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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. -
Acadia Geology Alumni/Ae Newsletter
Acadia Geology Alumni/ae Newsletter Issue 21 December, 2009 Department of Earth and Environmental Science, Acadia University, Wolfville, Nova Scotia, B4P 2R6 [email protected] VIEW FROM ACADIA As I write this message, my term as the “acting head” course, it costs less to deliver. Another aspect of of Earth and Environmental Science is rapidly budgetary constraints is a lack of replacements for drawing to a close. Rob Raeside returns as head faculty on sabbatical. In the “good old days” such beginning Jan. 1, 2010, and it is probably a “toss-up” absences were typically covered by a full-time faculty as to which one of us is happier about that! To be replacement, but now we are lucky to receive one honest, however, I found many aspects of being “per-course replacement”. Such replacements have department head to be rewarding, and if we did not been great but they are paid specifically to teach the have a capable and willing incumbent returning to the single course assigned to them, and hence do not job, continuing in the role would have been OK. provide any coverage for other activities integral to running a department, such as counselling students, The past year at Acadia has more than lived up to the supervising honours and special project students, supposed ancient Chinese curse “may you live in serving on committees, and so on. This ripple-down interesting times”. The main topic occupying effect hits especially hard in a small department such everyone’s mind on campus has been the university as ours. Fortunately, faculty in E&ES have been budget. -
FREEVIEW DTT Multiplexes (UK Inc NI) Incorporating Planned Local TV and Temporary HD Muxes
As at 07 December 2020 FREEVIEW DTT Multiplexes (UK inc NI) incorporating planned Local TV and Temporary HD muxes 3PSB: Available from all transmitters (*primary and relay) 3 COM: From *80 primary transmitters only Temp HD - 25 Transmiters BBC A (PSB1) BBC A (PSB1) continued BBC B (PSB3) HD SDN (COM4) ARQIVA A (COM5) ARQIVA B (COM6) ARQIVA C (COM7) HD ARQIVA D (COM8) HD LCN LCN LCN LCN LCN LCN LCN 1 BBC ONE 65 TBN UK 12 QUEST 11 Sky Arts 22 Ideal World 64 Free Sports BBC RADIO: 1 BBC ONE NI Cambridge, Lincolnshire, 74 Shopping Quarter 13 E4 (Wales only) 17 Really 23 Dave ja vu 70 Quest Red+1 722 Merseyside, Oxford, 1 BBC ONE Scot Solent, Somerset, Surrey, 101 BBC 1 Scot HD 16 QVC 19 Dave 26 Yesterday 83 NOW XMAS Tyne Tees, WM 1 BBC ONE Wales 101 BBC 1 Wales HD 20 Drama 30 4Music 33 Sony Movies 86 More4+1 2 BBC TWO 101 BBC ONE HD 21 5 USA 35 Pick 36 QVC Beauty 88 TogetherTV+1 (00:00-21:00) 2 BBC TWO NI BBC RADIO: 101 BBC ONE NI HD 27 ITVBe 39 Quest Red 37 QVC Style 93 PBS America+1 726 BBC Solent Dorset 2 BBC TWO Wales BBC Stoke 102 BBC 2 Wales HD 28 ITV2 +1 42 Food Network 38 DMAX 96 Forces TV 7 BBC ALBA (Scot only) 102 BBC TWO HD 31 5 STAR 44 Gems TV 40 CBS Justice 106 BBC FOUR HD 9 BBC FOUR 102 BBC TWO NI HD 32 Paramount Network 46 Film4+1 43 HGTV 107 BBC NEWS HD Sony Movies Action 9 BBC SCOTLAND (Scot only) BBC RADIO: 103 ITV HD 41 47 Challenge 67 CBS Drama 111 QVC HD (exc Wales) 734 Essex, Northampton, CLOSED 24 BBC FOUR (Scot only) Sheffield, 103 ITV Wales HD 45 Channel 5+1 48 4Seven 71 Jewellery Maker 112 QVC Beauty HD 201 CBBC -
Australian Aborigines and Meteorites
Records of the Western Australian Museum 18: 93-101 (1996). Australian Aborigines and meteorites A.W.R. Bevan! and P. Bindon2 1Department of Earth and Planetary Sciences, 2 Department of Anthropology, Western Australian Museum, Francis Street, Perth, Western Australia 6000 Abstract - Numerous mythological references to meteoritic events by Aboriginal people in Australia contrast with the scant physical evidence of their interaction with meteoritic materials. Possible reasons for this are the unsuitability of some meteorites for tool making and the apparent inability of early Aborigines to work metallic materials. However, there is a strong possibility that Aborigines witnessed one or more of the several recent « 5000 yrs BP) meteorite impact events in Australia. Evidence for Aboriginal use of meteorites and the recognition of meteoritic events is critically evaluated. INTRODUCTION Australia, although for climatic and physiographic The ceremonial and practical significance of reasons they are rarely found in tropical Australia. Australian tektites (australites) in Aboriginal life is The history of the recovery of meteorites in extensively documented (Baker 1957 and Australia has been reviewed by Bevan (1992). references therein; Edwards 1966). However, Within the continent there are two significant areas despite abundant evidence throughout the world for the recovery of meteorites: the Nullarbor that many other ancient civilizations recognised, Region, and the area around the Menindee Lakes utilized and even revered meteorites (particularly of western New South Wales. These accumulations meteoritic iron) (e.g., see Buchwald 1975 and have resulted from prolonged aridity that has references therein), there is very little physical or allowed the preservation of meteorites for documentary evidence of Aboriginal acknowledge thousands of years after their fall, and the large ment or use of meteoritic materials. -
Vaibhav Gems Cover Options
FORWARD LOOKING STATEMENT All statements that address expectations or projections about the future, product development, market position, expenditures and financial results, are forward looking statements. Forward-looking statements are based on certain assumptions and expectations of future conditions. The Company cannot guarantee the accuracy of these assumptions and expectations. Therefore, actual performance may differ from the projected performance as there are certain factors affecting the Company’s performance such as international market conditions, Government policies and laws, changes in the economic conditions affecting demand and supply etc. The Company does not take any responsibility to change/modify any forward-looking statement on the basis of any subsequent developments or events. Annual Report 2009-10 Board of Directors Vaibhav Gems Limited Sunil Agrawal - Chairman Rahimullah - Managing Director Nirmal Kumar Bardiya - Director Anandi Lal Roongta - Director Mitha Lal Mehta - Director Surendra Singh Bhandari - Director Sheela Agrawal - Director Company Secretary Mukesh Khetan Statutory Auditors Haribhakti & Co., Mumbai B. Khosla & Co., Jaipur Registrar & Share Transfer Agents Karvy Computershare (P) Limited 17-24, Vittal Rao Nagar, Madhapur Hyderabad-500 081 Bankers Punjab National Bank State Bank of Bikaner & Jaipur Union Bank of India IDBI Bank Registered Office K-6B, Fateh Tiba, Adarsh Nagar, Jaipur-302004 Tel: 91-141-2601020; Fax: 91-141-2603228/2010 Corporate Office E-68, EPIP, Sitapura, Jaipur-302022 Tel: 91-141-2770648; Fax: 91-141-2770510 1 Vaibhav Gems Limited Our Vision To be the most preferred global jewellery company for all stakeholders worldwide Our Mission Mission B14X Our Core Values I will serve my customers with passion. I will keep my word. -
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. -
Compilation of Minimum and Maximum Isotope Ratios of Selected Elements in Naturally Occurring Terrestrial Materials and Reagents by T
U.S. Department of the Interior U.S. Geological Survey Compilation of Minimum and Maximum Isotope Ratios of Selected Elements in Naturally Occurring Terrestrial Materials and Reagents by T. B. Coplen', J. A. Hopple', J. K. Bohlke', H. S. Reiser', S. E. Rieder', H. R. o *< A R 1 fi Krouse , K. J. R. Rosman , T. Ding , R. D. Vocke, Jr., K. M. Revesz, A. Lamberty, P. Taylor, and P. De Bievre6 'U.S. Geological Survey, 431 National Center, Reston, Virginia 20192, USA 2The University of Calgary, Calgary, Alberta T2N 1N4, Canada 3Curtin University of Technology, Perth, Western Australia, 6001, Australia Institute of Mineral Deposits, Chinese Academy of Geological Sciences, Beijing, 100037, China National Institute of Standards and Technology, 100 Bureau Drive, Stop 8391, Gaithersburg, Maryland 20899 "institute for Reference Materials and Measurements, Commission of the European Communities Joint Research Centre, B-2440 Geel, Belgium Water-Resources Investigations Report 01-4222 Reston, Virginia 2002 U.S. Department of the Interior GALE A. NORTON, Secretary U.S. Geological Survey Charles G. Groat, Director The use of trade, brand, or product names in this report is for identification purposes only and does not imply endorsement by the U.S. Government. For additional information contact: Chief, Isotope Fractionation Project U.S. Geological Survey Mail Stop 431 - National Center Reston, Virginia 20192 Copies of this report can be purchased from: U.S. Geological Survey Branch of Information Services Box 25286 Denver, CO 80225-0286 CONTENTS Abstract...................................................... -
Abstract: Investigation of the Form and Age of the Bloody Creek Crater
Atlantic Geology . Volume 48 . 2012 40 Investigation of the form and age of the Bloody Creek Crater, southwestern Nova Scotia Mariella Nalepa1, Ian Spooner1, and Peter Williams2 1. Department of Earth and Environmental Science, Acadia Uni- versity, Wolfville, Nova Scotia B4P 2R6, Canada <[email protected]> ¶ 2. Department of Physics, Acadia Uni- versity, Wolfville, Nova Scotia B4P 2R6, Canada Virtually all terrestrial impact craters exhibit a circular geometry in plan-form; only three impact sites exhibiting non-circular, elongate forms have been identified on Earth. One of these exceptional sites is the Bloody Creek Crater located in southwestern Nova Scotia, an approximately 0.42 km long-axis elliptical crater first identified in 1987 during a regional air photo survey. It was confirmed as an impact crater in 2009 through integrated geomorphic, geophysical, and petrographic data. The structure’s rare ellipticity, pristine definition, preservation through shock metamorphic features of anomalously high pressures at the rim, low depth-to-diameter ratio, as well as age remain ambiguous and complicate the interpretation of the origin and evolution of the crater. The purpose of this study is to quantify the form of the feature in order to better understand the nature and age of impact. To achieve this objective, analytical software was used to assess the shape of the crater rim. An extensive review of the literature was also performed to understand the controls on crater formation as well as to synthesize a model for the geological evolution of the site which would aid in the interpretation of the age of the structure. Results demonstrate that the form of the crater rim is best approximated by an ellipse, as illustrated by comparison of the RMSE (Root-Mean-Square Error) calculated for various geometric models. -
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Determination of the Origin of Unusual Glass with Metallic Spherule
Per. Mineral. (2006), 75, 2-3, 11-24 http://go.to/permin An International Journal of O PERIODICO di MINERALOGIA MINERALOGY, CRYSTALLOGRAPHY, GEOCHEMISTRY, established in 1930 ORE DEPOSITS, PETROLOGY, VOLCANOLOGY and applied topics on Environment, Archaeometry and Cultural Heritage Determination of the origin of unusual glass with metallic spherule inclusions found in the area between Inzingkofen and Sigmaringen (Bavaria, Germany), South-West of the Steinheim-Ries craters Matteo Ardit,1 Anna Maria Fioretti,2* Gianmario Molin,3 Emilio Ramous4 and Ulf-Christian Bauer5 1 Centro di Ateneo per i Musei, via Orto Botanico, 15 – 35122 Padova (Italy) 2 Istituto Geoscienze e Georisorse - CNR, c.so Garibaldi, 37 – 35137 Padova (Italy) 3 Dipartimento di Mineralogia e Petrologia, Università di Padova, c.so Garibaldi, 37 – 35137 Padova (Italy) 4 Dipartimento di Innovazione Meccanica e Gestionale, Università di Padova, via Venezia, 1 – 35139 Padova (Italy) 5 Seestrasse, 46a – 83727 Schliarsee (Germany) Abstract. — This paper reports the characteristics Riassunto. — In questo lavoro vengono studiati of a suite of pale green glass fragments and their diversi frammenti di vetro verde chiaro aventi metallic spherule inclusions (5 to 400 μm) found la particolarità di contenere inclusioni di sferule over a relatively wide area between Inzigkofen and metalliche (di dimensioni variabili tra 5 e 400 Sigmaringen (Bavaria, Germany), about 150 km SW μm), ritrovati in un’area relativamente vasta tra of the Steinheim-Ries impact craters. The distribution Inzigkofen e Sigmaringen (Baviera, Germania), a area of these glasses and their close macroscopic ~150 km SW dai crateri di impatto di Steinheim- similarity (apart from the spherules) with moldavite Ries. -
Shock Wave Distribution at Ries Impact Crater, Germany?:A Micro-Raman Spectroscopical Study of Shocked Zircon
Workshop on Impact Cratering II (2007) 8050.pdf “ANTISYMMETRIC” SHOCK WAVE DISTRIBUTION AT RIES IMPACT CRATER, GERMANY?:A MICRO-RAMAN SPECTROSCOPICAL STUDY OF SHOCKED ZIRCON. A. Gucsik, Max Planck Institute for Chemistry, Department of Geochemistry,. Joh.-J.-Becherweg 27, D-55128 Mainz, Germany (gucsik@mpch- mainz.mpg.de). Introduction: Zircon is a highly refractory and weather- parallel and perpendicular to the c-axis, for the pur- ing-resistant mineral that has proven useful as an indi- pose of Raman spectrometric analysis. cator of shock metamorphism in the study of impact Raman spectra were obtained with a Renishaw structures and formations that are old, deeply eroded, RM1000 confocal micro-Raman spectrometer with a and metamorphically overprinted (e.g., [1-3]. Zircon 20 mW, 632 nm He-Ne laser excitation system and a has advantages compared to quartz or other shock- thermo-electrically cooled CCD detector. The power metamorphosed rock-forming minerals that have been of the laser beam on the sample was approximately 3 widely used as impact indicators, but are far less re- mW. Spectra were obtained in the range 100-1200 cm- fractory. Furthermore, U-Pb dating of zircon can pro- 1, with approximately thirty seconds total exposure vide constraints on the ages of impact events or depo- time. The spectral resolution (apparatus function) was sition of impact formations (e.g., [4] and references 4 cm-1. Raman spectra were taken from 3 µm3 sample therein). volume and CL spectra were obtained from approxi- Effects of high degrees of shock deformation (>10 mately 35 x 45 µm areas. GPa) in quartz and other rock-forming minerals (e.g., Further details on the samples and methodology feldspars), such as planar deformation features (PDFs), can be found in [7]. -
Lechatelierite in Moldavite Tektites: New Analyses of Composition
52nd Lunar and Planetary Science Conference 2021 (LPI Contrib. No. 2548) 1580.pdf LECHATELIERITE IN MOLDAVITE TEKTITES: NEW ANALYSES OF COMPOSITION. Martin Molnár1, Stanislav Šlang2, Karel Ventura3. Kord Ernstson4.1Resselovo nám. 76, Chrudim 537 01, Czech Republic ([email protected]) 2Center of Materials and Nanotechnologies, University of Pardubice, 532 10 Pardubice, Czech Republic, [email protected] 3Faculty of Chemical Technology, University of Pardubice, 530 02 Pardubice, Czech Republic, [email protected]. 4University of Würzburg, D-97074 Würzburg, Deutschland ([email protected]) Introduction: Moldavites are tektites with a Experiments and Results: Experiments 1 and 2 - beautiful, mostly green discoloration and a very the boron question. The question of lowering the pronounced sculpture (Fig.1), which have been studied melting point and acid resistance led to the possibility many times e.g. [1-3]). of adding boron. The experiment 1 on a moldavite plate etched in 15%-HF to expose the lechatelierite was performed by laser ablation spectrometry and showed B2O3 concentration of >1%. In experiment 2, 38 g of lechatelierite fragments were then separated from 482 g of pure moldavite, and after the boron Fig. 1. Moldavites from Besednice analyzed in this content remained high (Tab. 2), the remaining carbon study. Scale bar 1 cm. was washed away. The analysis in Tab. 3 shows According to the most probable theory, they were remaining low boron content, which is obviously formed 14.5 million years ago together with the Ries bound to the carbon of the moldavites [8]. crater meteorite impact in Germany. They belong to the mid-European tektite strewn field and fell mostly in Bohemia.