Gem Quality Johachidolite: Occurrence, Chemical Composition and Crystal Structure
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New Mineral Names*
American Mineralogist, Volume 73, pages 1492-1499. 1988 NEW MINERAL NAMES* JOHN L. JAMBOR CANMET, 555 Booth Street, Ottawa, Ontario KIA OGI, Canada ERNST A. J. BURKE lnstituut voor Aardwetenschappen, Vrije Universitiete, De Boelelaan 1085, 1081 HV, Amsterdam, Netherlands T. SCOTT ERCIT, JOEL D. GRICE National Museum of Natural Sciences, Ottawa, Ontario KIA OM8, Canada Acuminite* prismatic to acicular crystals that are up to 10 mm long and 0.5 H. Pauly, O.Y. Petersen (1987) Acuminite, a new Sr-fluoride mm in diameter, elongate and striated [001], rhombic to hex- from Ivigtut, South Greenland. Neues Jahrb. Mineral. Mon., agonal in cross section, showing {l00} and {l10}. Perfect {100} 502-514. cleavage, conchoidal fracture, vitreous luster, H = 4, Dm'.. = 2.40(5) glcm3 (pycnometer), Dcale= 2.380 glcm3 for the ideal Wet-chemical analysis gave Li 0.0026, Ca 0.0185, Sr 37.04, formula, and Z = 4. Optically biaxial positive, a = 1.5328(4), (3 Al 11.86, F 33.52, OH (calc. from anion deficit) 6.82, H20 (calc. = 1.5340(4), 1.5378(4), 2 Vmoa,= 57(2)°, 2 Vcale= 59°; weak assuming 1 H20 in the formula) 7.80, sum 97.06 wt%, corre- 'Y = dispersion, r < v; Z = b, Y A c = -10°. X-ray structural study sponding to Sro98AIl.o2F.o7(OH)o.93H20. The mineral occurs as indicated monoclinic symmetry, space group C21c, a = 18.830(2), aggregates of crystals shaped like spear points and about I mm b= I 1.517(2), c= 5.190(I)A,{3 = 100.86(1)°. A Guinierpowder long. -
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. -
Winter 2005 Gems & Gemology
G EMS & G VOLUME XLI WINTER 2005 EMOLOGY W INTER 2005 P AGES 295–388 Dr. Edward J. Gübelin V OLUME (1913–2005) 41 N O. 4 THE QUARTERLY JOURNAL OF THE GEMOLOGICAL INSTITUTE OF AMERICA ® Winter 2005 VOLUME 41, NO. 4 EDITORIAL _____________ 295 One Hundred Issues and Counting... Alice S. Keller 297 LETTERS ________ FEATURE ARTICLES _____________ 298 A Gemological Pioneer: Dr. Edward J. Gübelin Robert E. Kane, Edward W. Boehm, Stuart D. Overlin, Dona M. Dirlam, John I. Koivula, and Christopher P. Smith pg. 299 Examines the prolific career and groundbreaking contributions of Swiss gemologist Dr. Edward J. Gübelin (1913–2005). 328 Characterization of the New Malossi Hydrothermal Synthetic Emerald Ilaria Adamo, Alessandro Pavese, Loredana Prosperi, Valeria Diella, Marco Merlini, Mauro Gemmi, and David Ajò Reports on a hydrothermally grown synthetic emerald manufactured since 2003 in the Czech Republic. Includes the distinctive features that can be used to separate this material from natural and other synthetic emeralds. pg. 337 REGULAR FEATURES _____________________ 340 Lab Notes Yellow CZ imitating cape diamonds • Orange diamonds, treated by multiple processes • Pink diamonds with a temporary color change • Unusually large novelty-cut diamond • Small synthetic diamonds • Diaspore “vein” in sapphire • Unusual pearl from South America • Unusually small natural-color black cultured pearls • Identification of turquoise with diffuse reflectance IR spectroscopy 350 Gem News International Ornamental blueschist from northern Italy • Emerald phantom crystal • Unusual trapiche emerald earrings • Large greenish yellow grossular from Africa • Opal triplet resembling an eye • Green orthoclase feldspar from pg. 340 Vietnam • New discoveries of painite in Myanmar • Gem plagioclase reported- ly from Tibet • Spinel from southern China • Update on tourmaline from Mt. -
Spring 2003 Gems & Gemology
Spring 2003 VOLUME 39, NO. 1 EDITORIAL 1 In Honor of Dr. Edward J. Gübelin Alice S. Keller FEATURE ARTICLES ______________ 4 Photomicrography for Gemologists John I. Koivula Reviews the fundamentals of gemological photomicrography and introduces new techniques, advances, and discoveries in the field. pg. 16 NOTES AND NEW TECHNIQUES ________ 24 Poudretteite: A Rare Gem Species from the Mogok Valley Christopher P. Smith, George Bosshart, Stefan Graeser, Henry Hänni, Detlef Günther, Kathrin Hametner, and Edward J. Gübelin Complete description of a faceted 3 ct specimen of the rare mineral poudretteite, previously known only as tiny crystals from Canada. 32 The First Transparent Faceted Grandidierite, from Sri Lanka Karl Schmetzer, Murray Burford, Lore Kiefert, and Heinz-Jürgen Bernhardt Presents the gemological, chemical, and spectroscopic properties of the first known transparent faceted grandidierite. pg. 25 REGULAR FEATURES __________________________________ 38 Gem Trade Lab Notes • Diamond with fracture filling to alter color • Intensely colored type IIa diamond with substantial nitrogen-related defects • Diamond with unusual overgrowth • Euclase specimen, with apatite and feldspar • “Cherry quartz” glass imitation • Cat’s-eye opal • “Blue” quartz • Heat-treated ruby with a large glass-filled cavity • Play-of-color zircon 48 Gem News International • 2003 Tucson report • Dyed “landscape” agate • Carved Brazilian bicolored beryl and Nigerian tourmaline • New deep pink Cs-“beryl” from Madagascar • New demantoid find in Kladovka, Russia • Fire opal from Oregon pg. 33 • Cultured pearls with diamond insets • Gemewizard‰ gem communication and trading software • AGTA corundum panel • European Commission approves De Beers Supplier of Choice initiative • Type IaB diamond showing “tatami” strain pattern • Poldervaartite from South Africa • Triphylite inclusions in quartz • LifeGem synthetic diamonds • Conference reports • Announcements 65 The Dr. -
Formation of Large Synthetic Zincite (Zno) Crystals During Production of Zinc White
257 Formation of large synthetic zincite (ZnO) crystals during production of zinc white John W. Nowak1†, R.S.W. Braithwaite2, J. Nowak3, K. Ostojski4, M. Krystek5 and W. Buchowiecki6 1. 71 Glenhurst Avenue, Bexley, Kent, DA5 3QH 2. School of Chemistry, University of Manchester, Manchester, M13 9PL Email: [email protected] 3. Jelenia 4, 92-309 Lodz, Poland. Email: [email protected] 4. Olawa S.A. Foundry, Olawa, Poland 5. Geological Museum, University of Lodz, 90-142 Lodz, Kopcinskiego 31, Poland Email: [email protected] 6. Mieszczanska 17/40, 93-322 Lodz, Poland. Email: [email protected] (corresponding author) Abstract: Remarkable zincite crystals have formed as a by-product of zinc white production in Olawa Foundry, Poland. Some are of gem quality and have been faceted. Small primary crystals formed by reaction of zinc vapour with carbon dioxide from fuel burning gases leaking through faults in a diaphragm of a retort furnace. Some of these have undergone carbon monoxide-promoted and zinc vapour-assisted sublimation to form large secondary crystals. Many of these crystals are brightly coloured and transparent, and have been found up to 2 kg in weight. Most of the crystals are fluorescent in ultraviolet light. Keywords: chemical assisted sublimation, crystal growth, zinc oxide, zincite Introduction Zincite is a relatively rare natural oxide of of rare fluorescent species (Palache, 1935; zinc, with the ideal formula ZnO. The world’s Bancroft, 1984). Zincite occurs here mainly largest deposit of zincite is near Franklin and as a massive material or as small granules Ogdensburg, Sussex County, New Jersey, with other major zinc-bearing minerals such USA. -
Laurentthomasite, Mg K(Be2al)Si12o30
Eur. J. Mineral., 32, 355–365, 2020 https://doi.org/10.5194/ejm-32-355-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Laurentthomasite, Mg2K(Be2Al)Si12O30: a new milarite-group-type member from the Ihorombe region, Fianarantsoa Province, Madagascar Cristiano Ferraris1, Isabella Pignatelli2, Fernando Cámara3, Giancarlo Parodi1, Sylvain Pont1, Martin Schreyer4, and Fengxia Wei5 1Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie, UMR 7590, Muséum National d’Histoire Naturelle, CP 52, 61 rue Buffon, 75005 Paris, France 2Laboratoire GeoRessources, Université de Lorraine, Faculté des Sciences et Technologies, Rue Jacques Callot, BP 70239, 54506 Vandœuvre-lès-Nancy, France 3Dipartimento di Scienze della Terra “A. Desio”, Università degli Studi di Milano, Via Mangiagalli, 34 – 20133 Milan, Italy 4Malvern Panalytical B.V., Lelyweg 1 (7602 EA), P.O. Box 13, 7600 AA Almelo, the Netherlands 5Institute of Materials Research and Engineering (IMRE), 2 Fusionopolis Way, Innovis, #08-03, 138634 Singapore Correspondence: Cristiano Ferraris ([email protected]) Received: 12 February 2020 – Revised: 6 May 2020 – Accepted: 14 May 2020 – Published: 17 June 2020 Abstract. Laurentthomasite, ideally Mg2K(Be2Al)Si12O30, is a new milarite-group member found within quartz-syenite pegmatites from the Ihorombe region, Fianarantsoa Province, Madagascar. It occurs as euhedral {0001} hexagonal crystals, maximum 15 mm large and 5 mm thick. The crystals show a very strong dichroism with cobalt blue and green-yellow colours when observed along [0001] and [1000], respectively. The mineral is transparent, uniaxial (C) and its lustre is vitreous. The hardness is about 6 (Mohs scale), showing a poor {0001} cleavage, irregular to conchoidal fracture, and a measured density of 2.67(8) g cm−3. -
Volume 36/ No. 5/ 2019
Volume 36 / No. 5 / 2019 Inclusions in Burmese Spinel Peridot from China and N. Korea Connemara Marble Gem Faceting in Sri Lanka Examination of ‘Coconut Pearls’ Volume 36 / No. 5 / 2019 Cover photo: Burmese spinel is available as attractive crystals and colourful gemstones, and a detailed study of the inclusions in this material appears on pp. COLUMNS 418–435 of this issue. The Burmese spinels shown here include the 6.30 ct centre stone in a gold and carbon-fiber ring that was designed and manufactured by What’s New 393 Marc Höllmüller for Carley Jewels (Chattanooga, Tennessee, USA), as well as GemPen | J-Certain Synthetic three larger and nine smaller crystals (courtesy of Federico Barlocher, Como, Diamond Detector | Sherlock Italy, and Kathryn Bonanno, New York, New York, USA, respectively) and numerous cut gemstones that weigh up to 10.48 ct (courtesy of RareSource, Holmes 2.0 Synthetic Diamond Chattanooga Tennessee, USA). Photo by Jeff Scovil. Detector | ABN-AMRO Diamond Reports | AGTA GemFair Tucson Seminars | Gem Abstracts from ARTICLES the 16th Swiss Geoscience Meeting | Gem Abstracts from Spinel from Mogok, Myanmar—A Detailed Inclusion Study by 418 the 2018 GSA Annual Meeting | Raman Microspectroscopy and Scanning Electron Microscopy Gem Identification Pamphlet By Myint Myat Phyo, Eva Bieler, Leander Franz, and Poster | GIT Reports on Colour-Change Grossular and Walter Balmer and Michael S. Krzemnicki Musgravite | Global Diamond Industry 2018 | Gold Demand Characterisation of Peridot from China’s Jilin Province 436 Trends 2018 -
Bumble Bee Stone from Indonesia Tracking and Traceability
Volume 36 / No. 3 / 2018 Bumble Bee Stone from Indonesia Tracking and Traceability in the Gem Industry Circling on Ming Cultured Pearls Volume 36 / No. 3 / 2018 Volume 36 / No. 3 / 2018 Cover photo: Bumble Bee Stone from Indonesia is an unusual carbonate- rich rock that is coloured by arsenic sulphide minerals and may also contain COLUMNS black areas of ‘sooty’ pyrite. A pattern resembling an erupting volcano is Bumble Bee Stone seen in this cabochon (45 × 65 mm), and is reminiscent of the volcanic from Indonesia Tracking and Traceability What’s New 181 origin of this gem. Courtesy of Rare Earth Mining Company. in the Gem Industry Circling on Alrosa Diamond Inspector | Ming Cultured Pearls D-Tect | DiaColor Colorimeter | Torcia 365 Long-wave LED Flashlight | Amberif 2017 and 2018 Proceedings | EGU General ARTICLES Assembly 2018 Gem Abstracts | FTC’s ‘Jewelry Guides’ Revised | Blockchain, Chain of Custody and Trace Elements: 212 Governing the Gemstone Sector: An Overview of Tracking and Traceability Opportunities Lessons from Global Experience | in the Gem Industry GSJ 2018 Annual Meeting By Laurent E. Cartier, Saleem H. Ali and Michael S. Krzemnicki Abstracts | PGI Insight 2018 | Sapphires from Mogok, Bumble Bee Stone: A Bright Yellow-to-Orange and 228 Myanmar | Wooshin Gem Lab Black Patterned Gem from West Java, Indonesia Magazine | Yellow Diamonds Educational Video | Call for By Emmanuel Fritsch and Joel Ivey Papers: Gem Issue of The An Explanation of a Specific Type of Circling as Extractive Industries and Society 240 | Diamond Museum -
Gemological Analysis of Some Rare Gemstones from Mogok Area, Mandalay Region
ICIC Express Letters Part B: Applications ICIC International c 2020 ISSN 2185-2766 Volume 11, Number 11, November 2020 pp. 1077–1086 GEMOLOGICAL ANALYSIS OF SOME RARE GEMSTONES FROM MOGOK AREA, MANDALAY REGION Htin Lynn Aung1 and Thi Thi Zin2 1Department of Geology Dawei University Kamyawgin Village, Loung Lone Township, Tanintharyi, Myanmar [email protected] 2Graduate School of Engineering University of Miyazaki 1-1, Gakuen Kibanadai-nishi, Miyazaki-City 889-2192, Japan [email protected] Received March 2020; accepted June 2020 Abstract. Mogok has long been noted as a supplier of various gemstones over the past decades. The principal gemstones are ruby, sapphire and spinel. Nowadays, fabulous rare gemstones from Mogok are being sold in foreign markets. This area is mainly composed of igneous and metamorphic rocks. Exceptionally rare gemstones are also discovered and they are johachidolite, poudretteite, thorite, etc. The fantastic occurrences of rare gemstones provoke attraction and well attention to mineralogists and gemmologists. Most of the rare gemstones in the present research work are studied from gems dealers from Mogok. Other rare samples are recorded and studied in the favor of the gems collectors. The data on primary occurrence of these rare gemstones are still uncertain and further investigation should be required. In the Mogok area, these rare minerals are recovered from alluvial, eluvial, residual deposits along the riverside, hill slope, flat plains and low- lying area. Economically, rare gemstones are highly important for both local and foreign gem markets. Some gemstones are important economically as well as technologically for its composition, such as thorite and beryl, which are used in space and aeronautical purposes. -
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. -
Mg2si6o18, a New Mineral of the Beryl Group from the Gem Deposits of Mogok, 3 Myanmar
This is the peer-reviewed, final accepted version for American Mineralogist, published by the Mineralogical Society of America. The published version is subject to change. Cite as Authors (Year) Title. American Mineralogist, in press. DOI: https://doi.org/10.2138/am-2021-7785. http://www.minsocam.org/ 1 REVISION 1 2 Johnkoivulaite, Cs(Be2B)Mg2Si6O18, a new mineral of the beryl group from the gem deposits of Mogok, 3 Myanmar 4 Aaron C. Palke1*, Lawrence M. Henling2, Chi Ma3, George R. Rossman3, Ziyin Sun1, Nathan Renfro1, 5 Anthony R. Kampf4, Kyaw Thu5, Nay Myo6, Patcharee Wongrawang7, Vararut Weeramonkhonlert7 6 7 1Gemological Institute of America, Carlsbad, CA 92008, USA 8 2Beckman Institute, California Institute of Technology, Pasadena, CA 91125, USA 9 3Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, 10 USA 11 4Mineral Sciences Department, Natural History Museum of Los Angeles County, Los Angeles, California 12 90007, USA 13 5S Gemmological Institute, Yangon 11201, Myanmar 14 6Greatland Gems and Jewelry, Mogok 11101, Myanmar 15 7Gemological Institute of America, Bangkok 10500, Thailand 16 *E-mail: [email protected] 17 18 Abstract 19 A new mineral of the beryl group, johnkoivulaite, Cs(Be2B)Mg2Si6O18, was recovered from the gem 20 gravels of the Pein Pyit area of the Mogok region in Myanmar. Thus far, only a single crystal has been 21 identified. It has dimensions about 5.8×5.7×5.5 mm. This specimen has an irregular shape but still has 22 discernible crystal form with geometric growth patterns observed on the crystal faces. The crystal of 23 Johnkoivulaite is grayish-violet in color and strongly pleochroic going from nearly colorless with Ec to 24 dark bluish-violet with E||c.