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Coesite Inclusions: Microbarometers in Diamond
Coesite Inclusions: Microbarometers in Diamond Ren Lu GIA Laboratory, New York Mineral inclusions in diamond provide valuable information for decoding their thermobarometric, mechanical, and mineralogical conditions during and after diamond formation deep within the earth’s mantle. Coesite, a polymorph of silica (SiO2), shares the same chemical composition as quartz but has a different crystal structure and a higher Mohs hardness Anthony et al., 1990). Coesite forms at pressures greater than 2 GPa (i.e., 20,000 times atmospheric pressure). It has been found in high-impact meteorite craters and as inclusions in minerals and diamonds in ecologites in ultrahigh-pressure metamorphic terrains (Sobolev et al., 1999). Mineral inclusions in diamonds record the physical and chemical history of diamond formation; consequently, they provide a window to processes occurring in the deep interior of the mantle. Microscopic Raman spectroscopy is a very effective “fingerprint” technique for identifying unknown materials such as inclusions in gems, because Raman spectral features closely correlate to the crystal structure and chemistry of a material. Furthermore, this technique is nondestructive and requires virtually no sample preparation. We recently examined a suite of high-quality pink diamonds set in a bracelet. These stones were type Ia and exhibited gemological and spectral characteristics typical of the rarest group of high-quality Argyle pink diamonds (refer to table 2 in Shigley et al., 2001). A cluster of mineral inclusions were present in a 0.21 ct marquise in the intense to vivid purple-pink color range (figure 1). Raman spectra were collected with a Renishaw inVia confocal Raman system interfaced with 488, 514, 633, and 830 nm laser excitations. -
Jahrbuch Der Kais. Kn. Geologischen Reichs-Anstalt
Digitised by the Harvard University, Download from The BHL http://www.biodiversitylibrary.org/; www.biologiezentrum.at Die Meteoritensammlung des k. k. mineralogischen Hof kabinetes in Wien am I. Mai 1885. Von Dr. Aristides Breziua. Mit vier Tafe'.n (Nr. 11— V). Von dieser Saminluug, welche schon zu Chladm's Zeiten von hohem wissenschaftlichen Werthe war und seither inamer eine erste Stelle einnahm, ist seit dem Jahre 1872 keine vollständige Gewichts- liste veröffentlicht worden ; in dem genannten Jahre gab der damalige Director des Kabinetes, Hofrath G. Tschermak, ein Verzeichnisse), das er bei seinem Abgange vom Museum durch einen Nachtrag ^) bis Ende September 1877 vervollständigte. Als mir nach dem Ausscheiden Tschermak's von meinem seither verstorbenen Vorstande, Hofrath Ritter v. Hochstetter, die Obsorge über die Sammlung übertragen wurde, war es mein nächstes Ziel, die Fälle aus den letzten Jahr- zehnten zu vervollständigen und die vielen nur durch kleine Splitter von einem Gramm und darunter vertretenen Localitäten durch grössere Stücke zu repräsentiren, weil so kleine Fragmente die petrographische Beschaffenheit eines gemengten Körpers nicht genügend erkennen lassen. Es zeigte sich bald, dass ein solches Ziel nur durch Anlegung einer eigenen Meteoritentauschsammlung zu erreichen war, welche bei Gele- genheit grösserer Fälle oder Funde mit Doublettenmateriale zu billigen Preisen versehen werden konnte und dann die Erwerbung auch der selteneren und kostbareren Fallorte auf dem Tauschwege gestattete; denn die Meteoritenpreise sind gegen frühere Jahrzehnte so wesentlich gestiegen, dass eine Ergänzung der Sammlung durch vorwiegenden Ankauf nicht mehr möglich ist, während andererseits eine Abgabe an- sehnlicher Stücke aus der Hauptsammlung, wie sie unter Hoernes- Haidinger üblich war, eine gewisse Beweglichkeit der Sammlung hervorbringt, welche bei einem so kostbaren Materiale wohl vermieden werden soll ; auch ein Tausch mit kleinen, von den Hauptstücken abge- kueipten Splittern, wie er ebenfalls häufig stattfand, bringt nur einen ') Die Meteoriten des k, k. -
Hong Kong SAR
China Data Supplement November 2006 J People’s Republic of China J Hong Kong SAR J Macau SAR J Taiwan ISSN 0943-7533 China aktuell Data Supplement – PRC, Hong Kong SAR, Macau SAR, Taiwan 1 Contents The Main National Leadership of the PRC 2 LIU Jen-Kai The Main Provincial Leadership of the PRC 30 LIU Jen-Kai Data on Changes in PRC Main Leadership 37 LIU Jen-Kai PRC Agreements with Foreign Countries 47 LIU Jen-Kai PRC Laws and Regulations 50 LIU Jen-Kai Hong Kong SAR 54 Political, Social and Economic Data LIU Jen-Kai Macau SAR 61 Political, Social and Economic Data LIU Jen-Kai Taiwan 65 Political, Social and Economic Data LIU Jen-Kai ISSN 0943-7533 All information given here is derived from generally accessible sources. Publisher/Distributor: GIGA Institute of Asian Affairs Rothenbaumchaussee 32 20148 Hamburg Germany Phone: +49 (0 40) 42 88 74-0 Fax: +49 (040) 4107945 2 November 2006 The Main National Leadership of the PRC LIU Jen-Kai Abbreviations and Explanatory Notes CCP CC Chinese Communist Party Central Committee CCa Central Committee, alternate member CCm Central Committee, member CCSm Central Committee Secretariat, member PBa Politburo, alternate member PBm Politburo, member Cdr. Commander Chp. Chairperson CPPCC Chinese People’s Political Consultative Conference CYL Communist Youth League Dep. P.C. Deputy Political Commissar Dir. Director exec. executive f female Gen.Man. General Manager Gen.Sec. General Secretary Hon.Chp. Honorary Chairperson H.V.-Chp. Honorary Vice-Chairperson MPC Municipal People’s Congress NPC National People’s Congress PCC Political Consultative Conference PLA People’s Liberation Army Pol.Com. -
Terrestrial Impact Structures Provide the Only Ground Truth Against Which Computational and Experimental Results Can Be Com Pared
Ann. Rev. Earth Planet. Sci. 1987. 15:245-70 Copyright([;; /987 by Annual Reviews Inc. All rights reserved TERRESTRIAL IMI!ACT STRUCTURES ··- Richard A. F. Grieve Geophysics Division, Geological Survey of Canada, Ottawa, Ontario KIA OY3, Canada INTRODUCTION Impact structures are the dominant landform on planets that have retained portions of their earliest crust. The present surface of the Earth, however, has comparatively few recognized impact structures. This is due to its relative youthfulness and the dynamic nature of the terrestrial geosphere, both of which serve to obscure and remove the impact record. Although not generally viewed as an important terrestrial (as opposed to planetary) geologic process, the role of impact in Earth evolution is now receiving mounting consideration. For example, large-scale impact events may hav~~ been responsible for such phenomena as the formation of the Earth's moon and certain mass extinctions in the biologic record. The importance of the terrestrial impact record is greater than the relatively small number of known structures would indicate. Impact is a highly transient, high-energy event. It is inherently difficult to study through experimentation because of the problem of scale. In addition, sophisticated finite-element code calculations of impact cratering are gen erally limited to relatively early-time phenomena as a result of high com putational costs. Terrestrial impact structures provide the only ground truth against which computational and experimental results can be com pared. These structures provide information on aspects of the third dimen sion, the pre- and postimpact distribution of target lithologies, and the nature of the lithologic and mineralogic changes produced by the passage of a shock wave. -
Mineral Processing
Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19 -
With Julia Woodman
TESSELATIONTHE THREE-DIMENSIONAL FORM OCTOBER WORKSHOP METALSOCIETY OF SOUTHERN ARTS CALIFORNIA Sept Oct 2013 with Julia Woodman October 19th & 20th, 2013 Saddleback Community College in Mission Viejo $195 for MASSC members / $220 for non members Learn a new skill using metalsmithing tools, bolts and an industrial punch. That’s all that’s needed to form small silver discs, squares, jump rings, etc., into 3-D shapes suitable for bracelets, earrings or spoon handles. Students are shown how to experiment with these and more to create beautifully textured miniature sculpture to adorn or for décor. Some soldering, sawing and filing skills are needed to learn this fun, new technique – TESSELLATION. So bring your imagination and an Optivisor and let’s PLAY!! www.juliawoodman.com NEWSLETTER OCTOBER WORKSHOP TESSELATIONTHE THREE-DIMENSIONAL FORM “My work using 3D tessellation for serving utensils shows clean simple lines Julia Woodman has lived in Lahti, Finland where she studied with third and with ornate texture, almost a by-product of the technique itself.” fourth generation Fabergé masters while on a Fulbright Grant and was certified Master Silversmith in Finland, the first American. She has a MFA degree from Woodman uses tessellation to construct handles for serving pieces, arms and Georgia State University and has studied with Heikki Seppä and other masters upright portions of crosses for churches, and stems and bases for cups, trophies at the Penland School of Craft during many summer sessions. Also, she teaches and other vessels. Utility and function are major components of her work: the at the Spruill Center for the Arts in Atlanta, Chastain Arts Center and substitute teapots must work and fish slices must serve fish. -
Spatiotemporal Patterns of Population Mobility and Its Determinants in Chinese Cities Based on Travel Big Data
sustainability Article Spatiotemporal Patterns of Population Mobility and Its Determinants in Chinese Cities Based on Travel Big Data Zhen Yang 1,2 , Weijun Gao 1,2,* , Xueyuan Zhao 1,2, Chibiao Hao 3 and Xudong Xie 3 1 Innovation Institute for Sustainable Maritime Architecture Research and Technology, Qingdao University of Technology, Qingdao 266033, China; [email protected] (Z.Y.); [email protected] (X.Z.) 2 Faculty of Environmental Engineering, The University of Kitakyushu, Kitakyushu 808-0135, Japan 3 College of Architecture and Urban Planning, Qingdao University of Technology, Qingdao 266033, China; [email protected] (C.H.); [email protected] (X.X.) * Correspondence: [email protected]; Tel.: +81-93-695-3234 Received: 16 April 2020; Accepted: 13 May 2020; Published: 14 May 2020 Abstract: Large-scale population mobility has an important impact on the spatial layout of China’s urban systems. Compared with traditional census data, mobile-phone-based travel big data can describe the mobility patterns of a population in a timely, dynamic, complete, and accurate manner. With the travel big dataset supported by Tencent’s location big data, combined with social network analysis (SNA) and a semiparametric geographically weighted regression (SGWR) model, this paper first analyzed the spatiotemporal patterns and characteristics of mobile-data-based population mobility (MBPM), and then revealed the socioeconomic factors related to population mobility during the Spring Festival of 2019, which is the most important festival in China, equivalent to Thanksgiving Day in United States. During this period, the volume of population mobility exceeded 200 million, which became the largest time node of short-term population mobility in the world. -
Relict Zircon Inclusions in Muong Nong-Type Australasain Tektites: Implications Regarding the Location of the Source Crater
Lunar and Planetary Science XXXI 1196.pdf RELICT ZIRCON INCLUSIONS IN MUONG NONG-TYPE AUSTRALASAIN TEKTITES: IMPLICATIONS REGARDING THE LOCATION OF THE SOURCE CRATER. B. P. Glass, Geology Department, University of Delaware, Newark, DE 19716, USA ([email protected]) Introduction: Over the last thirty years we Australasian tektite samples from which we have have recovered crystalline inclusions from ap- identified inclusions; however, not all of the recov- proximately forty Muong Nong-type tektites from ered inclusions have been identified by XRD. the Australasian tektite strewn field in order to Based on appearance, the percent of inclusion- learn more about the nature of the parent material bearing specimens containing zircon is probably and the formation process [e.g., 1, 2]. More re- 100% or very close to it. Nearly all the zircons cently we have used geographic variations in con- are opaque white and their X-ray patterns show centration (number/gm) of crystalline inclusions to extreme X-ray asterism. However, of the 28 zir- indicate the possible location of the source crater cons identified by X-ray diffraction, only two [3]. The purpose of this abstract is to summarize (both from the same specimen whose place of ori- all the presently available data regarding relict gin is unknown) produced X-ray diffraction pat- zircon inclusions recovered from Australasian terns indicating that baddeleyite may be present. Muong Nong-type tektites and to discuss implica- The X-ray patterns from these two grains con- tions regarding the possible location of the source tained the two strongest lines for baddeleyite and crater which has still not been found. -
Stishovite and Seifertite in Lunar Meteorite Northwest Africa 4734
71st Annual Meteoritical Society Meeting (2008) 5058.pdf FIRST EVIDENCE OF HIGH PRESSURE SILICA: STISHOVITE AND SEIFERTITE IN LUNAR METEORITE NORTHWEST AFRICA 4734. H. Chennaoui Aoudjehane1-2, A. Jambon2 1Université Hassan II Aïn Chock, Laboratoire Géosciences, BP 5366 Maârif Casa- blanca Morocco (e-mail: [email protected]), 2Université Pierre et Marie Curie-Paris6 and IPGP Laboratoire MAGIE, Case 110, 4 place Jussieu, 75252 Paris France. Introduction: Silica is a rare phase in lunar rocks; it has been described as either quartz, cristobalite and/or tridymite [1]. Northwest Africa 4734, is an uncommon type of lunar rock, which may be launched paired with the LaPaz Icefield Lunar Mare basalts found in 2002-03 in Antarctica [2-6], it is a coarse grained rock of basaltic composition, exhibits a number of sig- nificant shock features, such as PDFs, extensive fracturation of pyroxene, impact melt pockets and transformation of plagioclase to maskelynite; silica is present as a minor phase. Analytical procedures: We studied the speciation of silica polymorphs to characterize the shock, using SEM imaging, Ra- man spectroscopy, CL imaging and spectroscopy. Further details can be found in [7]. Results: According to the CL spectra [7-9], cristobalite, tridymite, high-pressure silica glass, stishovite and seifertite, are all present. Special emphasis is made on stishovite and seifertite, which, like in shergottites, exhibit specific textural features [7]. Cathodoluminescence spectra characteristic of high-pressure sil- ica phases: glass, stishovite and seifertite have been recorded in addition to the original low-pressure phases. The remanence of cristobalite and tridymite underscores a significant heterogeneity of the shock supported by the rock. -
PRESS RELEASE the Goldsmiths' Company Becomes a Founding
PRESS RELEASE The Goldsmiths’ Company becomes a Founding Partner of the new Museum of London and pledges £10m donation Queen Elizabeth II Coronation Cup, designed by Goldsmith R.Y. Goodden in 1953 is pictured in the Corporation of London’s current salt store, which by 2022 will have been transformed into galleries at the new Museum of London in West Smithfield with the Thameslink track running through them. Image © Museum of London. Collection: The Worshipful Company of Goldsmiths. The Museum of London and the Worshipful Company of Goldsmiths (one of the major City Livery Companies) today announced that the Goldsmiths' Company is to become a Founding Partner of the new Museum of London, due to open in West Smithfield in 2022. The Goldsmiths' Company and its affiliated Charity have pledged £10 million to the Museum project. This landmark donation goes towards the Museum’s plans to create a spectacular new home for the history of London and its people in the beautiful but disused market buildings at West Smithfield. This follows the news earlier this year that the City of London Corporation and Mayor of London have together pledged £180 million. Counting the donation from the Goldsmiths’ Company and its affiliated Charity, the Museum has £60 million left to raise. A gallery bearing the Goldsmiths’ name will be at the heart of the new Museum, showcasing the Cheapside Hoard together with highlights from the Company’s world-renowned Collection of historic and contemporary silver. Judith Cobham-Lowe, Prime Warden of the Goldsmiths' Company, said: "We are thrilled to be playing our part in the new Museum of London as a Founding Partner. -
Nickel Minerals from Barberton, South Africa: I
American Mineralogist, Volume 58, pages 733-735, 1973 NickelMinerals from Barberton,South Africa: Vl. Liebenbergite,A NickelOlivine SvsneNoA. nn Wnar Nationnl Institute lor Metallurgy, I Yale Road.,Milner Park, I ohannesburg,South Alrica Lnwrs C. ClI.x Il. S. GeologicalSuruey, 345 Middlefield Road, Menlo Park, California 94025 Abstract Liebenbergite, a nickel olivine from the mineral assemblage trevorite-liebenbergite-nickel serpentine-nickel ludwigite-bunsenite-violarite-millerite-gaspeite-nimite, is described mineral- ogically.Ithasa-1.820,P-1.854,7-1.888,ZVa-88",specificgravity-4'60,Mohs hardness- 6 to 6.5, a - 4.727, b - 10.191,c = 5.955A, and Z - 4. X-ray powder data (48 lines) were indexed according to the space grottp Pbnm. The mean chemical composi- tion, calculated from electron microprobe analyses of eight separate liebenbergite grains, gives the mineral formula: (NL eMgoaCoo,sFeo o)Sio "nOn The name is for W. R. Liebenberg, Deputy Director-General of the National Institute for Metallurgy, South Africa. Introduction mission on New Minerals and Mineral Names (rMA). A re-investigationof the trevorite deposit at Bon Accord in the Barberton Mountain Land, South Experimental Methods Africa, led to the discovery of two peculiar but distinct nickel mineral assemblages.Minerals from The refractive indices were determined by the the assemblagewillemseite-nimite-feroan trevorite- conventional liquid immersion method using a reevesite-millerite-violarite-goethitehave been de- sodium lamp as light source.The optical and crystal scribed in earlier papers in this series (de Waal, morphologicalparameters were studiedwith the aid 1969, l97oa, 1970b;de Waal and Viljoen, I97L). of a universal stage. -
Geochemical Characterization of Moldavites from a New Locality, the Cheb Basin, Czech Republic
Geochemical characterization of moldavites from a new locality, the Cheb Basin, Czech Republic Item Type Article; text Authors Řanda, Zdeněk; Mizera, Jiři; Frána, Jaroslav; Kučera, Jan Citation Řanda, Z., Mizera, J., Frána, J. and Kučera, J. (2008), Geochemical characterization of moldavites from a new locality, the Cheb Basin, Czech Republic. Meteoritics & Planetary Science, 43(3), 461-477. DOI 10.1111/j.1945-5100.2008.tb00666.x Publisher The Meteoritical Society Journal Meteoritics & Planetary Science Rights Copyright © The Meteoritical Society Download date 30/09/2021 11:07:40 Item License http://rightsstatements.org/vocab/InC/1.0/ Version Final published version Link to Item http://hdl.handle.net/10150/656405 Meteoritics & Planetary Science 43, Nr 3, 461–477 (2008) AUTHOR’S PROOF Abstract available online at http://meteoritics.org Geochemical characterization of moldavites from a new locality, the Cheb Basin, Czech Republic ZdenÏk ÿANDA1, Ji¯í MIZERA1, 2*, Jaroslav FRÁNA1, and Jan KU»ERA1 1Nuclear Physics Institute, Academy of Sciences of the Czech Republic, 250 68 ÿež, Czech Republic 2Institute of Rock Structure and Mechanics, Academy of Sciences of the Czech Republic, V HolešoviËkách 41, 182 09 Praha 8, Czech Republic *Corresponding author. E-mail: [email protected] (Received 02 June 2006; revision accepted 15 July 2007) Abstract–Twenty-three moldavites from a new locality, the Cheb Basin in Western Bohemia, were analyzed by instrumental neutron activation analysis for 45 major and trace elements. Detailed comparison of the Cheb Basin moldavites with moldavites from other substrewn fields in both major and trace element composition shows that the Cheb Basin is a separate substrewn field.