documentos A presente obra reúne um conjunto de contribuições apresentadas no I Congresso Imprensa da Universidade de Coimbra Internacional de Geociências na CPLP, que decorreu de 14 a 16 de maio de 2012 no Coimbra University Press Auditório da Reitoria da Universidade de Coimbra.
    [Show full text]
  • Riebeckite Na2[(Fe2+,Mg)3Fe 2 ]Si8o22(OH)
    2+ 3+ Riebeckite Na2[(Fe ; Mg)3Fe2 ]Si8O22(OH)2 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Monoclinic. Point Group: 2=m: As prismatic crystals, to 20 cm. Commonly ¯brous, asbestiform; earthy, massive. Twinning: Simple or multiple twinning 100 . k f g Physical Properties: Cleavage: Perfect on 110 , intersecting at 56 and 124 ; partings f g ± ± on 100 , 010 . Fracture: [Conchoidal to uneven.] Tenacity: Brittle. Hardness = 6 f g f g D(meas.) = 3.28{3.44 D(calc.) = 3.380 Optical Properties: Semitransparent. Color: Black, dark blue; dark blue to yellow-green in thin section. Luster: Vitreous to silky. Optical Class: Biaxial (+) or ({). Pleochroism: X = blue, indigo; Y = yellowish green, yellow- brown; Z = dark blue. Orientation: Y = b; X c = 8 to 7 ; Z c = 6 {7 . Dispersion: ^ ¡ ± ¡ ± ^ ± ± Strong. ® = 1.656{1.697 ¯ = 1.670{1.708 ° = 1.665{1.740 2V(meas.) = 50±{90±. Cell Data: Space Group: C2=m: a = 9.822 b = 18.07 c = 5.334 ¯ = 103:52± Z = 2 X-ray Powder Pattern: Doubrutscha [Dobrudja], Romania. (ICDD 19-1061). 8.40 (100), 3.12 (55), 2.726 (40), 2.801 (18), 4.51 (16), 2.176 (16), 3.27 (14) Chemistry: (1) (2) (1) (2) SiO2 52.90 50.45 CaO 0.12 0.08 TiO2 0.57 0.14 Li2O 0.54 Al2O3 0.12 1.96 Na2O 6.85 6.80 Fe2O3 17.20 17.52 K2O 0.03 1.48 Cr2O3 0.04 F 2.58 + FeO 17.95 17.90 H2O 0.87 MnO 0.00 1.40 O = F 1.09 ¡ 2 MgO 2.96 0.05 Total 98.74 100.68 (1) Dales Gorge Iron Formation, Western Australia; by electron microprobe, corresponds to 2+ 3+ (Na2:00Ca0:02K0:01)§=2:03(Fe2:26Mg0:66Ti0:06)§=2:98Fe1:95(Si7:98Al0:02)§=8:00O22(OH)2: (2) Pikes 2+ Peak area, Colorado, USA; corresponds to (Na2:02K0:29Ca0:01)§=2:32(Fe2:30Li0:33Mn0:18Al0:10 3+ Ti0:02Mg0:01)§=2:94Fe2:02(Si7:75Al0:25)§=8:00O22[F1:25(OH)0:89]§=2:14: Polymorphism & Series: Forms a series with magnesioriebeckite.
    [Show full text]
  • C:\Documents and Settings\Alan Smithee\My Documents\MOTM
    Rdosdladq1//6Lhmdq`knesgdLnmsg9@bshmnkhsd This month’s featured mineral has many interesting and unusual varieties: While our specimens have well-developed prismatic crystals, which is unusual for actinolite, a fibrous variety is a former ore of asbestos, and a microcrystalline variety is one of the two types of the gemstone jade. Read on! OGXRHB@K OQNODQSHDR 2+ Chemistry: GCa2(Mg,Fe )5Si8O22(OH)2 Basic Calcium Magnesium Iron Silicate (Calcium Magnesium Iron Silicate Hydroxide) Class: Silicates Subclass: Inosilicates (Double-Chain Silicates) Group: Tremolite (Amphibole Group) Crystal System: Monoclinic Crystal Habits: Usually long prismatic with diamond-shaped cross section; also bladed, columnar, acicular, divergent, fibrous (asbestiform), and radiating. A compact, microcrystalline form is known as nephrite jade. Color: Bright-to-dark green, grayish-green, and greenish-black. Luster: Vitreous; silky and pearly on cleavage surfaces. Transparency: Transparent to translucent Streak: Colorless to white Cleavage: Perfect in two directions lengthwise with intersecting cleavage planes. Fracture: Splintery, uneven; fibrous forms are flexible. Hardness: 5.0-6.0, nephrite variety is 6.5. Specific Gravity: 3.0-3.5 Luminescence: None Refractive Index: 1.63-1.66 Distinctive Features and Tests: Best field marks are the prismatic, often-radiating crystal habit and narrow cleavage-intersection angle. Can be confused with wollastonite, which is fluorescent; the tourmaline-group minerals, which lack cleavage; and epidote, which has a broader cleavage angle. Laboratory methods are necessary to differentiate actinolite from tremolite and ferro- actinolite, as explained in the box on Page 3. Dana Classification Number: 66.1.3a.2 M @L D The name “actinolite,” pronounced ack-TIH-no-lite, derives from the Greek aktino, meaning “ray,” a reference to the common radiate habit of its prismatic crystals.
    [Show full text]
  • Crystal Morphology and Xrd Peculiarities of Brazilianite from Different Localities
    NAT. CROAT. VOL. 20 No 1 1¿18 ZAGREB June 30, 2011 original scientific paper / izvorni znanstveni rad CRYSTAL MORPHOLOGY AND XRD PECULIARITIES OF BRAZILIANITE FROM DIFFERENT LOCALITIES ANDREA ^OBI]*1,VLADIMIR ZEBEC2,RICARDO SCHOLZ3, VLADIMIR BERMANEC1 &SANDRA DE BRITO BARRETO4 ¹Faculty of Science, Institute of Mineralogy and Petrography, Horvatovac 95, Zagreb, Croatia 2Croatian Natural History Museum, Demetrova 1, Zagreb, Croatia 3Department of Geology, School of Mining, Federal University Ouro Preto, Ouro Preto, MG, Brazil 4Department of Geology, Federal University of Pernambuco, Av. Academico Hélio Ramos. S/N. 5 andar., Cidade Universitária, Recife, PE, Brasil ^obi}, A., Zebec, V., Scholz, R., Bermanec, V. & de Brito Barreto, S.: Crystal morphology and xrd peculiarities of brazilianite from different localities. Nat. Croat., Vol. 20, No. 1., 1–18, 2011, Zagreb. Forty four brazilianite crystals from several localities in Brazil, Rwanda and Canada were measured on a two-circle goniometer to determine brazilianite morphology. Twenty forms were recorded; six of them have not been recorded before. All faces in the [001] zone are striated along crystallographic axis c. All striated forms in the [001] zone exhibit multiple signals. Two of the signals observed on the form {110} are always very clear. There is an exception on one crystal where just one face, (110), exhibits only one clear signal. Five groups of habits were recorded, two of them new to this mineral species. Eleven samples were examined by X-ray diffraction for calculation of the unit cell parameters yield- ing a=11.201(1)–11.255(2) Å, b=10.1415(5)–10.155(1) Å, c=7.0885(7)–7.119(2) Å and b=97.431(7)–97.34(1) °.
    [Show full text]
  • NEW MINERALS It Is Proposed Hereafter to Indicate In.A General Way the Classification of All New Minerals Recoided in This Department
    JOURNAL MINERALOGICAL SOCIETY OF AMENICA 63 Dr. Kunz then spoke of the various city localities and the minerals found therein. He stated that the East Side, from 37 to 110 St., probably afforded the most specimens. The various tunnels and their minerals were spoken of. Capt. Miller called attention to the fine collection of Brooklyn Drift Minerals and Rocks in the collection of the Long Island Historical Society. Ife abo mentioned the occurrence of monazite and xenotime crystals, on the Speedway,Harlem River. Dr. Kunz emphasizedthe irnportance of complete records being kept of all finds. Tnou,q,s L Mrr,r,nn, SecretaryPro, Tem. NEW MINERALS It is proposed hereafter to indicate in.a general way the classification of all new minerals recoided in this department. Subdivision will be first into "families," of which nine may be recognized,as listed in the January number (Am. Min.6 (1), 12,1921). Eachfamilywillbe separatedinto "subfamilies " based on special features of composition. This arrangement is tentative and open to modification, and criticism of it will be welcome, [Eo.] FAMILY 2. SULFIDES, ETC. SosreMrr,v 3. Doust,u suLFrDEs oF METALSAND sEMr-METAr,s. I'LTRABASITE V. Rosrcxf and J. Srnnse-Btinu. Ultrabasit, ein neues Mineral aus Freiberg in Sachsen. (Ultrabasite, a new mineral from Freiberg, Saxony). Rozpr.Eeslcd Ako,il. Prag,25, No. 45, 1916;Z. Krgst. Min., 55,43H39, 1920, Neun: From its extremely basic chemical composition. Pnrsrcar, Pnopnnrrus Color black, somewhat grayish; luster metallic; streak black; cleavage none; fracture scaly, with somewhat greasy luster on the surface. H. : 5; sp. gr.
    [Show full text]