Fall 1985 Gems & Gemology
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Magnetic Susceptibility Index for Gemstones ©2010 Kirk Feral Magnetic Responses Are Standardized to 1/2" X 1/2" N-52 Magnet Cylinders
Magnetic Susceptibility Index for Gemstones ©2010 Kirk Feral Magnetic responses are standardized to 1/2" X 1/2" N-52 magnet cylinders. Colorless and extremely pale stones of any species tend to be Inert (diamagnetic). Black opaque stones of many species are strongly magnetic and may Pick Up or Drag. Pick Up and Drag responses are weight-dependent. Direct responses on the Index apply to gems 1-4cts. Larger gems may be too heavy to Pick Up or Drag. Smaller non-Garnet gems with strong magnetism may Pick Up. Gemstone Response Range SI X 10 (-6) Range Cause of Color Actinolite Nephrite Jade (black) Strong to Drags 321-577 SI Iron Nephrite Jade (green) Moderate to Drags 91-343 Iron, Chromium Nephrite Jade (white, yellow) Inert < 0 (diamagnetic) Iron Pargasite (green) Inert < 0 (diamagnetic) Iron, Vanadium Pargasite (orangey brown) Weak 35 SI Iron Afghanite (blue) Inert < 0 (diamagnetic) Chromium, Vanadium Amber (any color) Inert < 0 (diamagnetic) Charge Transfer involving Organic Compounds Amblygonite-Montebrasite (blue, green) Inert < 0 (diamagnetic) Iron, Manganese Andalusite Inert to Weak < 0 -26 Iron-Oxygen-Titanium Charge Transfer Apatite Transparent blue, green, yellow Inert (Weak in rare cases) < 0 (diamagnetic) Mang., Rare-earth, Charge Transfer, Color Centers Cat's eye translucent yellow, yellowish brown Weak to Strong < 20 - >120 Rare-earth Metals Astrophyllite Strong 1146-1328 Iron, Manganese Axinite Drags 603-616 SI Iron Azurite (opaque) Strong 382 SI Copper Barite (pale brown, blue) Inert < 0 (diamagnetic) Color Centers Bastnasite -
Phase Equilibria and Thermodynamic Properties of Minerals in the Beo
American Mineralogist, Volwne 71, pages 277-300, 1986 Phaseequilibria and thermodynamic properties of mineralsin the BeO-AlrO3-SiO2-H2O(BASH) system,with petrologicapplications Mlnx D. B.qnroN Department of Earth and SpaceSciences, University of California, Los Angeles,Los Angeles,California 90024 Ansrru,cr The phase relations and thermodynamic properties of behoite (Be(OH)r), bertrandite (BeoSirOr(OH)J, beryl (BerAlrSiuO,r),bromellite (BeO), chrysoberyl (BeAl,Oo), euclase (BeAlSiOo(OH)),and phenakite (BerSiOo)have been quantitatively evaluatedfrom a com- bination of new phase-equilibrium, solubility, calorimetric, and volumetric measurements and with data from the literature. The resulting thermodynamic model is consistentwith natural low-variance assemblagesand can be used to interpret many beryllium-mineral occurTences. Reversedhigh-pressure solid-media experimentslocated the positions of four reactions: BerAlrSiuO,,: BeAlrOo * BerSiOo+ 5SiO, (dry) 20BeAlSiOo(OH): 3BerAlrsi6or8+ TBeAlrOo+ 2BerSiOn+ l0HrO 4BeAlSiOo(OH)+ 2SiOr: BerAlrSiuO,,+ BeAlrOo+ 2H2O BerAlrSiuO,,+ 2AlrSiOs : 3BeAlrOa + 8SiO, (water saturated). Aqueous silica concentrationswere determined by reversedexperiments at I kbar for the following sevenreactions: 2BeO + H4SiO4: BerSiOo+ 2H2O 4BeO + 2HoSiOo: BeoSirO'(OH),+ 3HrO BeAlrOo* BerSiOo+ 5H4Sio4: Be3AlrSiuOr8+ loHro 3BeAlrOo+ 8H4SiO4: BerAlrSiuOrs+ 2AlrSiO5+ l6HrO 3BerSiOo+ 2AlrSiO5+ 7H4SiO4: 2BerAlrSiuOr8+ l4H2o aBeAlsioloH) + Bersio4 + 7H4sio4:2BerAlrsiuors + 14Hro 2BeAlrOo+ BerSiOo+ 3H4SiOo: 4BeAlSiOr(OH)+ 4HrO. -
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. -
An Exploration of Jade Maria Jones
Eastern Michigan University DigitalCommons@EMU Senior Honors Theses Honors College 2004 An Exploration of Jade Maria Jones Follow this and additional works at: http://commons.emich.edu/honors Recommended Citation Jones, Maria, "An Exploration of Jade" (2004). Senior Honors Theses. 85. http://commons.emich.edu/honors/85 This Open Access Senior Honors Thesis is brought to you for free and open access by the Honors College at DigitalCommons@EMU. It has been accepted for inclusion in Senior Honors Theses by an authorized administrator of DigitalCommons@EMU. For more information, please contact lib- [email protected]. An Exploration of Jade Abstract Abstract: This is a research paper studying the history of Jade carving during the Chinese Han Dynasty from 206 B.C to 220 A.D. The ap per explains the meaning of jade to the Chinese people and examines the origin of the precious stone for the Han people and other generations of dynasties. There is an accurate telling of Han beliefs followed by a descriptive passage on the history of religious influence on the Han people. There is an extensive study on the history of the Han people in general and a lengthy report on the different forms of jade and their functions for the Han people. Degree Type Open Access Senior Honors Thesis Department Art First Advisor Dr. Richard Rubenfeld Second Advisor Leslie Atzmon Keywords Jade art objects, Art objects, Chinese, Jade This open access senior honors thesis is available at DigitalCommons@EMU: http://commons.emich.edu/honors/85 AN EXPLORATION OFJ/\DL: by :'vlariaJones A St~nior ThcsIs Submitted to the !:astern tv1ichigan Umversny 1ionors Program In Partial Fulfillment of the Requiremems for Graduation With Honors in Fine Art: CcHJCcntratinnin Graphic Design 1 I I ! ~--'~""'-"""'- ,,=.. -
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. -
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. -
Symposium on Agate and Cryptocrystalline Quartz
Symposium on Agate and Cryptocrystalline Quartz September 10 – 13, 2005 Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter; Colorado School of Mines Geology Museum; and U.S. Geological Survey 2 Cover Photos {top left} Fortification agate, Hinsdale County, Colorado, collection of the Geology Museum, Colorado School of Mines. Coloration of alternating concentric bands is due to infiltration of Fe with groundwater into the porous chalcedony layers, leaving the impermeable chalcedony bands uncolored (white): ground water was introduced via the symmetric fractures, evidenced by darker brown hues along the orthogonal lines. Specimen about 4 inches across; photo Dan Kile. {lower left} Photomicrograph showing, in crossed-polarized light, a rhyolite thunder egg shell (lower left) a fibrous phase of silica, opal-CTLS (appearing as a layer of tan fibers bordering the rhyolite cavity wall), and spherulitic and radiating fibrous forms of chalcedony. Field of view approximately 4.8 mm high; photo Dan Kile. {center right} Photomicrograph of the same field of view, but with a 1 λ (first-order red) waveplate inserted to illustrate the length-fast nature of the chalcedony (yellow-orange) and the length-slow character of the opal CTLS (blue). Field of view about 4.8 mm high; photo Dan Kile. Copyright of articles and photographs is retained by authors and Friends of Mineralogy, Colorado Chapter; reproduction by electronic or other means without permission is prohibited 3 Symposium on Agate and Cryptocrystalline Quartz Program and Abstracts September 10 – 13, 2005 Editors Daniel Kile Thomas Michalski Peter Modreski Held at Green Center, Colorado School of Mines Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter Colorado School of Mines Geology Museum U.S. -
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 .................................... -
Post Mortem Analysis of a JET Quartz Microbalance System “This Document Is Intended for Publication in the Open Literature
EFDA-JET-CP(06)02-10 H.G. Esser, V. Philipps, P. Wienhold, K. Sugiyama, A. Kreter, P. Coad, T. Tanabe and JET EFDA contributors Post Mortem Analysis of a JET Quartz Microbalance System “This document is intended for publication in the open literature. It is made available on the understanding that it may not be further circulated and extracts or references may not be published prior to publication of the original when applicable, or without the consent of the Publications Officer, EFDA, Culham Science Centre, Abingdon, Oxon, OX14 3DB, UK.” “Enquiries about Copyright and reproduction should be addressed to the Publications Officer, EFDA, Culham Science Centre, Abingdon, Oxon, OX14 3DB, UK.” Post Mortem Analysis of a JET Quartz Microbalance System H.G. Esser1, V. Philipps1, P. Wienhold1, K. Sugiyama3, A. Kreter1, P. Coad2, T. Tanabe3 and JET EFDA contributors* 1Institut für Plasmaphysik, Forschungszentrum Jülich GmbH, EURATOM Association, Trilateral Euregio Cluster, D-52425 Jülich, Germany 2EURATOM/UKAEA Fusion Association, Culham Science Centre, Abingdon, OX14 3DB, UK 4Department of Nuclear Engineering, Graduate School of Engineering, Nagoya University, Furo-cho, Chikusa-ku, Nagoya 464-8603, Japan * See annex of J. Pamela et al, “Overview of JET Results”, (Proc.20th IAEA Fusion Energy Conference, Vilamoura, Portugal (2004). Preprint of Paper to be submitted for publication in Proceedings of the 17th Plasma Surface Interactions in Fusion Devices, (Hefei Anhui, China, 22nd May - 26th May 2006) . ABSTRACT. In the year 2001 a Quartz Microbalance System (QMB) was installed in the remote area of the inner JET divertor to measure in-situ erosion and redeposition processes. -
Pyrophyllite Solid Solutions in the System A|,O,-S|O,-H,O
American Minerulogist, Volume 59, pages 254-260, 1974 PyrophylliteSolid Solutions in the SystemA|,O,-S|O,-H,O Pnrr,rp E. RoseNnenc D ep art ment ol G eolo gy, 14as hing ton Stat e U nio er sity, P ullman, 14as hington 99 I 6 3 Abstract Pyrophyllite solid solutions have been synthesized in the system Al,O'-SiOr-H,O between 400' and 565'C at 2 kbar from a variety of starting materials using sealed gold tubes and conventional hydrothermal techniques. The duration of experiments was 3-9 weeks. Products were characterized by X-ray measurementsand by infrared spectroscopy. Appreciably larger basal spacings were observed for pyrophyllite synthesized from gels than for natural pyrophyllite; small amounts of quartz were present in these samples. Basal spacings of pyrophyllite synthesized from mixtures of kaolinite and quartz approach but do not equal those of natural pyrophyllite. Rehydroxylation of dehydroxylated pyrophyllite under hydrothermal conditions suggests that enlargement of basal spacings cannot be due to dehydroxylation. Substitution of the type Al"* + H* : Sia* is proposed to explain the observed variations. The coupled substitution of Al3* and (OH)- for Sin*and O- results in expanded basal spacingsdue largely to the formation of OH on the basal surface and in increased thermal stability due to the formation of H-bonds between oxygens in adjacent silica sheets.Analyses of natural pyrophyllite also suggest limited substitution of this type. Failure to recognize these substitutions in synthetic samples accounts, in part, for dis- crepancies in the reported thermal stability of pyrophyllite. Phase characterization, often lack- ing, is essentialin experimentalstudies of mineral stabilities. -
Ancient Jades Map 3,000 Years of Prehistoric Exchange in Southeast Asia
Ancient jades map 3,000 years of prehistoric exchange in Southeast Asia Hsiao-Chun Hunga,b, Yoshiyuki Iizukac, Peter Bellwoodd, Kim Dung Nguyene,Be´ re´ nice Bellinaf, Praon Silapanthg, Eusebio Dizonh, Rey Santiagoh, Ipoi Datani, and Jonathan H. Mantonj Departments of aArchaeology and Natural History and jInformation Engineering, Australian National University, Canberra ACT 0200, Australia; cInstitute of Earth Sciences, Academia Sinica, P.O. Box 1-55, Nankang, Taipei 11529, Taiwan; dSchool of Archaeology and Anthropology, Australian National University, Canberra ACT 0200, Australia; eDepartment of Ancient Technology Research, Vietnam Institute of Archaeology, Hanoi, Vietnam; fCentre National de la Recherche Scientifique, Unite´Mixte de Recherche 7528, 27 Rue Paul Bert, 94204 Ivry-sur-Seine, France; gDepartment of Archaeology, Silpakorn University, Bangkok 10200, Thailand; hArchaeology Division, National Museum of the Philippines, Manila, Philippines; and iSarawak Museum, Kuching, Malaysia Edited by Robert D. Drennan, University of Pittsburgh, Pittsburgh, PA, and approved October 5, 2007 (received for review August 3, 2007) We have used electron probe microanalysis to examine Southeast Japanese archaeologist Kano Tadao (7) recognized four types of Asian nephrite (jade) artifacts, many archeologically excavated, jade earrings with circumferential projections that he believed dating from 3000 B.C. through the first millennium A.D. The originated in northern Vietnam, spreading from there to the research has revealed the existence of one of the most extensive Philippines and Taiwan. Beyer (8), Fox (3), and Francis (9) also sea-based trade networks of a single geological material in the suggested that the jade artifacts found in the Philippines were of prehistoric world. Green nephrite from a source in eastern Taiwan mainland Asian origin, possibly from Vietnam. -
Read Jet Blue Master Card Login Rar for Android
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