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Total Lot Value = $8,189.80 LOT #128 Location Id Lot # Item Id Sku Image Store Price Model Store Quantity Classification Total Value
Total Lot Value = $8,189.80 LOT #128 location_id Lot # item_id sku Image store_price model store_quantity classification Total Value A07-S05-D001 128 182363 TICB-1001 $13.95 16G 5/16" Internally Threaded Implant Grade Titanium Curved Barbell 8 Curved Barbell $111.60 A07-S05-D003 128 186942 NR-1316 $8.95 Purple 2mm Bezel-Set Synthetic Opal Rose Gold-Tone Steel Nose Ring Twist 1 Nose Ring $8.95 A07-S05-D005 128 65492 A208 $11.99 Celtic Swirl Reverse Belly Button Ring 4 Belly Ring Sale $47.96 A07-S05-D006 128 104247 PLG-1345-14 $10.95 9/16" Pink Heart-Shaped Cut Out Flexible Silicone Tunnel Plugs Pair 4 Plugs $43.80 A07-S05-D007 128 65494 D103 $5.95 16G 3/8 - Anodized Rainbow Titanium-Plated Captive Bead Ring 3 Captive Ring , Daith $17.85 A07-S05-D008 128 65496 D103b $5.95 Rainbow Titanium-Plated Captive Bead Ring - 14G 1/2 1 Captive Ring $5.95 A07-S05-D010 128 65499 D103d $4.99 16G 5/8 - Rainbow Anodized Steel Captive Bead Ring 51 Captive Ring $254.49 A07-S05-D011 128 87697 BR-1429 $11.99 Pink CZ Crown & Flower Dangle Belly Button Navel Ring 2 Belly Ring Sale $23.98 A07-S05-D012 128 64066 BR-1496 $11.99 Purple CZ Crown & Flower Dangle Belly Button Navel Ring 4 Belly Ring Sale $47.96 A07-S05-D013 128 65502 D111 $5.99 Spiky -Ball Twister - Body Jewelry 14 Gauge 43 Twister Barbell Sale $257.57 A07-S05-D014 128 104271 PLG-1345-16 $10.95 5/8" - Pink Heart-Shaped Cut Out Flexible Silicone Tunnel Plugs - Pair 2 Plugs $21.90 A07-S05-D015 128 104185 PLG-1345-4 $8.95 6G - Pink Heart-Shaped Cut Out Flexible Silicone Tunnel Plugs - Pair 2 Plugs $17.90 -
HIGHLIGHTS and BREAKTHROUGHS Sapphire, A
1 HIGHLIGHTS AND BREAKTHROUGHS 2 Sapphire, a not so simple gemstone 3 F. LIN SUTHERLAND1* 4 1Geoscience, Australian Museum, 1 William Street, Sydney, NSW 2010, Australia. 5 *E-mail: [email protected] 6 Abstract: Sapphire is a gemstone of considerable reach and is much researched. It still delivers scientific surprises, as exemplified by a 7 recent paper in American Mineralogist that re-interprets the origin of needle-like rutile inclusions that form “silk” in sapphires. 8 Understanding of variations in sapphire genesis continues to expand. Keywords: Sapphire, inclusions, trace elements, genesis 9 Sapphire as a gem variety of corundum has wide use in the gem trade as one of the more historically valuable colored gem stones 10 (CGS) and is mined from a great variety of continental gem deposits across the world. A masterly compendium on this gemstone and its 11 ramifications is recently available (Hughes 2017). As a gem, sapphire ranges through all the colors of corundum, except where 12 sufficient Cr enters its α-alumina crystal structure and causes the red color of the variety ruby. Sapphire, as a key pillar in a wide 13 economic network of gem enhancing treatments, jewelry and other manufacturing enterprises, has elicited numerous scientific and 14 gemological enquiries into its internal nature and natural genesis and subsequent treatments. A further use of sapphire as a synthetic 15 material with a great variety of purposes also has triggered a proliferation of detailed studies on its growth, properties and other element 16 substitutional effects (Dobrovinski et al. 2009). Even with this vast range of studies, this apparently simple gemstone still yields 17 controversies and breakthroughs in understanding its genetic formation. -
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 .................................... -
Do Zircon and Monazite Consistently Record Garnet Growth in High-Grade Rocks?
Geophysical Research Abstracts Vol. 21, EGU2019-5915-1, 2019 EGU General Assembly 2019 © Author(s) 2019. CC Attribution 4.0 license. Do zircon and monazite consistently record garnet growth in high-grade rocks? Lorraine Tual (1,2), Ellen Kooijman (1), Melanie Schmitt (1), and Matthijs Smit (2) (1) Department of Geosciences, Swedish Museum of Natural History, Stockholm, Sweden ([email protected]), (2) Department of Earth, Ocean, and Atmospheric Sciences, University of British Columbia, Vancouver, Canada Garnet Lu-Hf ages are used to monitor the systematics of rare earth elements (REE) and age record in accessory minerals. We performed in-situ LA-(MC-)ICPMS U-(Th-)Pb dating and REE analysis on zircon and monazite in two contrasting high-grade rock samples: dry felsic granulite xenoliths from the Pamir, Tajikistan and fluid-rich, ultrahigh-pressure (UHP) migmatites from the Western Gneiss Region (WGR), Norway. In parallel, garnet from the same samples were subjected to REE analysis and dated by Lu-Hf. The datasets are compared to see whether, and to what extent, REE systematics in accessory phases can be correlated with garnet growth. Garnet in the hydrous UHP migmatite contains abundant zircon and monazite inclusions. The Gd/Yb values and U-(Th-)Pb ages of these inclusions show significant dispersion and do not systematically correlate. Highest Gd/Yb values occur at 420-410 and c. 420 Ma for monazite and zircon, respectively. Garnet in this rock yielded a Lu-Hf garnet bulk age of c. 422 Ma. The data obtained from the dry Pamir xenoliths show a different pattern. Accessory minerals grew in distinct pulses between 50 and 11 Ma, and indicate garnet growth between 42-37 Ma [1]. -
Distinctive Designs
Distinctive Designs Brides Ring in an Era of Self-Expression by Stacey Marcus Diamond rings have been sporting the hands of newly can elevate a traditional setting to an entirely new level. While engaged women since ancient times. In the mid 1940s, diamonds are always in vogue for engagement rings, millen- DeBeers revived the ritual with its famous “Diamonds Are nials are also opting for nontraditional stones, such as color- Forever” campaign. Today’s brides are blazing new trails by changing alexandrite, beautiful tanzanite, black opal, and even selecting nontraditional wedding rings that express their aquamarine. We are in an age when anything goes, and brides individual style. are embracing the idea of individuality and self-expression!” True Colors says Jordan Fine, CEO of JFINE. “Brides today want to be unique and they don’t mind taking Kathryn Money, vice president of strategy and merchandising chances with colors, settings, and stones. When it comes to at Brilliant Earth agrees: “Customers are seeking products that choosing an engagement ring, natural pink, blue, and even express their individuality and are increasingly drawn towards green diamonds are trending. These precious and rare dia- uniqueness. They want a ring that isn’t like everyone else’s, monds originate from only a few mines in the world, and they which we’re seeing manifested in many different ways, such 34 Spring 2018 BRIDE&GROOM as choosing a distinctive ring setting, using colored gemstones in lieu of a diamond, using a fancy (non-round) diamond, or opting for rose gold.” Money adds that 16% of respondents in a recent survey they conducted favored a colored gemstone engagement ring over a diamond. -
MAGAZINE • LEAWOOD, KS SPECIAL EDITION 2016 ISSUE 3 Fine Jewelers Magazine
A TUFTS COMMUNICATIONS fine jewelry PUBLICATION MAZZARESE MAGAZINE • LEAWOOD, KS SPECIAL EDITION 2016 ISSUE 3 fine jewelers magazine Chopard: Racing Special The New Ferrari 488 GTB The Natural Flair of John Hardy Black Beauties Omega’s New 007 SPECIAL EDITION 2016 • ISSUE 3 MAZZARESE FINE JEWELERS MAGAZINE • SPECIAL EDITION 2016 welcome It is our belief that we have an indelible link with the past and a responsibility to the future. In representing the fourth generation of master jewelers and craftsmen, and even as the keepers of a second generation family business, we believe that the responsibility to continually evolve and develop lies with us. We endeavor to always stay ahead of the latest jewelry and watch trends and innovations. We stay true to our high standards and objectives set forth by those that came before us by delivering a jewelry experience like no other; through the utmost attention to service, knowledge and value. Every great story begins with a spark of inspiration. We are reminded day after day of our spark of inspiration: you, our esteemed customer. Your stories help drive our passion to pursue the finest quality pieces. It is a privilege that we are trusted to provide the perfect gift; one that stands the test of time and is passed along through generations. We find great joy in assisting the eager couple searching for the perfect engagement ring, as they embark on a lifetime of love, helping to select a quality timepiece, or sourcing a rare jewel to mark and celebrate a milestone. We are dedicated to creating an experience that nurtures relationships and allows those who visit our store to enter as customers, but leave as members of our family. -
Radiohalos and Diamonds: Are Diamonds Really for Ever?
The Proceedings of the International Conference on Creationism Volume 6 Print Reference: Pages 323-334 Article 28 2008 Radiohalos and Diamonds: Are Diamonds Really for Ever? Mark H. Armitage Andrew A. Snelling Answers in Genesis Follow this and additional works at: https://digitalcommons.cedarville.edu/icc_proceedings DigitalCommons@Cedarville provides a publication platform for fully open access journals, which means that all articles are available on the Internet to all users immediately upon publication. However, the opinions and sentiments expressed by the authors of articles published in our journals do not necessarily indicate the endorsement or reflect the views of DigitalCommons@Cedarville, the Centennial Library, or Cedarville University and its employees. The authors are solely responsible for the content of their work. Please address questions to [email protected]. Browse the contents of this volume of The Proceedings of the International Conference on Creationism. Recommended Citation Armitage, Mark H. and Snelling, Andrew A. (2008) "Radiohalos and Diamonds: Are Diamonds Really for Ever?," The Proceedings of the International Conference on Creationism: Vol. 6 , Article 28. Available at: https://digitalcommons.cedarville.edu/icc_proceedings/vol6/iss1/28 In A. A. Snelling (Ed.) (2008). Proceedings of the Sixth International Conference on Creationism (pp. 323–334). Pittsburgh, PA: Creation Science Fellowship and Dallas, TX: Institute for Creation Research. Radiohalos and Diamonds: Are Diamonds Really for Ever? Mark H. Armitage, M.S. Ed.S., Microspecialist, 587 Ventu Park Road 304, Thousand Oaks, CA 91320 Andrew A. Snelling, Ph.D., Director of Research, Answers in Genesis, P.O. Box 510, Hebron, KY 41048 Abstract Radiohalos were first reported in diamonds more than a decade ago. -
Gem Wealth of Tanzania GEMS & GEMOLOGY Summer 1992 Fipe 1
By Dona M.Dirlarn, Elise B. Misiorowski, Rosemaiy Tozer, Karen B. Stark, and Allen M.Bassett The East African nation of Tanzania has he United Republic of Tanzania, the largest of the East great gem wealth. First known by Western- 1African countries, is composed of mainland Tanzania and ers for its diamonds, Tanzania emerged in the island of Zanzibar. 1t is regarded by many as the birthplace the 1960s as a producer of a great variety of of the earliest ancestors of Homo sapiens. To the gem indus- other gems such as tanzanite, ruby, fancy- try, however, Tanzania is one of the most promising fron- colored sapphire, garnet, and tourmaline; to date, more than 50 gem species and vari- tiers, with 50 gem species and varieties identified, to date, eties have been produced. As the 1990s from more than 200 occurrences. begin, De Beers has reinstated diamond "Modem" mining started in the gold fields of Tanzania in exploration in Tanzania, new gem materials the late 1890s (Ngunangwa, 19821, but modem diamond min- such as transparent green zoisite have ing did not start until 1925, and nearly all mining of colored appeared on the market, and there is stones has taken place since 1950. Even so, only a few of the increasing interest in Tanzania's lesser- gem materials identified have been exploited to any significant known gems such as scapolite, spinel, and extent: diamond, ruby, sapphire, purplish blue zoisite (tan- zircon. This overview describes the main zanite; figure l),and green grossular [tsavorite)and other gar- gems and gem resources of Tanzania, and nets. -
Guaranteed Shops Ocho Rios
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Olivine – Peridot 橄欖石 Prof
Olivine – Peridot 橄欖石 Prof. Dr H.A. Hänni, FGA, SSEF Research Associate Email: [email protected] Fig. 1 Peridots rough and cut, from various locations. Photo © H.A.Hänni 作者述了寶石級橄欖石的特性，它歸屬於橄欖石 類礦物，它有三種成因，化學成的改變而引致顏 色、折射率和比重的變異，並簡報其內含物、人工 合成方法和產地，以及作為首飾時應注意的地方。 Peridot is a widely appreciated green gemstone (Fig. 1). It belongs to the Olivine group, which also includes the major minerals forsterite Mg2SiO4, fayalite Fe2SiO4 and tephroite Mn2SiO4. Olivines are the main constituents of maic and ultramaic rocks that are formed in the earth’s mantle. Olivine-basalt rocks bring the crystals to the surface, where they are found e.g. in extended basalt layers such as in China (Hebei province) (Fig. 2), and the Fig. 3 A Pallasite, an iron-nickel matrix with olivine crystals. Photo © H.A.Hänni USA (Arizona). Another genetic type of olivines is found in rocks formed by metamorphism like in Myanmar or Pakistan. Olivines are also the main constituents of rare pallasites, nickel-iron meteorites, with large inclusions of olivine (Fig. 3). Synthetic forsterites with dopants are used for laser technology applications. Gemstone olivine is called peridot, and also chrysolite. It is represented by a solid mixture between the Mg member forsterite (fo) and the Fe member fayalite (fa), with high fo and low fa concentrations. Occasional Fig. 2 An olivine-basalt rock sample with olivine grain contributions of Mn, Ni or Cr are always very small, but clusters and a larger olivine crystal from Zhangjikou- inluence the colour of the stone. Forsterite and fayalite Xuanhua, Hebei Province, China. are a solid solution series just as pyrope and almandine Photo © H.A.Hänni garnets. -
The Geochronology and Geochemistry of Zircon As Evidence for the Reconcentration of REE in the Triassic Period in the Chungju Area, South Korea
minerals Article The Geochronology and Geochemistry of Zircon as Evidence for the Reconcentration of REE in the Triassic Period in the Chungju Area, South Korea Sang-Gun No 1,* and Maeng-Eon Park 2 1 Mineral Resources Development Research Center, Korea Institute of Geoscience and Mineral Resources, Daejeon 34132, Korea 2 Department of Earth Environmental Science, Pukyong National University, Busan 48513, Korea; [email protected] * Correspondence: [email protected]; Tel.: +82-10-9348-7807 Received: 1 November 2019; Accepted: 2 January 2020; Published: 5 January 2020 Abstract: The Chungju rare-earth element (REE) deposit is located in the central part of the Okcheon Metamorphic Belt (OMB) in the Southern Korean Peninsula and research on REE mineralization in the Gyemyeongsan Formation has been continuous since the first report in 1989. The genesis of the REE mineralization that occurred in the Gyemyeongsan Formation has been reported by previous researchers; theories include the fractional crystallization of alkali magma, magmatic hydrothermal alteration, and recurrent mineralization during metamorphism. In the Gyemyeongsan Formation, we discovered an allanite-rich vein that displays the paragenetic relationship of quartz, allanite, and zircon, and we investigated the chemistry and chronology of zircon obtained from this vein. We analyzed the zircon’s chemistry with an electron probe X-ray micro analyzer (EPMA) and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS). The grain size of the zircon is as large as 50 µm and has an inherited core (up to 15 µm) and micrometer-sized sector zoning (up to several micrometers in size). In a previous study, the zircon ages were not obtained because the grain size was too small to analyze. -
Weight of Production of Emeralds, Rubies, Sapphires, and Tanzanite from 1995 Through 2005
Weight of Production of Emeralds, Rubies, Sapphires, and Tanzanite from 1995 Through 2005 By Thomas R. Yager, W. David Menzie, and Donald W. Olson Open-File Report 2008–1013 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2008 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Yager, T.R., Menzie, W.D., and Olson, D. W., 2008, Weight of production of emeralds, rubies, sapphires, and tanzanite from 1995 through 2005: U.S. Geological Survey Open-File Report 2008-1013, 9 p., available only online, http://pubs.usgs.gov/of/2008/1013. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. ii Contents Introduction ...................................................................................................................................1 Emeralds.......................................................................................................................................2