Summer 1982 Gems & Gemology
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Rhodochrosite Gems Unstable Colouration of Padparadscha-Like
Volume 36 / No. 4 / 2018 Effect of Blue Fluorescence on the Colour Appearance of Diamonds Rhodochrosite Gems The Hope Diamond Unstable Colouration of in London Padparadscha-like Sapphires Volume 36 / No. 4 / 2018 Cover photo: Rhodochrosite is prized as both mineral specimens and faceted stones, which are represented here by ‘The Snail’ (5.5 × 8.6 cm, COLUMNS from N’Chwaning, South Africa) and a 40.14 ct square-cut gemstone from the Sweet Home mine, Colorado, USA. For more on rhodochrosite, see What’s New 275 the article on pp. 332–345 of this issue. Specimens courtesy of Bill Larson J-Smart | SciAps Handheld (Pala International/The Collector, Fallbrook, California, USA); photo by LIBS Unit | SYNTHdetect XL | Ben DeCamp. Bursztynisko, The Amber Magazine | CIBJO 2018 Special Reports | De Beers Diamond ARTICLES Insight Report 2018 | Diamonds — Source to Use 2018 The Effect of Blue Fluorescence on the Colour 298 Proceedings | Gem Testing Appearance of Round-Brilliant-Cut Diamonds Laboratory (Jaipur, India) By Marleen Bouman, Ans Anthonis, John Chapman, Newsletter | IMA List of Gem Stefan Smans and Katrien De Corte Materials Updated | Journal of Jewellery Research | ‘The Curse Out of the Blue: The Hope Diamond in London 316 of the Hope Diamond’ Podcast | By Jack M. Ogden New Diamond Museum in Antwerp Rhodochrosite Gems: Properties and Provenance 332 278 By J. C. (Hanco) Zwaan, Regina Mertz-Kraus, Nathan D. Renfro, Shane F. McClure and Brendan M. Laurs Unstable Colouration of Padparadscha-like Sapphires 346 By Michael S. Krzemnicki, Alexander Klumb and Judith Braun 323 333 © DIVA, Antwerp Home of Diamonds Gem Notes 280 W. -
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. -
Preliminary Investigation of Purple Garnet from a New Deposit in Mozambique
GIT GEMSTONE UPDATE Preliminary Investigation of Purple Garnet from a New Deposit in Mozambique By GIT-Gem testing laboratory 11 May 2016 Introduction In March 2016, a group of Thai gem dealer led by Mr. Pichit Nilprapaporn paid a visit to the GIT and informed us about a new garnet deposit in Mozambique, that was discovered near the western border with Zimbabwe. They also displayed a large parcel of rough and a few cut stones claimed to be the material found in this new deposit (Figure 1). According to the stone’s owner, these garnet specimens were unearthed from an unconsolidated sediment layer, just a few meters below ground surface. This brief report is our preliminary investigation on the interesting vivid purple garnet from the new deposit in Mozambique. Figure 1: Mr. Pichit Nilprapaporn (center), the stone’s owner, showing a large parcel of purple gar- net roughs claimed to be from a new deposit in Mozambique to the GIT director (left). The Gem and Jewelry Institute of Thailand (Public Organization) 140, 140/1-3, 140/5 ITF-Tower Building. 1st - 4th and 6th Floor,Silom Road, Suriyawong, Bangrak, Bangkok 10500 Thailand Tel: +66 2634 4999 Fax: +66 2634 4970; Web: http://www.git.or.th; E-mail: [email protected] 11 May, 2016 Preliminary Investigation of Purple Garnet from a New Deposit in Mozambique 2 Samples and Testing Procedure The stone’s owners donated some specimens (one 6.10 ct oval-facetted stone and 13 rough samples weighing from 3.83 to 9.43 cts) to the GIT Gem Testing Laboratory for studying. -
Phenomenal Gemstones Possess Striking Optical Effects, Making Them Truly a Sight for Sore Eyes
THE PHENOMENAL PROPERTIES OF GEMS Phenomenal gemstones possess striking optical effects, making them truly a sight for sore eyes. Here is GIA’s guide to understanding what makes each phenomenon so uniquely brilliant. ASTERISM CROSSING BANDS OF REFLECTED LIGHT CREATE A SIX-RAYED STAR-LIKE APPEARANCE. ASTERISM OCCURS IN THE DOME OF A CABOCHON, AND CAN BE SEEN IN GEMS LIKE RUBIES AND SAPPHIRES. ADULARESCENCE THE SAME SCATTERING OF LIGHT THAT MAKES THE SKY BLUE CREATES A MILKY, BLUISH-WHITE GLOW, LIKE MOONLIGHT SHINING THROUGH A VEIL OF CLOUDS. MOONSTONE IS THE ONLY GEM THAT DISPLAYS IT. AVENTURESCENCE FOUND IN NATURAL GEMS LIKE SUNSTONE FELDSPAR AND AVENTURINE QUARTZ, IT DISPLAYS A GLITTERY EFFECT CAUSED BY LIGHT REFLECTING FROM SMALL, FLAT INCLUSIONS. CHATOYANCY OTHERWISE KNOWN AS THE “CAT’S EYE” EFFECT, BANDS OF LIGHT ARE CAUSED BY THE REFLECTION OF LIGHT FROM MANY PARALLEL, NEEDLE-LIKE INCLUSIONS INSIDE A CABOCHON. NOTABLE GEMS THAT DISPLAY CHATOYANCY INCLUDE CAT’S EYE TOURMALINE AND CAT’S EYE CHRYSOBERYL. IRIDESCENCE ALSO SEEN IN SOAP BUBBLES AND OIL SLICKS, IT’S A RAINBOW EFFECT THAT IS CREATED WHEN LIGHT IS BROKEN UP INTO DIFFERENT COLORS. LOOK FOR IT IN FIRE AGATE AND OPAL AMMONITE (KNOWN BY THE TRADE AS AMMOLITE). LABR ADORESCENCE A BROAD FLASH OF COLOR THAT APPEARS IN LABRADORITE FELDSPAR, IT’S CAUSED BY LIGHT INTERACTING WITH THIN LAYERS IN THE STONE, AND DISAPPEARS WHEN THE GEM IS MOVED. INSIDER’S TIP: THE MOST COMMON PHENOMENAL COLOR IN LABRADORITE IS BLUE. PLAY OF COLOR THE FLASHING RAINBOW-LIKE COLORS IN OPAL THAT FLASH AT YOU AS YOU TURN THE STONE OR MOVE AROUND IT. -
Garnet Cigdem Lule, Phd., FGA, GG (GIA)
Market Trends Garnet Cigdem Lule, PhD., FGA, GG (GIA) he Tucson 2015 Gem Show demonstrated that there are considerably more options than just the big three (Truby, sapphire and emerald) for buyers seeking fine quality gemstones. The availability of bigger and higher Figure 1. Tsavorite garnet quality garnets in a range of colors, including color- 6.00cts. Courtesy change was notable. Gem professionals know only too of Mayer & Watt, well that, although red garnets are common, it is no easy photo by Geoffrey task to locate a fine quality rhodolite or spessartine of Watt. 10cts or larger. Dealers with fine red garnets in these sizes reported that the issue isn’t with demand; it is with trying to replace the stone after it’s sold. Similarly, in the Rhodolite 3 carats Commercial Good Fine Extra Fine 2005 4-18 18-35 35-50 50-60 2010 4-18 18-35 35-60 60-70 2015 4-22 30-50 60-95 120-140 Tsavorite 3 carats Commercial Good Fine Extra Fine 2005 225 & up 675-1,000 1,000-1,300 1,300-2,000 2010 240 & up 800-1,400 1,400-1,900 1,900-2,850 2015 240-450 1,150-1,725 2,000-2,400 3,000-3,500 Note. Current price tables have 10 categories but for representation here, categories are combined to show only the four main quality grades. orange category, fine grade mandarin garnets are also their own merit. The per carat price, one of the highest once again achieving greater popularity, and prices are for any garnet, is proof enough of that. -
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. -
History of the Gems Found in North Carolina
'I F \1111111:1111'11\\' .'·f .1 (;,,..r'j, >'IJ·I .. , I· I,.t 'I I ,~ /'t\1 t(l~'F-" (-- , ,'. ,',' I.~ .()U~lr., , l' _,\ .... +'" .... (.Jf'J.:"') i ~ j' ~" . ..... ," - (" , .. - "'r' .. BARVARD UNIVERSITY LIBRARY OF THE MINERALOGICAL LABORATORY UNIVERSITY MUSEUM Transferred to CABOT SCIENCE LIBRARY June 2005 I ~/~_ . Digitized by Google • HISTORY OF THE GEMS FOUND IN NORTH CAROLINA H GIIORGB lI'RBDBRICE KUNZ, PH.D. Digitized by Google NORTH CAROLINA GEOLOGICAL lAND ECONOMIC SURVEY JOSEPH HYDE PRATT, STATE GEOLOGIST BULLETIN NO. 12 HISTORY OF THE GEMS FOUND IN NORTH CAROLINA BY GEORGE FREDERICK KUNZ, PH.D. RALEIGH E. M. UZZELL .t Co., PUBLIO PaINTEB8 AND BINDD8 1907 Digitized byGQogle BOARD GovJm.NOB R. B. GLDN," of/lClo Olaoirm.cm •.....•••••••••••.• Raleigh. BuBy FBD:8. • • • . • • • • . .. • • • • . • • • .. • • .. • •••.••• Wlnlton·Salem. s.wrrr. ... ....... , .... " ...... • ... Asheville. HUGH MAoR.&l: ... ..................................•....... Wllmlngton. lI'Iu.NK WOOD .•.................................•.......... llIdenton. GeologiBt. '" .... .. .. Chapel .' Digitized LETTER OF TRANSMITTAL CHAPEL HILL, N. C., November 15, 1906. To Bil E:Z;C6lZency, HON. R. B. GLENN, G01J6mof' of N orl.h Ocwolina. B1,r.-I have the honor to submit for publication as Bulletin No. 12 of the Geological and Economic Survey, the report of Dr. George Frederick Kunz on the History of the Gems found in North Carolina. Yours obediently, JOSEPH HYDE PUTT, 8tate Geologist. Digitized by Google CONTENTS P.GJC PBD.CJC "............................................................. Ill: Ilft'aODUCTIOK .......................... .. • .. .. .. • • • .. • • • .. • • .. .. • .. • • %1 ClU.Pl'EB I.-HISTOBIc.&L 8KJCTCB: 01' GJCK xmmG m NOBTH C.aoLIK.. • • • 1 II.-DL\J(OKDB • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • 5 III.-COBUNDl1J( GJCK8 ••••••••••••••••••••••••••••••••••••••• 10 IV.-GBK HINEB.&L8 01' THJC ne-.'l'1'1'JC Dm.. • • . • • • • . • • • • . • • 25 The feldspars •....•...•...•••••••••••••••••..••••••• J7 Orthoclase . -
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. -
Star Stones (Asterism)
Learning Series: Basic Rockhound Knowledge Star Stones (Asterism) When parallel, needle-like inclusions, or tube-like channels, are oriented along two or more of the crystal faces of a mineral, and when that stone is cut as a domed cabochon, a four- to six-rayed figure is displayed on the dome. This phenomenon of reflected light is called "asterism" and the gems are called star stones. The most commonly seen examples are star corundums; where there are inclusions of titanium oxide (rutile or "silk") parallel to three crystal faces giving a six-rayed star. In rare cases, a twinned crystal slightly offset with its own set of rutile needles can lead to the formation of a twelve-rayed star. Although rutile is an extremely common inclusion in sapphire, few good, natural, star sapphires are found. One of the major reasons is that the heating, which is almost universally done to sapphire rough, dissolves rutile needles; clarifying and sometimes color enhancing the stone, yes, but eliminating potential stars! [Rutile needles (silk) aligned in three directions in unheated corundum] [Star ruby, white star sapphire ring, rare bi-colored star sapphire] The only other gem which commonly forms stars is quartz, where the phenomenon tends to be more visible in transmitted than in reflected light. In this species, rose quartz is the most frequently asterated variety. Most citrine in commerce has been heated, which tends to dissolve the fine rutile inclusions necessary for star formation, so it is rather rare. In fine, near-transparent quartzes which have been cut to a spherical shape, multiple stars can form an intersecting pattern over the surface. -
Mining, Geology, and Geological History of Garnet at the Barton Garnet Mine, Gore Mountain, New York William Kelly
6: RARE EARTH ELEMENT AND YTTRIUM MINERAL OCCURENCES IN THE ADIRONDACK MOUNTAINS 7 MINING, GEOLOGY, AND GEOLOGICAL HISTORY OF GARNET AT THE BARTON GARNET MINE, GORE MOUNTAIN, NEW YORK WILLIAM KELLY New York State Geologist, Emeritus, Division of Research and Collections, New York State Museum, Albany, NY 12230, [email protected] KEYWORDS: Garnet, Mining, Gore Mountain, Metamorphism, Lyon Mountain Granite ABSTRACT Garnet megacrysts commonly 30 centimters (cm) ranging up to 1 meter (m) in diameter occur at the summit of Gore Mountain, Adirondacks, NY and were mined there for abrasives for more than a century. The mine, owned by Barton Mines Co., LLC, is roughly 2 km x 150 m and is located in a hornblende-rich garnet amphibolite at the southern boundary of a metamorphosed olivine gabbro body that is in fault contact with charnockite. Barton supplies garnet, a chemically homogeneous pyrope-almandine, to the waterjet cutting, lapping, and abrasive coatings industries. The garnet megacrysts are reliably dated at 1049 ± 5 Ma. The growth of the garnet megacrysts was facilitated by an influx of hydrothermal fluid emanating from the ore body’s southern boundary fault. The fluids were most probably associated with the intrusion of the Lyon Mountain Granite (1049.9 ± 10 Ma) and/or associated pegmatitic rocks late in the tectonic history of the Adirondacks. INTRODUCTION The Adirondack Mountains in upstate New York are a small outlier of a larger body of rocks of similar age and geologic history that is located to the north in Canada. The Adirondack region can be loosely divided into amphibolite metamorphic facies Lowlands, in the northwest, and the granulite facies Central Highlands, which are 86 THE ADIRONDACK JOURNAL OF ENVIRONMENTAL STUDIES VOLUME 21 87 7: MINING, GEOLOGY, AND GEOLOGICAL HISTORY OF GARNET AT THE BARTON GARNET MINE, GORE MOUNTAIN, NEW YORK separated by a very large, northwest-dipping fault zone. -
Tiara Pair of Earrings in Chinoiserie Style
1 1. Italy or France Tiara Gold and coral, about 1817 Purchased with funds given by Rita Barbour Kern, 1996.27 French Neoclassicism revived the fashion for wearing a tiara, a head ornament based on an ancient Greek diadem. Tiaras of varying degrees of intrinsic value were worn by every woman from the middle classes to royalty. Coral, which was believed to posses protective powers, was often used in jewelry for children and young adults. A portrait painted by Luigi Bernero in 1817 of Maria Teresa of Savoy (1803– 1879) shows the 14-year-old Italian princess wearing a hair ornament almost exactly like this tiara. Most coral in Europe came from the sea around Naples and nearby Torre del Greco. In the 19th century coral jewelry became a fashionable souvenir. This was partly because people could travel more once the Napoleonic wars had ended in 1815, but also due to the growing popularity of Luigi Bernero (Italy, 1775–1848), Maria Teresa di Savoia. Oil on canvas, naturalistic jewelry in the 1850s. about 1817. Palazzo Reale, Turin, Italy 2. and pagoda-shaped elements of these earrings reflect the England period’s romantic taste for the Far East, known as chinoiserie Pair of Earrings in (sheen-WAH-zer-ee). Chinoiserie Style Pierced earrings were a sign of maturity. The first pair of earrings was usually given to a young girl in England at Silver, gold, diamonds, pearls and rubies, age 16, when simple ‘top-and-drop’ pearl earrings were considered to be more appropriate for a young, unmarried about 1820 girl. -
The Minerals of Tasmania
THE MINERALS OF TASMANIA. By W. F. Petterd, CM Z.S. To the geologist, the fascinating science of mineralogy must always be of the utmost importance, as it defines with remarkable exactitude the chemical constituents and com- binations of rock masses, and, thus interpreting their optical and physical characters assumed, it plays an important part part in the elucidation of the mysteries of the earth's crust. Moreover, in addition, the minerals of a country are invari- ably intimately associated with its industrial progress, in addition to being an important factor in its igneous and metamorphic geology. In this dual aspect this State affords a most prolific field, perhaps unequalled in the Common- wealth, for serious consideration. In this short article, I propose to review the subject of the mineralogy of this Island in an extremely concise manner, the object being, chiefly, to afford the members of the Australasian Association for the Advancement of Science a cursory glimpse into Nature's hidden objects of wealth, beauty, and scientific interest. It will be readily understood that the restricted space at the disposal of the writer effectually prevents full justice being done to an absorbing subject, which is of almost universal interest, viewed from the one or the other aspect. The economic result of practical mining operations, as carried on in this State, has been of a most satisfactory character, and has, without doubt, added greatly to the national wealth ; but, for detailed information under this head, reference must be made to the voluminous statistical information, and the general progress, and other reports, issued by the Mines Department of the local Government.