Summer 2002 Gems & Gemology

Total Page:16

File Type:pdf, Size:1020Kb

Summer 2002 Gems & Gemology G EMS & G VOLUME XXXVIII SUMMER 2002 EMOLOGY S UMMER 2002 P AGES 123–204 Featuring: Characteristics and Grading of Pink Diamonds V OLUME 38 N O. 2 THE QUARTERLY JOURNAL OF THE GEMOLOGICAL INSTITUTE OF AMERICA Summer 2002 VOLUME 38, NO. 2 EDITORIAL 123 Remembering Gemology’s Renaissance Man John Sinkankas (1915–2002) Alice S. Keller 124 LETTERS FEATURE ARTICLES 128 Characterization and Grading of Natural-Color Pink Diamonds Carat Points John M. King, James E. Shigley, Scott S. Guhin, Thomas H. Gelb, and Matthew Hall Based on the largest sample of pink diamonds published to date, this report looks at differences between type I and type II pink diamonds and examines the color description terminology used for pink diamonds on GIA Gem Trade pg. 129 Laboratory grading reports. NOTES AND NEW TECHNIQUES 148 New Chromium- and Vanadium-Bearing Garnets from Tranoroa, Madagascar Karl Schmetzer, Thomas Hainschwang, Heinz-Jürgen Bernhardt, and Lore Kiefert A study of pyrope-spessartine garnets with unusual color behavior from Tranoroa, southern Madagascar. 156 Update on the Identification of Treated “Golden” South Sea Cultured Pearls Shane Elen pg. 157 On the basis of their fluorescence and atypical absorption features, 33 of 35 “golden” South Sea cultured pearls in a strand were identified as color treated. REGULAR FEATURES 161 Gem Trade Lab Notes • Aurichalcite cabochon • Another commercial U.S. facility offers HPHT annealing • Recognizing a color attribute’s effect on color grading fancy-color diamonds • Diamond “pearl” necklace • Internal laser drilling update • Unusual “pink” diamond • High-quality synthetic jadeite from General Electric • Cobalt-”diffused” sapphire • Schlossmacherite beads 170 Gem News International • Conference reports • New round cuts from Antwerp • Benitoite update • Cassiterite from Bolivia • Brazilian emerald with feldspar matrix • Sunstone feldspar from Tanzania • Update on Namibian demantoid garnet • Kyanite from Brazil • South Sea cultured pearls with broken beads • Developments in fresh- water cultured and “keshi” pearls • New sapphire locality in Afghanistan • Elbaite-liddicoatite tourmaline from Vietnam • Green zoisite reappears • Fuchsite imitations of emerald • Unusual synthetic rubies • Identification method for imitation asterism • Irradiated color-change fluorite 187 Thank You, Donors 188 Book Reviews 192 Gemological Abstracts pg. 165 203 Guidelines for Authors Remembering Gemology’s Renaissance Man John Sinkankas (1915–2002) ems & Gemology mourns the passing of associate editor 14,000-item library in 1988, it was the world’s finest private G John Sinkankas, who died in San Diego, California, on collection of gem and mineral literature. Now housed in the May 17 after a brief illness. John had celebrated his 87th Institute’s Richard T. Liddicoat Library and Information birthday just two days before. Center in Carlsbad, California, the Sinkankas collection John Sinkankas was the quintessential “Renaissance Man” includes thousands of rare and important books (see D. of gemology. He was a prolific author, a renowned lapidary, Dirlam et al., “The Sinkankas Library,” Spring 1989 G&G, the undisputed bibliophile in his field, a gem and mineral pp. 2–15). connoisseur, and a successful miner. He was also an accom- In 1982, John was awarded an honorary doctorate from plished artist in watercolor, and several of his paintings of William Paterson University. Two years later, a new peg- gems and minerals appeared in his books. Add to that his matitic phosphate mineral was named sinkankasite in recogni- more than two decades of contributions to G&G, and it is safe tion of his extraordinary contributions to the field. John to say that there will never be another John Sinkankas in received the Carnegie Mineralogical Award in 1988, and was gemology. named an Honorary Lifetime Member of the American Gem A native of Paterson, New Jersey, John began collecting Trade Association (AGTA) in 1992. minerals from the local quarries by the age of seven. After John’s contributions to Gems & Gemology were immeasur- graduating in 1936 from the New Jersey State Teachers able. A member of the editorial review board from 1981 to College (later William Paterson University), John started his 1983, and associate editor since 1984, he not only contributed 25-year career as a Navy pilot. He married his college sweet- numerous articles and book reviews, but he also diligently heart Marjorie Jane McMichael in 1940. John rose to the rank reviewed (and sometimes even rewrote) dozens of of captain before retiring in 1961, whereupon he and Marge manuscripts. settled in San Diego’s Pacific Beach community. This posi- As a friend of John’s for more than 25 years, I treasured his tioned him well for his many forays into the local gem peg- dry wit and unassuming personality. He was generous with matites. his encyclopedic knowledge and had a unique ability to take John’s childhood interest in gems and minerals continued complex concepts, such as crystallography, and put them in throughout his naval career. After World War II, he enrolled terms that a layperson could understand. His influence was in correspondence courses from GIA and the American Gem global, especially in the lapidary arts, where many who never Society (AGS). A self-taught lapidary, John began cutting even met John spoke of him as their mentor. gems in 1947. Today two of his most important gem carv- John Sinkankas is survived by his wife, Marjorie; daugh- ings, a 7,478 ct quartz egg and the world’s largest faceted ters, Sharon J. Tooley of San Diego and Marjorie E. Coates of golden beryl (2,054 ct), are on permanent display at the Virginia; sons, John W. Sinkankas of Los Angeles and Smithsonian Institution in Washington, DC. George M. Sinkankas of Tennessee; nine grandchildren; and Inspired to light the way for others, he began writing an six great-grandchildren. amateur lapidary column for Rocks & Minerals magazine in At the request of the Sinkankas family, GIA has estab- 1951. His first book, Gem Cutting—A Lapidary’s Manual, was lished the John Sinkankas Library Fund. If you would like to published in 1955. More than a dozen books followed, contribute to the fund, please send your donation to: Dona including Emerald and Other Beryls (1981), Gemology: An Dirlam, Liddicoat Gemological Library and Information Annotated Bibliography (1993), and the three-volume series Center, 5345 Armada Drive, Carlsbad, California 92008 Gemstones of North America (1959, 1976, and 1997). ([email protected]). John once described his approach to writing: “It’s really quite a thrill when you find little bits of information that you didn’t know, that you’ve never seen before. And you have a great deal of satisfaction in putting it down in black and white so everybody else can share that information.” As John’s writing projects expanded, so did his and Alice S. Keller, Editor Marge’s private library. At the time GIA purchased their [email protected] EDITORIAL GEMS &GEMOLOGY SUMMER 2002 123 LETTERSLETTERS color emissions (fire) for each of these 16 viewing posi- COMMENTS ON THE GIA tions for a variety of diamond proportions would more ANALYSIS OF DIAMOND “FIRE” closely represent the real-world observation of diamonds. This article from GIA’s study of the impact of proportions on the appearance of a round brilliant cut diamond The GIA Study Is a Huge First Step. This first step (Reinitz et al., Fall 2001, pp. 174–197) is a work of includes the ability to measure and compare the number, admirable dedication, intelligence, and technology and color distributions, and intensity of rays entering and represents a huge commitment of resources. emerging from diamonds of differing proportions. It is unfortunate that this huge effort has two major Although not included in the GIA articles (see also T. S. gaps. First, it confines the study of entering rays to the ver- Hemphill et al., “Modeling the appearance of the round tical, ignoring the vast majority of rays that enter the dia- brilliant cut diamond: An analysis of brilliance,” Fall mond from directions other than the perpendicular, and 1998 Gems & Gemology, pp. 158–183), it seems reason- therefore result in very different emerging light patterns. able and important to combine the diverse brilliance and Second, the “fire” (dispersion) calculations are taken fire measurements into a single “metric.” from the total of emitted rays impacting on a virtual Table 2 of the Fall 2001 article (p. 179), which compares hemisphere that encloses all of the diamond above the “Proportions and Calculated Metric Values for 28 girdle. In the real world, diamonds are viewed from indi- Diamonds” from the study, is the only place where the fire vidual points of view, so that the “fire” of the diamond metric is examined in actual (as opposed to virtual) dia- can be judged only from those points. Thus, the study monds. Note that within this group of 28 diamonds, five of uses only one illumination direction, where in actuality the eight that most closely adhere to both the American diamonds are illuminated from an infinity of positions. Ideal Cut (AGS “0”) and the Tolkowsky cut* show DCLR Conversely, simultaneous viewing from an infinity of (dispersed colored light return, the metric for fire) of over positions over an entire hemisphere could never occur, as 3.75 and a combined WLR (weighted light return, the met- diamonds can be seen from only one location at a time. ric for brilliance) and DCLR of over 4.03. Thus, the two fundamental bases for this study do not Those stones are: reflect what actually happens when diamonds are illumi- nated or viewed. If we were to add three other entering beams of light— No. Crown Pavilion Table WLR DCLR Combined angle angle WLR and DCLR say, at 20°, 40°, and 60° from the vertical—the light emis- sions resulting from these new sources would likely be very different from the purely vertical rays used in the 1 34.3° 40.6° 54% 0.283 3.97 4.25 study.
Recommended publications
  • Mount Apatite Park, Auburn, Maine
    Mount Apatite Park is a 325-acre wooded park located in the western portion of the city. The park offers a wide variety of recreational opportunities not often found in municipal park settings. Rock hounds have known about this area for over 150 years, when the first discoveries of gem-quality tourmaline were found there. Since then, the area has experienced a great deal of mineral exploration, both commercial and amateur. Today amateurs may still search the mine tailings for apatite, tourmaline, and quartz specimens (special rules apply). The park features approximately four miles of trails for non-motorized uses such as hiking, mountain biking, cross-country skiing, and snowshoeing. The Andy Valley Sno Gypsies also maintain a snowmobile trailhead within the park, which links to miles of regional snowmobile trails.The park is open from dawn until dusk year-round. As with all municipal parks, hunting is not allowed within park boundaries. Park brochures, which include a trail map, park rules, and other park information, are available at the Auburn Parks & Recreation Department office, Monday through Friday, 8a.m.-4:30p.m. Mount Apatite Park, Auburn, Maine Significance The Mt. Apatite quarries were important producers of commercial feldspar in the early 1900's. They played a prominent part in Maine's mining history. During the course of this mining activity, rare minerals and colorful crystals of green and pink tourmaline were found in both the Greenlaw and Maine Feldspar Quarries. These quarries also produced many large crystals of transparent smoky quartz. The complexity of the mineral assemblage at Mt.
    [Show full text]
  • Download PDF About Minerals Sorted by Mineral Name
    MINERALS SORTED BY NAME Here is an alphabetical list of minerals discussed on this site. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). APATITE Crystal system: hexagonal. Fracture: conchoidal. Color: red, brown, white. Hardness: 5.0. Luster: opaque or semitransparent. Specific gravity: 3.1. Apatite, also called cellophane, occurs in peridotites in eastern and western Kentucky. A microcrystalline variety of collophane found in northern Woodford County is dark reddish brown, porous, and occurs in phosphatic beds, lenses, and nodules in the Tanglewood Member of the Lexington Limestone. Some fossils in the Tanglewood Member are coated with phosphate. Beds are generally very thin, but occasionally several feet thick. The Woodford County phosphate beds were mined during the early 1900s near Wallace, Ky. BARITE Crystal system: orthorhombic. Cleavage: often in groups of platy or tabular crystals. Color: usually white, but may be light shades of blue, brown, yellow, or red. Hardness: 3.0 to 3.5. Streak: white. Luster: vitreous to pearly. Specific gravity: 4.5. Tenacity: brittle. Uses: in heavy muds in oil-well drilling, to increase brilliance in the glass-making industry, as filler for paper, cosmetics, textiles, linoleum, rubber goods, paints. Barite generally occurs in a white massive variety (often appearing earthy when weathered), although some clear to bluish, bladed barite crystals have been observed in several vein deposits in central Kentucky, and commonly occurs as a solid solution series with celestite where barium and strontium can substitute for each other. Various nodular zones have been observed in Silurian–Devonian rocks in east-central Kentucky.
    [Show full text]
  • 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.
    [Show full text]
  • Bedrock Geology Glossary from the Roadside Geology of Minnesota, Richard W
    Minnesota Bedrock Geology Glossary From the Roadside Geology of Minnesota, Richard W. Ojakangas Sedimentary Rock Types in Minnesota Rocks that formed from the consolidation of loose sediment Conglomerate: A coarse-grained sedimentary rock composed of pebbles, cobbles, or boul- ders set in a fine-grained matrix of silt and sand. Dolostone: A sedimentary rock composed of the mineral dolomite, a calcium magnesium car- bonate. Graywacke: A sedimentary rock made primarily of mud and sand, often deposited by turbidi- ty currents. Iron-formation: A thinly bedded sedimentary rock containing more than 15 percent iron. Limestone: A sedimentary rock composed of calcium carbonate. Mudstone: A sedimentary rock composed of mud. Sandstone: A sedimentary rock made primarily of sand. Shale: A deposit of clay, silt, or mud solidified into more or less a solid rock. Siltstone: A sedimentary rock made primarily of sand. Igneous and Volcanic Rock Types in Minnesota Rocks that solidified from cooling of molten magma Basalt: A black or dark grey volcanic rock that consists mainly of microscopic crystals of pla- gioclase feldspar, pyroxene, and perhaps olivine. Diorite: A plutonic igneous rock intermediate in composition between granite and gabbro. Gabbro: A dark igneous rock consisting mainly of plagioclase and pyroxene in crystals large enough to see with a simple magnifier. Gabbro has the same composition as basalt but contains much larger mineral grains because it cooled at depth over a longer period of time. Granite: An igneous rock composed mostly of orthoclase feldspar and quartz in grains large enough to see without using a magnifier. Most granites also contain mica and amphibole Rhyolite: A felsic (light-colored) volcanic rock, the extrusive equivalent of granite.
    [Show full text]
  • The Anjahamiary Pegmatite, Fort Dauphin Area, Madagascar
    The Anjahamiary pegmatite, Fort Dauphin area, Madagascar Federico Pezzotta* & Marc Jobin** * Museo Civico di Storia Naturale, Corso Venezia 55, I-20121 Milano, Italy. ** SOMEMA, BP 6018, Antananarivo 101, Madagascar. E-mail:<[email protected]> 21 February, 2003 INTRODUCTION Madagascar is among the most important areas in the world for the production, mainly in the past, of tourmaline (elbaite and liddicoatite) gemstones and mineral specimens. A large literature database documents the presence of a number of pegmatites rich in elbaite and liddicoatite. The pegmatites are mainly concentrated in central Madagascar, in a region including, from north to south, the areas of Tsiroanomandidy, Itasy, Antsirabe-Betafo, Ambositra, Ambatofinandrahana, Mandosonoro, Ikalamavony, Fenoarivo and Fianarantsoa (e.g. Pezzotta, 2001). In general, outside this large area, elbaite-liddicoatite-bearing pegmatites are rare and only minor discoveries have been made in the past. Nevertheless, some recent work made by the Malagasy company SOMEMEA, discovered a great potential for elbaite-liddicoatite gemstones and mineral specimens in a large, unusual pegmatite (the Anjahamiary pegmatite), hosted in high- metamorphic terrains. The Anjahamiary pegmatite lies in the Fort Dauphin (Tôlanaro) area, close to the southern coast of Madagascar. This paper reports a general description of this locality, and some preliminary results of the analytical studies of the accessory minerals collected at the mine. Among the most important analytical results is the presence of gemmy blue liddicoatite crystals with a very high Ca content, indicating the presence in this tourmaline crystal of composition near the liddicoatite end-member. LOCATION AND ACCESS The Anjahamiary pegmatite is located about 70 km NW of the town of Fort Dauphin (Tôlanaro) (Fig.
    [Show full text]
  • Geology and Selected Minerals of the Diamond Hill Quartz Mine Antreville, South Carolina by Mike Streeter, GMS Member Copyright March 2004
    Tips and Trips Page 11 The Georgia Mineral Society May 2004 Geology and Selected Minerals of the Diamond Hill Quartz Mine Antreville, South Carolina by Mike Streeter, GMS Member Copyright March 2004 Chrissy and I have spent a great deal of time at the Diamond Diamond Hill is nothing short of remarkable when you consider Hill Quartz Mine near Antreville, South Carolina over the past that the actual collecting areas occupy a total of less than 3 several months. Chester Karwoski, who purchased the acres and that each variety requires its own unique set of property in 2003, brought in some heavy earth-moving conditions to form. The three most sought after varieties of equipment last fall and has opened up some new collecting quartz at the mine are skeletal, smoky and amethyst. opportunities. On our most recent trip to the mine on February 28, 2004, members of the Rome Georgia Gem and Mineral Skeletal quartz (also known Society and the Southern Appalachian Mineral Society joined as elestial quartz) exhibits a us. Since it is no secret that that I am a geologist by trade, I layered or ribbed pattern. am often asked geological and mineralogical questions about Its appearance gave rise to collecting locales. While digging at Diamond Hill, I was asked the term "skeletal" as the to explain how the rocks and crystals formed. Now there's a crystals resemble what $64,000 question for you! I answered the question as best I someone with a good could at the time. Since then, I have researched the literature imagination would expect to obtain a more detailed explanation that I would like to share the skeleton of a quartz with you.
    [Show full text]
  • March 2019 Agate Explorer.Pub
    Cuyuna Rock, Gem and Mineral Society The Agate Explorer March 2019 Summer Field Trip Plans are being made for a long weekend trip to Thunder Bay to collect amethyst. The tentative dates are Friday -Sunday, July 5 -7. A sign -up sheet will be available at upcoming meeting in order to plan this trip. It is necessary to have a passport to travel to Canada. You may also check to see if an enhanced driver’s license is acceptable. March meeting Open Shop from 9 a.m. —noon Franklin Art Center Club member, Ray Strassberg, will be available for members to learn how Club Information to cut rocks using the 10” or 16” inch saws. Website -www.cuyunarockclub.org - Email [email protected] Bring rocks of your own or purchase something in the Rock Room. Meeting Place Lower level Franklin Arts Center Kids’ Program 1001 Kingwood St, Brainerd, MN 56401 Did you know that there are many Directions .4 mile east of Business Hwy. 371 different kinds of Lake Superior & Hwy. 210 intersection. agates? Lisa will tell you all about it (Castle turret water tower.) at the March meeting! Date/Time the 2nd Saturday of each month Rock Wrappers at 2 p.m. unless otherwise noted. Meets starting at 10 a.m. on meeting Saturdays. Club Dues $20/ family ,An open gathering for wire wrappers. Hang out with other wrappers, Free /unaccompanied juniors and work on your projects. (Bring all supplies needed.) Membership runs Learn tricks to make wrapping easier, a new design, from Jan. 1-Dec. 31st. or perhaps a new place to find supplies.
    [Show full text]
  • Crystal Guide for Business Success
    MARIAHEALS.COM DECEMBER 2016 C R Y S T A L G U I D E for B U S I N E S S S U C C E S S W E A L T H | H E A L T H | P R O S P E R I T Y Crystal Guide for Business Success Welcome To your Crystal Guide for Business Success for you, as a Heart Centered Entrepreneurs. You will find that it is a little different to the normal guide as the focus is on the feminine paradigm, creating lasting relationships and collaboration. As well as creating abundance, meaning the flow of energy (including money). These are my top 7 crystals to create your business success, as a Heart Centered Entrepreneur. These crystals when used in girds, meditation, ritual and ceremony will support you to activate your success. I have been using crystals for years now and when I realised that they could be used to heal, create and manifest health and wealth,things started to change in my life and the life of my clients. Now I share this knowledge with you. Many Blessings Maria ­2­ Crystal Guide for Business Success Index Citrine Quartz (Clear) Opalite Rose Quartz Pyrite Tiger's Eye Green Aventurine ­3­ Crystal Guide for Business Success Set the intention The intention with these crystals is to create success on your terms, energetically, with a solid foundation, supporting you to create your financial independence. Set your intention everytime you use one or all of these crystals. How to Use these crytals? Citrine, Quartz, Rose Quartz and Tiger Eye ­ these are wonderful combination to pop in a grid or meditate with.
    [Show full text]
  • Lts Ficez 5Coz7'a1ra
    ltS FicEz 5coZ7'a1ra he most valuable gem- Gem-quality red beryl on quality red beryl comes white devitri- from thc Wah Wah fied rhyolite Mountains of south- matrix. This western Utah (Fig. 1). sample mea- Red beryl occurs as a secondary sures 9 x 26 mm (O.35 x 1 mineral in topaz rhyolite. Market- in.l. (Photo by able crystals from the Wah Wah Sky Hall.) Mountains have been produced from the Violet Mine, operated on a limited scale since 1976 under the ownership of the Harris family of Delta, UT. From 1989 to 1995. oroduction from the mine amounted to more than $3 million with an inventory of several million dollars of unsold gems (Harris, 1995). In 7994, Kennecott Exploration leased the mine and surrounding claims to de- termine reserves and feasibility of gem recovery. Mining and explora- E.H. Christiansen and tion activity are continuing. J.D. Keith are proles- Previous work on red beryl has s0rs arld T.J. dealt mainly with crystallographic, Thompson is a student, chemical and optical properties of the crystals (Shigley and Foord, Ieparlment of Geohgy, 1984) with only general descriptions Brigham Yrung Univer- of the geology (Ream, 1979). How- sitt Brx 251 I l, Prlvn, ever. the conditions needed for for- mation of red beryl have not been UT 84fi[2 well constrained. It is generally pro- posed that beryl originates by pre- cipitation in fractures and vugs from high-temperature silica rhyolite and andesitic lava flows. gases as they are released from slowly cooled rhyolite Beginning about 23 Ma, the style and composition of lava.
    [Show full text]
  • Analytical Methods to Differentiate Romanian Amber and Baltic Amber for Archaeological Applications
    Cent. Eur. J. Chem. • 7(3) • 2009 • 560-568 DOI: 10.2478/s11532-009-0053-8 Central European Journal of Chemistry Analytical methods to differentiate Romanian amber and Baltic amber for archaeological applications Research Article Eugenia D. Teodor1*, Simona C. Liţescu1, Antonela Neacşu2, Georgiana Truică1 Camelia Albu1 1 National Institute for Biological Sciences, Centre of Bioanalysis, Bucharest, 060031, Romania 2 University of Bucharest, Faculty of Geology and Geophysics, Bucharest, 010041, Romania Received 27 August 2008; Accepted 02 March 2009 Abstract: The study aims to establish several definite criteria which will differentiate Romanian amber and Baltic amber to certify the local or Baltic origin of the materials found in archaeological sites on the Romanian territory, by using light microscopy and performing analytical methods, such as Fourier transform infrared spectroscopy-variable angle reflectance and liquid chromatography with mass spectrometry detection. Experiments especially by Fourier transformed infrared spectroscopy, were applied to a wide range of samples with controlled origin. The methods were optimised and resulted in premises to apply the techniques to analysis of the archaeological material. Keywords: Romanian amber • FTIR-VAR • LC-MS • Light microscopy © Versita Warsaw and Springer-Verlag Berlin Heidelberg. 1. Introduction (Oligocene). The resin-bearing strata are intercalated within the lower and medium part of the lower Kliwa Amber is a fossil resin originating from different types sandstone (0.20-1.40 m). They consist of siliceous clay of Conifers and certain flowering trees, especially in hot (0.20-1.40 m) always containing thin intercalations of climates. From the mineralogical point of view amber bituminous shales (2-5 cm) and of preanthracite coal could be considered a mineraloid.
    [Show full text]
  • 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 ....................................
    [Show full text]
  • Exceptional Works of Art 2017 PUSHKIN ANTIQUES – MAYFAIR –
    Exceptional works of art 2017 PUSHKIN ANTIQUES – MAYFAIR – At Pushkin Antiques we specialise in unique statement Each item is professionally selected and inspected pieces of antique silver as well as branded luxury items, to ensure we can give our customers a guarantee of stylish interior articles and objects d’art. authenticity and the required peace of mind when buying from us. Since the inception of our company, we’ve been at the forefront of online sales for high end, quality antiques. Our retail gallery is located on the lower floor of the world Our presence on most major platforms has allowed us famous Grays Antiques Centre in the heart of Mayfair. to consistently connect exquisite pieces with the most discerning collectors and interior decorators from all over the world with particular focus on the demands of the markets from the Far East, the Americas, Europe & Russia. www.pushkinantiques.com [email protected] We aim to provide the highest quality in every department: rare hand crafted articles, accurate item descriptions (+44) 02085 544 300 to include the history and provenance of each item, an (+44) 07595 595 079 extensive photography report, as well as a smooth buying process thus facilitating an efficient and pleasant online Shop 111, Lower Ground Floor, Grays Antiques Market. experience. 58 Davies St, London. W1K 5AB, UK. ALEX PUSHKIN OLGA PUSHKINA DUMITRU TIRA Founder & Director Managing Director Photographer Contents 6 ENGLISH SILVER 42 CHINESE SILVER 56 JAPANESE SILVER 66 INDIAN SILVER 78 BURMESE SILVER 86 CONTINENTAL SILVER 100 FRENCH SILVER 108 GERMAN SILVER 118 RUSSIAN SILVER 132 OBJECTS OF VERTU English Silver The style and technique in manufacturing silver during Hester Bateman (1708-1794) was one of the greatest this era (over 100 years) changed radically, reflecting silversmiths operating in this style, she is the most the variations in taste, society, costumes, economic and renowned and appreciated female silversmith of all time.
    [Show full text]