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Handbook of Iron Meteorites, Volume 3
Sierra Blanca - Sierra Gorda 1119 ing that created an incipient recrystallization and a few COLLECTIONS other anomalous features in Sierra Blanca. Washington (17 .3 kg), Ferry Building, San Francisco (about 7 kg), Chicago (550 g), New York (315 g), Ann Arbor (165 g). The original mass evidently weighed at least Sierra Gorda, Antofagasta, Chile 26 kg. 22°54's, 69°21 'w Hexahedrite, H. Single crystal larger than 14 em. Decorated Neu DESCRIPTION mann bands. HV 205± 15. According to Roy S. Clarke (personal communication) Group IIA . 5.48% Ni, 0.5 3% Co, 0.23% P, 61 ppm Ga, 170 ppm Ge, the main mass now weighs 16.3 kg and measures 22 x 15 x 43 ppm Ir. 13 em. A large end piece of 7 kg and several slices have been removed, leaving a cut surface of 17 x 10 em. The mass has HISTORY a relatively smooth domed surface (22 x 15 em) overlying a A mass was found at the coordinates given above, on concave surface with irregular depressions, from a few em the railway between Calama and Antofagasta, close to to 8 em in length. There is a series of what appears to be Sierra Gorda, the location of a silver mine (E.P. Henderson chisel marks around the center of the domed surface over 1939; as quoted by Hey 1966: 448). Henderson (1941a) an area of 6 x 7 em. Other small areas on the edges of the gave slightly different coordinates and an analysis; but since specimen could also be the result of hammering; but the he assumed Sierra Gorda to be just another of the North damage is only superficial, and artificial reheating has not Chilean hexahedrites, no further description was given. -
Metal-Silicate Fractionation and Chondrule Formation
A756 Goldschmidt 2004, Copenhagen 6.3.12 6.3.13 Metal-silicate fractionation and Fe isotopes fractionation in chondrule formation: Fe isotope experimental chondrules 1 2 2,3 constraints S. LEVASSEUR , B. A. COHEN , B. ZANDA , 2 1 1 1 1 2 2 R.H. HEWINS AND A.N. HALLIDAY X.K. ZHU , Y. GUO , S.H. TANG , A. GALY , R.D. ASH 2 AND R.K O’NIONS 1 ETHZ, Dep. of Earth Sciences, Zürich, Switzerland ([email protected]) 1 Lab of Isotope Geology, MLR, Chinese Academy of 2 Rutgers University, Piscataway, NJ, USA Geological Sciences, 26Baiwanzhuang Road, Beijing, 3 Muséum National d’Histoire Naturelle, Paris, France China ([email protected]) 2 Department of Earth Sciences, Oxford University, Parks Road, Oxford, OX1 3PR, UK Natural chondrules show an Fe-isotopic mass fractionation range of a few δ-units [1,2] that is interpreted either as the result of Fe depletion from metal-silicate Recent studies have shown that considerable variations of fractionation during chondrule formation [1] or as the Fe isotopes exist in both meteoritic and terrestrial materials, reflection of the fractionation range of chondrule precursors and that they are related, through mass-dependent [2]. In order to better understand the iron isotopic fractionation, to a single isotopically homogeneous source[1]. compositions of chondrules we conducted experiments to This implies that the Fe isotope variations recorded in the study the effects of reduction and evaporation of iron on iron solar system materials must have resulted from mass isotope systematics. fractionation incurred by the processes within the solar system About 80mg of powdered slag fayalite was placed in a itself. -
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. -
Lost Lake by Robert Verish
Meteorite-Times Magazine Contents by Editor Like Sign Up to see what your friends like. Featured Monthly Articles Accretion Desk by Martin Horejsi Jim’s Fragments by Jim Tobin Meteorite Market Trends by Michael Blood Bob’s Findings by Robert Verish IMCA Insights by The IMCA Team Micro Visions by John Kashuba Galactic Lore by Mike Gilmer Meteorite Calendar by Anne Black Meteorite of the Month by Michael Johnson Tektite of the Month by Editor Terms Of Use Materials contained in and linked to from this website do not necessarily reflect the views or opinions of The Meteorite Exchange, Inc., nor those of any person connected therewith. In no event shall The Meteorite Exchange, Inc. be responsible for, nor liable for, exposure to any such material in any form by any person or persons, whether written, graphic, audio or otherwise, presented on this or by any other website, web page or other cyber location linked to from this website. The Meteorite Exchange, Inc. does not endorse, edit nor hold any copyright interest in any material found on any website, web page or other cyber location linked to from this website. The Meteorite Exchange, Inc. shall not be held liable for any misinformation by any author, dealer and or seller. In no event will The Meteorite Exchange, Inc. be liable for any damages, including any loss of profits, lost savings, or any other commercial damage, including but not limited to special, consequential, or other damages arising out of this service. © Copyright 2002–2010 The Meteorite Exchange, Inc. All rights reserved. No reproduction of copyrighted material is allowed by any means without prior written permission of the copyright owner. -
March 21–25, 2016
FORTY-SEVENTH LUNAR AND PLANETARY SCIENCE CONFERENCE PROGRAM OF TECHNICAL SESSIONS MARCH 21–25, 2016 The Woodlands Waterway Marriott Hotel and Convention Center The Woodlands, Texas INSTITUTIONAL SUPPORT Universities Space Research Association Lunar and Planetary Institute National Aeronautics and Space Administration CONFERENCE CO-CHAIRS Stephen Mackwell, Lunar and Planetary Institute Eileen Stansbery, NASA Johnson Space Center PROGRAM COMMITTEE CHAIRS David Draper, NASA Johnson Space Center Walter Kiefer, Lunar and Planetary Institute PROGRAM COMMITTEE P. Doug Archer, NASA Johnson Space Center Nicolas LeCorvec, Lunar and Planetary Institute Katherine Bermingham, University of Maryland Yo Matsubara, Smithsonian Institute Janice Bishop, SETI and NASA Ames Research Center Francis McCubbin, NASA Johnson Space Center Jeremy Boyce, University of California, Los Angeles Andrew Needham, Carnegie Institution of Washington Lisa Danielson, NASA Johnson Space Center Lan-Anh Nguyen, NASA Johnson Space Center Deepak Dhingra, University of Idaho Paul Niles, NASA Johnson Space Center Stephen Elardo, Carnegie Institution of Washington Dorothy Oehler, NASA Johnson Space Center Marc Fries, NASA Johnson Space Center D. Alex Patthoff, Jet Propulsion Laboratory Cyrena Goodrich, Lunar and Planetary Institute Elizabeth Rampe, Aerodyne Industries, Jacobs JETS at John Gruener, NASA Johnson Space Center NASA Johnson Space Center Justin Hagerty, U.S. Geological Survey Carol Raymond, Jet Propulsion Laboratory Lindsay Hays, Jet Propulsion Laboratory Paul Schenk, -
Ron Hartman and the Lucerne Valley Meteorites by Robert Verish Ron Hartman and the Lucerne Valley Meteorites
Meteorite Times Magazine Contents by Editor Featured Monthly Articles Accretion Desk by Martin Horejsi Jim's Fragments by Jim Tobin Meteorite Market Trends by Michael Blood Bob's Findings by Robert Verish IMCA Insights by The IMCA Team Micro Visions by John Kashuba Meteorite Calendar by Anne Black Meteorite of the Month by Editor Tektite of the Month by Editor Terms Of Use Materials contained in and linked to from this website do not necessarily reflect the views or opinions of The Meteorite Exchange, Inc., nor those of any person connected therewith. In no event shall The Meteorite Exchange, Inc. be responsible for, nor liable for, exposure to any such material in any form by any person or persons, whether written, graphic, audio or otherwise, presented on this or by any other website, web page or other cyber location linked to from this website. The Meteorite Exchange, Inc. does not endorse, edit nor hold any copyright interest in any material found on any website, web page or other cyber location linked to from this website. The Meteorite Exchange, Inc. shall not be held liable for any misinformation by any author, dealer and or seller. In no event will The Meteorite Exchange, Inc. be liable for any damages, including any loss of profits, lost savings, or any other commercial damage, including but not limited to special, consequential, or other damages arising out of this service. © Copyright 2002–2011 The Meteorite Exchange, Inc. All rights reserved. No reproduction of copyrighted material is allowed by any means without prior written permission of the copyright owner. -
To Thermal History of Metallic Asteroids
44th Lunar and Planetary Science Conference (2013) 1129.pdf TO THERMAL HISTORY OF METALLIC ASTEROIDS. E.N. Slyuta, Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, 119991, Kosygin St. 19, Moscow, Russia. [email protected]. Introduction: Physical-mechanical properties of interval of temperatures T-transition from plastic to a iron meteorites depend on structure, chemical and min- fragile condition in iron meteorites is not observed that eralogical composition, from short-term shock loading usually is not characteristic for technical alloys and and from temperature [1]. The yield strength increases, steels at which at decreasing of temperature the plas- if size of kamacite and rhabdites crystals decreases, ticity can decrease down to 0. For example, for iron- and nickel and carbon contents increases. The more Ni nickel alloy at Ni content about 5% the curve T-bend is content, the more taenite, microhardness of which is observed already about 200 K [5]. The mechanism of more than one of kamacite, and accordingly more yield plastic deformation in iron meteorites at low tempera- strength. Short-term shock loading up to 25 GPа also tures varies only. Deformation at 300 K occurs by slid- increases the yield strength. The temperature of small ing, and at 4.2 K and 77 K is accompanied by forma- bodies which unlike planetary bodies have no en- tion and development of static twins, i.e. mechanical dogenic activity and an internal thermal flux, is de- twinning as the basic mechanism of deformation in fined by insolation level and depends on a body posi- iron meteorites at low temperatures dominates [6]. -
On the Distribution of the Gibeon Meteorites of South-West Africa Robert Citron
https://ntrs.nasa.gov/search.jsp?R=19670023688 2020-03-12T11:14:37+00:00Z ON THE DISTRIBUTION OF THE GIBEON METEORITES OF SOUTH-WEST AFRICA ROBERT CITRON L ZOB WYOl AJ.ll13Vd I. 'b Research in Space Science SA0 Special Report No. 238 ON THE DISTRIBUTION OF THE GIBEON METEORITES OF SOUTH-WEST AFRICA Robert C itron March 30, 1967 Smithsonian Institution Astrophysical Observatory Cambridge, Massachusetts, 02138 TABLE OF CONTENTS Sec tion Page BIOGRAPHICAL NOTE ....................... iv ABSTRACT ............................. -v 1 INTRODUCTION ........................... 1 2 GIBEONDISTRIBUTION ...................... 2 3 RECENTLY RECOVERED GIBEON METEORITES ..... 7 3. 1 The Lichtenfels Meteorite .................. 7 3.2 The Haruchas Meteorite ................... 8 3.3 The Donas Meteorite ...................... 9 3.4 The Bethanie Meteorite .................... 10 3.5 The Keetmanshoop Meteorite ................ 10 3. 6 The Kinas Putts Meteorite ................. 11 3. 7 The Kamkas Meteorite .................... 12 4 POSSIBLE IMPACT CRATERS .................. 15 5 ACKNOWLEDGMENTS ....................... 20 6 REFERENCES ............................ 21 Atmendix A WEIGHT LIST OF KNOWN GIBEON METEORITES - - - * A-1 B GIBEON METEORITES IN MUSEUMS .............. B-1 . C PHOTOGRAPHS OF RECENTLY RECOVERED GIBEON METEORITES ............................. C-1 D PHOTOGRAPHS OF METEORITES IN PUBLIC GARDENS, WINDHOEK, SOUTH-WEST AFRICA .............. D-1 ii LIST OF ILLUSTRATIONS Figure Page 1 Map of known Gibeon meteorite distribution . 5 2a Aerial view of Brukkaros crater . 16 2b Ground view of Brukkaros crater . 17 3 Aerial view of Roter Kamm crater . 19 C-1 The Lichtenfels meteorite . C-2 C-2 The Haruchas meteorite . C-2 C-3 The Donas meteorite . C-3 C-4 The Bethanie meteorite. C-3 C-5 The Kinas Putts meteorite . C-4 D-1 Twenty-seven Gibeon meteorites, whose total weight exceeds 10 metric tons, in the Public Gardens at Windhoek, South-West Africa . -
Research Outputs 1
Research outputs 1. Annealing of the seymchan meteorite at the temperature of 700 °C Brusnitsyna, E. V., Muftakhetdinova, R. F., Yakovlev, G. A., Tyutrina, T. V. & Grokhovsky, V. I., 9 Dec 2020, VII International Young Researchers'' Conference - Physics, Technology, Innovations, PTI 2020. Volkovich, V. A., Kashin, I. V., Smirnov, A. A. & Narkhov, E. D. (eds.). American Institute of Physics Inc., 5 p. 060002. (AIP Conference Proceedings; vol. 2313). 2. Structural features of the seymchan meteorite substance after compressing by spherically converging shock waves Muftakhetdinova, R. F., Grokhovsky, V. I., Kuchko, D. P. & Vorobiev, A. V., 9 Dec 2020, VII International Young Researchers'' Conference - Physics, Technology, Innovations, PTI 2020. Volkovich, V. A., Kashin, I. V., Smirnov, A. A. & Narkhov, E. D. (eds.). American Institute of Physics Inc., 6 p. 060012. (AIP Conference Proceedings; vol. 2313). 3. Synthesis of nanostructures on the Chinga meteorite Begunova, A. S., Yakovlev, G. A., Kamalov, R. V., Pankrushina, E. A. & Grokhovsky, V. I., 9 Dec 2020, VII International Young Researchers'' Conference - Physics, Technology, Innovations, PTI 2020. Volkovich, V. A., Kashin, I. V., Smirnov, A. A. & Narkhov, E. D. (eds.). American Institute of Physics Inc., 6 p. 030039. (AIP Conference Proceedings; vol. 2313). 4. Post-impact metamorphism of the Chelyabinsk meteorite in shock experiment Grokhovsky, V. I., Muftakhetdinova, R. F., Yakovlev, G. A., Brusnitsyna, E. V. & Petrova, E. V., 1 Nov 2020, In: Planetary and Space Science. 192, 8 p., 105050. 5. Experimental constraints on the ordinary chondrite shock darkening caused by asteroid collisions Kohout, T., Petrova, E. V., Yakovlev, G. A., Grokhovsky, V. I., Penttila, A., Maturilli, A., Moreau, J. -
New Unique Pyroxene Pallasite: Northwest Africa 10019 C
78th Annual Meeting of the Meteoritical Society (2015) 5084.pdf NEW UNIQUE PYROXENE PALLASITE: NORTHWEST AFRICA 10019 C. B. Agee, K. Ziegler, N. Muttik. Institute of Meteoritics and the Department of Earth and Planetary Sciences, University of New Mexico. E-mail: [email protected]. Introduction: Pyroxene pallasites were originally defined by the grouplet of Vermillion and Yamato 8451 [1], which have minor amounts (~1-3 vol%) of pyroxene, with oxygen isotope values that are distinct from the pallasite main group (PMG) and the Eagle Station grouplet (PES). In the meantime, additional pyroxene-bearing pallasites, Zinder, NWA 1911, and Choteau, have been discovered [2,3], however each of these meteorites appears to be unique based on oxygen isotopes and mineralogy -- thus not belonging to the original pyroxene pallasite grouplet. Here we report on yet another unique ungrouped pyroxene pallasite, Northwest Africa 10019, which now brings the total of distinct pyroxene pallasite types – possibly all from different parent bodies – to a total of five. History and Physical Chracteristics: NWA 10019 was purchased by Steve Arnold from Morocco in January 2015 and consisted of one 580 gram fusion crusted individual and 26 grams of several small fusion crusted pieces. Saw cuts and thin slices show angular orange-brown-green, translucent olivines (~50 vol%), the largest 28 mm long, with many smaller (0.5-5 mm) angular grains, some of which are darker colored orthopyroxenes (Fs15.4±0.2Wo1.0±0.2, Fe/Mn=23±1, n=6, ~10 vol %), all set in a matrix of taenite (Fe=72.0±4.0, Ni=27.4±2.4, Co=0.19±0.05 wt%, n=5, ~20 vol%) and kamacite (Fe=93.1±2.0, Ni=6.6±0.2, Co=0.61±0.03 wt%, n=4, ~15 vol %). -
W Numerze: – Wywiad Z Kustoszem Watykańskiej Kolekcji C.D. – Cz¹stki
KWARTALNIK MI£OŒNIKÓW METEORYTÓW METEORYTMETEORYT Nr 3 (63) Wrzesieñ 2007 ISSN 1642-588X W numerze: – wywiad z kustoszem watykañskiej kolekcji c.d. – cz¹stki ze Stardusta a meteorytry – trawienie meteorytów – utwory sp³ywania na Sikhote-Alinach – pseudometeoryty – konferencja w Tucson METEORYT Od redaktora: kwartalnik dla mi³oœników OpóŸnieniami w wydawaniu kolejnych numerów zaczynamy meteorytów dorównywaæ „Meteorite”, którego sierpniowy numer otrzyma³em Wydawca: w paŸdzierniku. Tym razem g³ówn¹ przyczyn¹ by³y k³opoty z moim Olsztyñskie Planetarium komputerem, ale w koñcowej fazie redagowania okaza³o siê tak¿e, i Obserwatorium Astronomiczne ¿e brak materia³u. Musia³em wiêc poczekaæ na mocno opóŸniony Al. Pi³sudskiego 38 „Meteorite”, z którego dorzuci³em dwa teksty. 10-450 Olsztyn tel. (0-89) 533 4951 Przeskok o jeden numer niezupe³nie siê uda³, a zapowiedzi¹ [email protected] dalszych k³opotów jest mi³y sk¹din¹d fakt, ¿e przep³yw materia³ów zacz¹³ byæ dwukierunkowy. W najnowszym numerze „Meteorite” konto: ukaza³ siê artyku³ Marcina Cima³y o Moss z „Meteorytu” 3/2006, 88 1540 1072 2001 5000 3724 0002 a w kolejnym numerze zapowiedziany jest artyku³ o Morasku BOŒ SA O/Olsztyn z „Meteorytu” 4/2006. W rezultacie jednak bêdzie mniej materia³u do Kwartalnik jest dostêpny g³ównie t³umaczenia i trzeba postaraæ siê o dalsze w³asne teksty. Czy mo¿e ktoœ w prenumeracie. Roczna prenu- merata wynosi w 2007 roku 44 z³. chcia³by coœ napisaæ? Zainteresowanych prosimy o wp³a- Z przyjemnoœci¹ odnotowujê, ¿e nabieraj¹ tempa przygotowania cenie tej kwoty na konto wydawcy do kolejnej konferencji meteorytowej, która planowana jest na 18—20 nie zapominaj¹c o podaniu czytel- nego imienia, nazwiska i adresu do kwietnia 2008 r. -
Zac Langdon-Pole Art Basel Hong Kong
Zac Langdon-Pole Art Basel Hong Kong Michael Lett 312 Karangahape Road Cnr K Rd & East St PO Box 68287 Newton Auckland 1145 New Zealand P+ 64 9 309 7848 [email protected] www.michaellett.com Zac Langdon-Pole Passport (Argonauta) (i) 2018 paper nautilus shell, Seymchan meteorite (iron pallasite, landsite: Serbia, Russia) 79 x 25 x 45mm ZL5205 Zac Langdon-Pole Passport (Argonauta) (i) (side view) 2018 paper nautilus shell, Seymchan meteorite (iron pallasite, landsite: Serbia, Russia) 79 x 25 x 45mm ZL5205 Zac Langdon-Pole Passport (Argonauta) (ii) 2018 paper nautilus shell, Sikhote Alin meteorite (iron; coarse octahedrite, landsite: Sikhote Alin mountains, Russia) 103 x 30 x 55mm ZL5209 Zac Langdon-Pole Passport (Argonauta) (ii) (side view) 2018 paper nautilus shell, Sikhote Alin meteorite (iron; coarse octahedrite, landsite: Sikhote Alin mountains, Russia) 103 x 30 x 55mm ZL5209 Zac Langdon-Pole Passport (Argonauta) (iii) (front view and side view) 2018 paper nautilus shell, Nantan meteorite (iron; coarse octahedrite, landsite: Nantan, Peoples Republic of China) 135 x 45 x 95mm ZL5213 Zac Langdon-Pole Passport (Argonauta) (iv) (front view and side view) 2018 paper nautilus shell, Muonionalusta meteorite (iron; fine octahedrite, landsite: Norrbotten, Sweden) 95 x 33 x 65mm ZL5208 Zac Langdon-Pole Passport (Argonauta) (v) 2018 paper nautilus shell, Sericho meteorite (iron pallasite, landsite: Sericho, Kenya) 107 x 33 x 56mm ZL5210 Zac Langdon-Pole Passport (Argonauta) (v) (side view) 2018 paper nautilus shell, Sericho meteorite (iron