Lab Information Circular Coated Tanzanite
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Some Uncommon Sapphire “Imitations”: Blue Co-Zirconia, Kyanite & Blue Dumortierite Dr Michael S
Some Uncommon Sapphire “Imitations”: Blue Co-zirconia, Kyanite & Blue Dumortierite Dr Michael S. Krzemnicki Swiss Gemmological Institute SSEF [email protected] 筆者滙報數個瑞士珠寶研究院(SSEF)近期收到 in the ring showed a negative RI reading 要求鑑證的藍色寶石,經檢測後確定其中包括 (above 1.79), an isotropic optical character 一些非常罕見的藍寶石模擬石:含錮氧化鋯、 (polariscope) and thus no pleochroism at all. 藍晶石及藍線石等。 Under the microscope, we saw no inclusions, however a slightly greenish reaction under Sapphires are among the most abundant gems the LWSW and there was a weaker similar we receive at the Swiss Gemmological Institute reaction under SWUV lamps. Based on these (SSEF) for testing. From time to time, however, properties and a chemical analysis by X-ray we are quite surprised by the imitations which fluorescence (EDXRF), the blue stone was we find among the goods sent in and this can readily identified as cubic zirconia (ZrO2). then be disappointing news for the clients. In Having seen this artificial product in a wide the following short note, the author presents a range of colours, the author had not previously few uncommon imitations identified recently at seen one of such a saturated and attractive the SSEF. Identification of these imitations is blue. Based on literature (Nassau 1981) the straightforward and should be no problem for analysed traces of cobalt in that stone have any experienced gemmologist. been identified as the colouring element in this specimen. The absorption spectrum of the stone The first case is that of an attractive blue (Fig. 2) – although superposed by several rare faceted stone of approximately 1.4 ct, set in a ring with diamonds (Fig. -
Compilation of Reported Sapphire Occurrences in Montana
Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area .................................... -
HK Fancy Sapphire
Hong Kong, March 2011 Fancy Coloured Sapphires: The Beauty beyond "Blue" of Sapphire and "Red" of Ruby Dr. Michael S. Krzemnicki Swiss Gemmological Institute SSEF Switzerland All photos © M.S. Krzemnicki, SSEF except where indicated. The range of colours... © Swiss Gemmological Institute SSEF 1 The range of colours... © Swiss Gemmological Institute SSEF The range of colours... © Swiss Gemmological Institute SSEF 2 The range of colours... © Swiss Gemmological Institute SSEF The range of colours... © Swiss Gemmological Institute SSEF 3 The range of colours... © Swiss Gemmological Institute SSEF The range of colours... © Swiss Gemmological Institute SSEF 4 The range of colours... © Swiss Gemmological Institute SSEF The range of colours... © Swiss Gemmological Institute SSEF 5 The range of colours... © Swiss Gemmological Institute SSEF The range of colours... © Swiss Gemmological Institute SSEF 6 The range of colours... © Swiss Gemmological Institute SSEF The range of colours... © Swiss Gemmological Institute SSEF 7 The range of colours... © Swiss Gemmological Institute SSEF The range of colours... © Swiss Gemmological Institute SSEF 8 The range of colours... © Swiss Gemmological Institute SSEF The range of colours... Fancy sapphires: The colour range beyond red of rubies and blue of sapphires © Swiss Gemmological Institute SSEF 9 The range of colours... Photo: © SilkenEast Ltd, Bangkok © Swiss Gemmological Institute SSEF The range of colours... Collection: SilkenEast Ltd, Bangkok © Swiss Gemmological Institute SSEF 10 Jewellery with fancy sapphires Photos © Luc Phan, SSEF © Swiss Gemmological Institute SSEF © Swiss Gemmological PhotoInstitute © Luc SSEF Phan, SSEF 11 Corundum Chemical composition: aluminium oxide, Al2O3 Chemical pure aluminium oxide is colourless © Wikipedia In nature always with trace elements (chemical impurities), usually: - Mg, Ti, V, Cr, Fe, Ga - and occasionally rare HFS-elements such as Nb, Sn, Ta, Th Not all trace elements are affecting the colour (e.g. -
Metamorphic and Metasomatic Kyanite-Bearing Mineral
Metamorphic and Metasomatic Kyanite-Bearing Mineral Assemblages of Thassos Island (Rhodope, Greece) Alexandre Tarantola, Panagiotis Voudouris, Aurélien Eglinger, Christophe Scheffer, Kimberly Trebus, Marie Bitte, Benjamin Rondeau, Constantinos Mavrogonatos, Ian Graham, Marius Etienne, et al. To cite this version: Alexandre Tarantola, Panagiotis Voudouris, Aurélien Eglinger, Christophe Scheffer, Kimberly Tre- bus, et al.. Metamorphic and Metasomatic Kyanite-Bearing Mineral Assemblages of Thassos Island (Rhodope, Greece). Minerals, MDPI, 2019, 10.3390/min9040252. hal-02932247 HAL Id: hal-02932247 https://hal.archives-ouvertes.fr/hal-02932247 Submitted on 7 Sep 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. minerals Article Metamorphic and Metasomatic Kyanite-Bearing Mineral Assemblages of Thassos Island (Rhodope, Greece) Alexandre Tarantola 1,* , Panagiotis Voudouris 2 , Aurélien Eglinger 1, Christophe Scheffer 1,3, Kimberly Trebus 1, Marie Bitte 1, Benjamin Rondeau 4 , Constantinos Mavrogonatos 2 , Ian Graham 5, Marius Etienne 1 and Chantal Peiffert -
Scientific Communication
SCIENTIFIC COMMUNICATION NOTES ON FLUID INCLUSIONS OF VANADIFEROUS ZOISITE (TANZANITE) AND GREEN GROSSULAR IN MERELANI AREA, NORTHERN TANZANIA ELIAS MALISA; KARI KINNUNEN and TAPIO KOLJONEN Elias Malisa: University of Helsinki, Department of Geology, SF-00170 Helsinki, Finland. Kari Kinnunen and Tapio Koljonen: Geological Survey of Finland, SF-02150 Espoo, Finland. Tanzanite is a trade name for a gem-quality has been reported in Lalatema and Morogoro in vanadiferous zoisite of deep sapphire-blue colour Tanzania and in Lualenyi and Lilani in Kenya discovered in Merelani area, Tanzania in 1967. (Naeser and Saul 1974; Dolenc 1976; Pohl and This mineral was first described as a strontium Niedermayr 1978). -bearing zoisite by Bank, H. & Berdesinski, W., Crystals of tanzanite occur mainly in bou- 1967. Other minor occurrences of this mineral dinaged pegmatitic veins and hydrothermal frac- Fig. 1. Tanzanite-bearing horizon in the graphite-rich diopside gneiss. The yellow colour indicates hydrothermal alteration, which can be used in pros- pecting for tanzanite. Length of photo ca. 8 m. 54 Elias Malisa, Kari Kinnunen and Tapio Koljonen given as Ca2Al3Si30120H (Ghose & Tsang 1971). The chemical compositions of tanzanites studied are given in Table 1. Unit cell dimensions, measured by X-ray dif- fraction, are a = 16.21, b = 5.55, c = 10.03 ± 0.01 Å in agreement with Hurlbut (1969). Zoisite shows diffraction symmetry mmmPn-a, which limits the possible space groups to Pnma if centric or Pn2, if acentric (Dallace 1968). The most striking property of tanzanite is its pleochroism, which changes from trichroic to dichroic on heating; normally its pleochroism varies: X = red-violet, Y = c = deep blue, Z = a = yellow- Fig. -
VOLUME 45, NO. 80 PLEOCHRONIC MINERALS Wednesday July 28 7:00—9:00 Pm Makiki District Park Administration Building NEXT MONTH
VOLUME 45, NO. 80 JULY 2010 PLEOCHRONIC MINERALS MEETING BY DEAN SAKABE Wednesday Pleochroic minerals are miner- July 28 als that show different colors 7:00—9:00 pm depending on what direction Makiki District you are observing the crystal. Park In order to view pleochroism Administration you need an individual transpar- Building ent crystal. This effect can be very dramatic. Many minerals NEXT MONTH are technically pleochroic, but Wednesday most often the color change is August 25, 2010 so small that it can be barely detected. For those few other LAPIDARY minerals, the color change is very, very obvious. The great- Every Thursday est change is limited to three 6:30-8:30pm colors and is called trichroic(1-3). Second-floor Arts A two color change occurrence and Crafts Bldg is called dichroic (4-5). Pleo- Makiki District chroic, which means "many col- Park ors", is used to cover both of 1-3 Tanzanite with all 3 colors of the natural these color changes. Most of trichroic crystal present and strongly show- ing down different axes of view the time, the color change is MEMBERSHIP limited to shade changes such COSTS as from pale pink to dark pink. 2008 Single: $10.00 Family: $15.00 Rock and Mineral Society of Hawai‛i INC. PLEOCHRONIC MINERALS , PAGE 2 rhombic, monoclinic, and triclinic minerals that can be trichroic. This is because they have three unique axes of symmetry and therefore three unique directions that can absorb light in three different ways. The most famous dichroic mineral is Cordierite, a Magne- sium Aluminum Silicate. -
The Journal of Gemmology Editor: Dr R.R
he Journa TGemmolog Volume 25 No. 8 October 1997 The Gemmological Association and Gem Testing Laboratory of Great Britain Gemmological Association and Gem Testing Laboratory of Great Britain 27 Greville Street, London Eel N SSU Tel: 0171 404 1134 Fax: 0171 404 8843 e-mail: [email protected] Website: www.gagtl.ac.uklgagtl President: Professor R.A. Howie Vice-Presidents: LM. Bruton, Af'. ram, D.C. Kent, R.K. Mitchell Honorary Fellows: R.A. Howie, R.T. Liddicoat Inr, K. Nassau Honorary Life Members: D.). Callaghan, LA. lobbins, H. Tillander Council of Management: C.R. Cavey, T.]. Davidson, N.W. Decks, R.R. Harding, I. Thomson, V.P. Watson Members' Council: Aj. Allnutt, P. Dwyer-Hickey, R. fuller, l. Greatwood. B. jackson, J. Kessler, j. Monnickendam, L. Music, l.B. Nelson, P.G. Read, R. Shepherd, C.H. VVinter Branch Chairmen: Midlands - C.M. Green, North West - I. Knight, Scottish - B. jackson Examiners: A.j. Allnutt, M.Sc., Ph.D., leA, S.M. Anderson, B.Se. (Hons), I-CA, L. Bartlett, 13.Se, .'vI.phil., I-G/\' DCi\, E.M. Bruton, FGA, DC/\, c.~. Cavey, FGA, S. Coelho, B.Se, I-G,\' DGt\, Prof. A.T. Collins, B.Sc, Ph.D, A.G. Good, FGA, f1GA, Cj.E. Halt B.Sc. (Hons), FGr\, G.M. Howe, FG,'\, oo-, G.H. jones, B.Se, PhD., FCA, M. Newton, B.Se, D.PhiL, H.L. Plumb, B.Sc., ICA, DCA, R.D. Ross, B.5e, I-GA, DGA, P..A.. Sadler, 13.5c., IGA, DCA, E. Stern, I'GA, DC/\, Prof. I. -
June 2008 'Tairus' Created Gems: “Part I - Beryl”
Sponsored by Ministry of Commerce & Industry Volume 51 Lab Information Circular June 2008 'Tairus' Created Gems: “Part I - Beryl” In the Volume 49 of Lab Information Circular, November 2007, PleochroismPleochroism: : Dichroism varied from weak in aquamarine to we reported “Synthetic Beryl of Paraiba colour” produced by very strong in darker coloured varieties like purple pink or Tairus Co. Ltd. in order to take the advantage of the popularity of orange red (see figure 2). 'Paraiba' tourmalines. Thereafter, we procured sets of various coloured beryls and corundum from the same manufacturer for our research and reference purpose. The study of these sets has been divided into two parts; this issue describes the study of beryl set, while the study of corundum set will be published in the next issue. 2.a 2.c 2.e The Beryl set consisted of five colour varieties (figure 1), namely, green (emerald), light blue (aquamarine), electric greenish blue (paraiba type), purple pink and orange red. All specimens were facetted as square step and measured 6 X 6 mm. 2.b 2.d 2.f Figure 2 Pleochroic colours of Tairus created Beryls Absorption Spectrum:Spectrum : The spectrum varied as per the colour variety; emerald showed a typical chromium spectrum while 'paraiba' colour displayed a strong band at around 430 nm. Purple pink and orange red varieties exhibited strong bands at 460 to 490 and 550 to 600 nm. UV fluorescence:fluorescence : All samples were inert to long wave as well as short wave UV light. Figure 1 Chelsea Filter Reactioneaction: : Emerald revealed a red glow while all Standard gemmological tests and advanced analysis on FTIR other varieties were either inert or did not displayed any reaction. -
Evaluation of Brilliance, Fire, and Scintillation in Round Brilliant
Optical Engineering 46͑9͒, 093604 ͑September 2007͒ Evaluation of brilliance, fire, and scintillation in round brilliant gemstones Jose Sasian, FELLOW SPIE Abstract. We discuss several illumination effects in gemstones and University of Arizona present maps to evaluate them. The matrices and tilt views of these College of Optical Sciences maps permit one to find the stones that perform best in terms of illumi- 1630 East University Boulevard nation properties. By using the concepts of the main cutter’s line, and the Tucson, Arizona 85721 anti-cutter’s line, the problem of finding the best stones is reduced by E-mail: [email protected] one dimension in the cutter’s space. For the first time it is clearly shown why the Tolkowsky cut, and other cuts adjacent to it along the main cutter’s line, is one of the best round brilliant cuts. The maps we intro- Jason Quick duce are a valuable educational tool, provide a basis for gemstone grad- Jacob Sheffield ing, and are useful in the jewelry industry to assess gemstone American Gem Society Laboratories performance. © 2007 Society of Photo-Optical Instrumentation Engineers. 8917 West Sahara Avenue ͓DOI: 10.1117/1.2769018͔ Las Vegas, Nevada 89117 Subject terms: gemstone evaluation; gemstone grading; gemstone brilliance; gemstone fire; gemstone scintillation; gemstone cuts; round brilliant; gemstones; diamond cuts; diamonds. James Caudill American Gem Society Advanced Instruments Paper 060668R received Aug. 28, 2006; revised manuscript received Feb. 16, 8881 West Sahara Avenue 2007; accepted for publication Apr. 10, 2007; published online Oct. 1, 2007. Las Vegas, Nevada 89117 Peter Yantzer American Gem Society Laboratories 8917 West Sahara Avenue Las Vegas, Nevada 89117 1 Introduction are refracted out of the stone. -
Across the Cascade Range
Series I B> DescriPtive Geology- 4l Bulletin No. 235 \ D, Petrography and Mineralogy, DEPARTMENT'OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES \). WALCOTT, Di HECTOR GEOLOGICAL RECONNAISSANCE ACROSS THE CASCADE RANGE NEAR THE FORTY-NINTH PARALLEL GEORGE OTIS SMITH AND FRANK C. CALKINS WASHINGTON GOVERNMENT PRINTING OFFICE 1904 Trri-o^) SL'BD C 0 N T E N T S. I'lliJO. Letter of transmittal. ---_--_---..-.._-_.____.._-______._....._.._____.._.. 9 Introduction-__-._.__,.__-.----._--._._.__..._....__....---_--__._.__.-.-_- 11 Scope of report ---.--_.____.._______-.--....._---.._...._.__ ._.- 11 Route followed ........................:......................... 12 Geography .............................................................. 12 Topography .......................................................... 12 Primary divisions of the region..--.........-.--.-.--.-.-.. 12 Okanogan Valley .................:.. ............................ 18 Cascade Range ...............:........,..._ ....^......i........ 13 General characteristics..._.....-.....-..----.--.----.-.-..-.. 13 Northern termination.,.---.....-......--.-.............._ 13 Subdivision .............................................. 14 Okanogan Mountains ........................................... 14 Hozonieen Range ............................................ 15 Skagit Mountains....-.... ......-.----....-.-----..-...--.--- 16 Drainage ..................................................... 17 Climate ...................................................... ...... 17 Roads and trails -
Optical Properties of Common Rock-Forming Minerals
AppendixA __________ Optical Properties of Common Rock-Forming Minerals 325 Optical Properties of Common Rock-Forming Minerals J. B. Lyons, S. A. Morse, and R. E. Stoiber Distinguishing Characteristics Chemical XI. System and Indices Birefringence "Characteristically parallel, but Mineral Composition Best Cleavage Sign,2V and Relief and Color see Fig. 13-3. A. High Positive Relief Zircon ZrSiO. Tet. (+) 111=1.940 High biref. Small euhedral grains show (.055) parallel" extinction; may cause pleochroic haloes if enclosed in other minerals Sphene CaTiSiOs Mon. (110) (+) 30-50 13=1.895 High biref. Wedge-shaped grains; may (Titanite) to 1.935 (0.108-.135) show (110) cleavage or (100) Often or (221) parting; ZI\c=51 0; brownish in very high relief; r>v extreme. color CtJI\) 0) Gamet AsB2(SiO.la where Iso. High Grandite often Very pale pink commonest A = R2+ and B = RS + 1.7-1.9 weakly color; inclusions common. birefracting. Indices vary widely with composition. Crystals often euhedraL Uvarovite green, very rare. Staurolite H2FeAI.Si2O'2 Orth. (010) (+) 2V = 87 13=1.750 Low biref. Pleochroic colorless to golden (approximately) (.012) yellow; one good cleavage; twins cruciform or oblique; metamorphic. Olivine Series Mg2SiO. Orth. (+) 2V=85 13=1.651 High biref. Colorless (Fo) to yellow or pale to to (.035) brown (Fa); high relief. Fe2SiO. Orth. (-) 2V=47 13=1.865 High biref. Shagreen (mottled) surface; (.051) often cracked and altered to %II - serpentine. Poor (010) and (100) cleavages. Extinction par- ~ ~ alleL" l~4~ Tourmaline Na(Mg,Fe,Mn,Li,Alk Hex. (-) 111=1.636 Mod. biref. -
SYNTHETIC GEM MATERIALS in the 2000S GEMS & GEMOLOGY WINTER 2010 Figure 1
SYNTHETIC GEM MATERIALS INTHE2000S: A DECADE IN REVIEW Nathan Renfro, John I. Koivula, Wuyi Wang, and Gary Roskin The first decade of the 2000s brought a constant flow of previously known synthetics into the marketplace, but little in the way of new technology. The biggest development was the commer- cial introduction of faceted single-crystal gem-quality CVD synthetic diamonds. A few other inter- esting and noteworthy synthetics, such as Malossi hydrothermal synthetic emeralds and Mexifire synthetic opals, also entered the market. Identification of synthetic gem materials continued to be an important function of—and, in some cases, challenge for—gemologists worldwide. he development of synthetics and the method- lished literature that the most significant develop- ologies used to detect new and existing materi- ments—and the focus of most research—during this Tals is of great importance to the international decade involved the production of gem-quality syn- gem community. Indeed, whether a synthetic gem thetic diamonds, primarily those grown by the com- was grown in the 2000s or the 1880s, today’s gemol- paratively new CVD (chemical vapor deposition) ogists must still be prepared to deal with it. Many process. Who can forget the September 2003 cover of synthetic gems were prominent in the marketplace Wired magazine, with a diamond-pavéd “supermod- in the first decade of the 2000s (see, e.g., figure 1). el” next to the headlines “$5 a carat. Flawless. Made The decade also saw some new synthetics. Among in a lab.”? This article proclaimed that “The dia- the synthetic colored stones introduced was the mond wars have begun,” and touted the potential for Malossi hydrothermal synthetic emerald (Adamo et outright cheap but extremely high-quality colorless al., 2005), which was gemologically similar to both and fancy-colored synthetic diamonds grown by two Russian synthetic emeralds and those manufactured very different processes (CVD and HPHT).