Chemistry of Space (New Chemistry)
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Warren and Taylor-2014-In Tog-The Moon-'Author's Personal Copy'.Pdf
This article was originally published in Treatise on Geochemistry, Second Edition published by Elsevier, and the attached copy is provided by Elsevier for the author's benefit and for the benefit of the author's institution, for non- commercial research and educational use including without limitation use in instruction at your institution, sending it to specific colleagues who you know, and providing a copy to your institution’s administrator. All other uses, reproduction and distribution, including without limitation commercial reprints, selling or licensing copies or access, or posting on open internet sites, your personal or institution’s website or repository, are prohibited. For exceptions, permission may be sought for such use through Elsevier's permissions site at: http://www.elsevier.com/locate/permissionusematerial Warren P.H., and Taylor G.J. (2014) The Moon. In: Holland H.D. and Turekian K.K. (eds.) Treatise on Geochemistry, Second Edition, vol. 2, pp. 213-250. Oxford: Elsevier. © 2014 Elsevier Ltd. All rights reserved. Author's personal copy 2.9 The Moon PH Warren, University of California, Los Angeles, CA, USA GJ Taylor, University of Hawai‘i, Honolulu, HI, USA ã 2014 Elsevier Ltd. All rights reserved. This article is a revision of the previous edition article by P. H. Warren, volume 1, pp. 559–599, © 2003, Elsevier Ltd. 2.9.1 Introduction: The Lunar Context 213 2.9.2 The Lunar Geochemical Database 214 2.9.2.1 Artificially Acquired Samples 214 2.9.2.2 Lunar Meteorites 214 2.9.2.3 Remote-Sensing Data 215 2.9.3 Mare Volcanism -
7 X 11 Long.P65
Cambridge University Press 978-0-521-85349-1 - Meteor Showers and their Parent Comets Peter Jenniskens Excerpt More information Part I Introduction © Cambridge University Press www.cambridge.org Cambridge University Press 978-0-521-85349-1 - Meteor Showers and their Parent Comets Peter Jenniskens Excerpt More information 1 How meteor showers were linked to comets When we wish upon a falling star, we appeal to an ancient belief that the stars represent our souls and a meteor is one falling into the hereafter.1 In Teutonic mythology, for example, your star was tied to heaven by a thread, spun by the hands of an old woman from the day of your birth, and when it snapped, the star fell and your life had ended.2 The Greek philosophers were the first to speculate on the nature of things without regard to ancient myths. Especially the world views of Aristotle of Stagira (384–322 BC) in his 350 BC book Meteorology3 were widely quoted for over two thousand years, embraced by Christian religion, and passionately defended until into the eight- eenth century. The Greeks held that all matter in the Universe is made of the elements ‘‘earth,’’ ‘‘water,’’ ‘‘air,’’ and ‘‘fire.’’ Aristotle was of the opinion that shooting stars, because of their rapid motion, occurred relatively nearby in the realm of the element ‘‘fire’’ above the layer of ‘‘air’’ that is now called our atmosphere. He believed that shooting stars were not caused by the falling of stars, but were caused by thin streams of a warm and dry ‘‘windy exhalation’’ (a mixture of the elements fire and air) that had risen from dry land warmed by the Sun. -
George P. Merrill Collection, Circa 1800-1930 and Undated
George P. Merrill Collection, circa 1800-1930 and undated Finding aid prepared by Smithsonian Institution Archives Smithsonian Institution Archives Washington, D.C. Contact us at [email protected] Table of Contents Collection Overview ........................................................................................................ 1 Administrative Information .............................................................................................. 1 Historical Note.................................................................................................................. 1 Descriptive Entry.............................................................................................................. 2 Names and Subjects ...................................................................................................... 3 Container Listing ............................................................................................................. 4 Series 1: PHOTOGRAPHS, CORRESPONDENCE AND RELATED MATERIAL CONCERNING INDIVIDUAL GEOLOGISTS AND SCIENTISTS, CIRCA 1800-1920................................................................................................................. 4 Series 2: PHOTOGRAPHS OF GROUPS OF GEOLOGISTS, SCIENTISTS AND SMITHSONIAN STAFF, CIRCA 1860-1930........................................................... 30 Series 3: PHOTOGRAPHS OF THE UNITED STATES GEOLOGICAL AND GEOGRAPHICAL SURVEY OF THE TERRITORIES (HAYDEN SURVEYS), CIRCA 1871-1877.............................................................................................................. -
NWA 5000 – ONE of a KIND? N. Artemieva1,2. 1Planetary Science Institute, [email protected]
77th Annual Meteoritical Society Meeting (2014) 5231.pdf NWA 5000 – ONE OF A KIND? N. Artemieva1,2. 1Planetary Science Institute, [email protected]. 2Instiitute for Dynamics of Geospheres, RAS, Russia. Introduction: The list of lunar meteorites consists of 95 names with the total mass of ~75 kg. The spallation theory [1] and numerical simulations [2-4] allowed to explain the formation of solid high-velocity ejecta and to reconcile the results of nu- merical models with observations. Presence of a porous regolith layer on the Moon decreases at least tenfold the total mass of sol- id escape ejecta because of much lower shock pressures required for shock melting [4]. Projectiles smaller than 10-20 m in diame- ter are able to propel exclusively the regolith (i.e., molten dust with random and unknown inclusions of consolidated breccia or rocks) into space. It means that the contribution of these small cratering events to the flux of lunar meteorites is non-predictable. Larger impact events which are able to excavate underlying megaregolith are statistically unlikely within a short, < 10 kyr, time frame [5]. Thus, one of the biggest (11.5 kg) and the young- est (terrestrial age <10 kyr, [6]) lunar meteorite, NWA 5000 (feldsparic breccia) is a real miracle. Numerical model and initial conditions: High-velocity im- pacts on the Moon are modeled using the 3D hydrocode SOVA [7] complemented by the ANEOS equation of state for geological materials. The lunar regolith porosity is described in the frame of ε-alpha model [8]. Tracer particles are used to find dynamics and thermal history of solid inclusions into the regolith. -
ELEMENTAL ABUNDANCES in the SILICATE PHASE of PALLASITIC METEORITES Redacted for Privacy Abstract Approved: Roman A
AN ABSTRACT OF THE THESIS OF THURMAN DALE COOPER for theMASTER OF SCIENCE (Name) (Degree) in CHEMISTRY presented on June 1, 1973 (Major) (Date) Title: ELEMENTAL ABUNDANCES IN THE SILICATE PHASE OF PALLASITIC METEORITES Redacted for privacy Abstract approved: Roman A. Schmitt The silicate phases of 11 pallasites were analyzed instrumen- tally to determine the concentrations of some major, minor, and trace elements.The silicate phases were found to contain about 98% olivine with 1 to 2% accessory minerals such as lawrencite, schreibersite, troilite, chromite, and farringtonite present.The trace element concentrations, except Sc and Mn, were found to be extremely low and were found primarily in the accessory phases rather than in the pure olivine.An unusual bimodal Mn distribution was noted in the pallasites, and Eagle Station had a chondritic nor- malized REE pattern enrichedin the heavy REE. The silicate phases of pallasites and mesosiderites were shown to be sufficiently diverse in origin such that separate classifications are entirely justified. APPROVED: Redacted for privacy Professor of Chemistry in charge of major Redacted for privacy Chairman of Department of Chemistry Redacted for privacy Dean of Graduate School Date thesis is presented June 1,1973 Typed by Opal Grossnicklaus for Thurman Dale Cooper Elemental Abundances in the Silicate Phase of Pallasitic Meteorites by Thurman Dale Cooper A THESIS submitted to Oregon State University in partial fulfillment of the requirements for the degree of Master of Science June 1974 ACKNOWLEDGMENTS The author wishes to express his gratitude to Prof. Roman A. Schmitt for his guidance, suggestions, discussions, and thoughtful- ness which have served as an inspiration. -
Storm Watchers the Turbulent History of Weather Prediction from Franklin’S Kite to El Niño • John D
Storm Watchers The Turbulent History of Weather Prediction from Franklin’s Kite to El Niño • john d. cox John Wiley & Sons, Inc. 01 cox part 1 6/20/02 11:16 AM Page 12 00 cox fm 6/20/02 11:16 AM Page i Storm Watchers The Turbulent History of Weather Prediction from Franklin’s Kite to El Niño • john d. cox John Wiley & Sons, Inc. 00 cox fm 6/20/02 11:16 AM Page ii To my mother and father, elizabeth cox and ernest y. cox Copyright © 2002 by John D. Cox. All rights reserved Published by John Wiley & Sons, Inc., Hoboken, New Jersey Published simultaneously in Canada No part of this publication may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, recording, scanning, or otherwise, except as permitted under Section 107 or 108 or the 1976 United States Copyright Act, without either the prior written permission of the Publisher, or authorization through payment of the appropriate per-copy fee to the Copyright Clearance Center, 222 Rosewood Drive, Danvers, MA 01923, (978) 750-8400, fax (978) 750-4470, or on the web at www.copyright.com. Requests to the Publiser for permission should be addressed to the Permissions Department, John Wiley & Sons, Inc., 111 River Street, Hoboken, NJ 07030, (201) 748-6011, fax (201) 748-6008, email: permcoordinator@wiley. com. Limit of Liability/Disclaimer of Warranty: While the publisher and author have used their best efforts in preparing this book, they make no representations or warranties with respect to the accuracy or completeness of the contents of this book and specifically disclaim any implied warranties of merchantability or fitness for a particular purpose. -
The Tennessee Meteorite Impact Sites and Changing Perspectives on Impact Cratering
UNIVERSITY OF SOUTHERN QUEENSLAND THE TENNESSEE METEORITE IMPACT SITES AND CHANGING PERSPECTIVES ON IMPACT CRATERING A dissertation submitted by Janaruth Harling Ford B.A. Cum Laude (Vanderbilt University), M. Astron. (University of Western Sydney) For the award of Doctor of Philosophy 2015 ABSTRACT Terrestrial impact structures offer astronomers and geologists opportunities to study the impact cratering process. Tennessee has four structures of interest. Information gained over the last century and a half concerning these sites is scattered throughout astronomical, geological and other specialized scientific journals, books, and literature, some of which are elusive. Gathering and compiling this widely- spread information into one historical document benefits the scientific community in general. The Wells Creek Structure is a proven impact site, and has been referred to as the ‘syntype’ cryptoexplosion structure for the United State. It was the first impact structure in the United States in which shatter cones were identified and was probably the subject of the first detailed geological report on a cryptoexplosive structure in the United States. The Wells Creek Structure displays bilateral symmetry, and three smaller ‘craters’ lie to the north of the main Wells Creek structure along its axis of symmetry. The question remains as to whether or not these structures have a common origin with the Wells Creek structure. The Flynn Creek Structure, another proven impact site, was first mentioned as a site of disturbance in Safford’s 1869 report on the geology of Tennessee. It has been noted as the terrestrial feature that bears the closest resemblance to a typical lunar crater, even though it is the probable result of a shallow marine impact. -
Meteorite Collections: Sample List
Meteorite Collections: Sample List Institute of Meteoritics Department of Earth and Planetary Sciences University of New Mexico October 01, 2021 Institute of Meteoritics Meteorite Collection The IOM meteorite collection includes samples from approximately 600 different meteorites, representative of most meteorite types. The last printed copy of the collection's Catalog was published in 1990. We will no longer publish a printed catalog, but instead have produced this web-based Online Catalog, which presents the current catalog in searchable and downloadable forms. The database will be updated periodically. The date on the front page of this version of the catalog is the date that it was downloaded from the worldwide web. The catalog website is: Although we have made every effort to avoid inaccuracies, the database may still contain errors. Please contact the collection's Curator, Dr. Rhian Jones, ([email protected]) if you have any questions or comments. Cover photos: Top left: Thin section photomicrograph of the martian shergottite, Zagami (crossed nicols). Brightly colored crystals are pyroxene; black material is maskelynite (a form of plagioclase feldspar that has been rendered amorphous by high shock pressures). Photo is 1.5 mm across. (Photo by R. Jones.) Top right: The Pasamonte, New Mexico, eucrite (basalt). This individual stone is covered with shiny black fusion crust that formed as the stone fell through the earth's atmosphere. Photo is 8 cm across. (Photo by K. Nicols.) Bottom left: The Dora, New Mexico, pallasite. Orange crystals of olivine are set in a matrix of iron, nickel metal. Photo is 10 cm across. (Photo by K. -
From the Moon to the Earth Without Jules Verne — Lunar Meteorites
45th Lunar and Planetary Science Conference (2014) 1659.pdf FROM THE MOON TO THE EARTH WITHOUT JULES VERNE – LUNAR METEORITES AND LU- NAR DUST DELIVERY. N. Artemieva1,2, 1Planetary Sciene Institute, [email protected], 2Institute for Dynamics of Geopsheres, Russia. Introduction: The list of lunar meteorites [1] con- required to melt porous materials, is much lower than sists of 95 names (taking into account obvious pairs) 50 -60 GPa [17]. Second, the spall effect is noticeably with the total mass of ~75 kg, which is approximately weaker in porous media [15, 18]. Another goal is to five times smaller than the total mass of lunar samples evaluate the total mass and 3He losses in the terrestrial delivered by the Apollo and Luna missions. In contrast atmosphere during the entry process. Mass losses may to “technical samples” lunar meteorites represent a be as high as 90% in typical meteorites [19]. random set of lunar material, including that from the Numerical model and initial conditions: High- far side of the Moon. Taking into account the diversity velocity impacts on the Moon are modeled using the of the available lunar meteorites probably associated 3D hydrocode SOVA [20] complemented by the with various impact events [2], the short time of their ANEOS equation of state for geological materials [21]. transportation to Earth [3, 4], and the distribution of The lunar regolith porosity is described in the frame of the crater size and age over the Moon [5], we can con- ε-alpha model [22].Tracer particles are used to find the clude that most of the lunar meteorites were ejected maximum shock compression and the initial depth of from the Moon during small impact events associated solid ejecta escaping the Moon (SEEM). -
Paneth Kolloquium 2005, Nördlingen Dear Participants, the List of Authors
Paneth Kolloquium 2005, Nördlingen Dear participants, the list of authors is arranged in alphabetical order. Abstracts are sorted by their reference numbers. Abstracts can be accessed from the list of authors via a “click” on the abstract reference number. Your organization team. For citations, we suggest using the form: Miller, G. (2005) The importance of carbon for life. Paneth Kolloquium, Nördlingen, #043 (abstract). All abstracts will be available on the web at http://www.cosmochemistry.org/paneth2005.html List of authors (in alphabetical order) Ammon, K. and I. Leya: Noble gas measurements in Grant IIIAB iron meteorite. abstract #007. Becker, H.: Highly siderophile elements as tracers for late accretion. abstract #27. Grimberg, A., Wieler, R., et al.: Surface studies and preliminary noble gas data from bulk metallic glass flown on GENESIS. abstract #005. Hezel, D.C.: Modeling 3-dimensional objects from 2-dimensional thin sections. abstract #006. Huber, L., B. Hofmann, I. Leya: The exposure history of the JaH 073 meteorite. abstract #014. Jagoutz, E., Jotter, R., Kubny, A., Zartman, R.: U-Pb isotope systematic of SNC meteorites. abstract #002. Kießwetter R., Palme, H., Hezel, D.C.: 3-dimensional, chemical analysis of Efremovka (CV3 ) chondrules. abstract #023. Kleine, T., Palme, H., Mezger, K., and Halliday, A.N.: Hf–W chronometry of lunar metals and the age and early differentiation of the Moon. abstract #021. Marhas, K. K. and Hoppe, P.: In-situ Search of Presolar Grains. abstract #017. Markowski, A., I. Leya, G. Quitté, R. Wieler, A.N. Halliday: Experimental evidence of cosmogenic effects on tungsten isotopic composition in iron meteorites. -
Fersman Mineralogical Museum of the Russian Academy of Sciences (FMM)
Table 1. The list of meteorites in the collections of the Fersman Mineralogical Museum of the Russian Academy of Sciences (FMM). Leninskiy prospect 18 korpus 2, Moscow, Russia, 119071. Pieces Year Mass in Indication Meteorite Country Type in found FMM in MB FMM Seymchan Russia 1967 Pallasite, PMG 500 kg 9 43 Kunya-Urgench Turkmenistan 1998 H5 402 g 2 83 Sikhote-Alin Russia 1947 Iron, IIAB 1370 g 2 Sayh Al Uhaymir 067 Oman 2000 L5-6 S1-2,W2 63 g 1 85 Ozernoe Russia 1983 L6 75 g 1 66 Gujba Nigeria 1984 Cba 2..8 g 1 85 Dar al Gani 400 Libya 1998 Lunar (anorth) 0.37 g 1 82 Dhofar 935 Oman 2002 H5S3W3 96 g 1 88 Dhofar 007 Oman 1999 Eucrite-cm 31.5 g 1 84 Muonionalusta Sweden 1906 Iron, IVA 561 g 3 Omolon Russia 1967 Pallasite, PMG 1,2 g 1 72 Peekskill USA 1992 H6 1,1 g 1 75 Gibeon Namibia 1836 Iron, IVA 120 g 2 36 Potter USA 1941 L6 103.8g 1 Jiddat Al Harrasis 020 Oman 2000 L6 598 gr 2 85 Canyon Diablo USA 1891 Iron, IAB-MG 329 gr 1 33 Gold Basin USA 1995 LA 101 g 1 82 Campo del Cielo Argentina 1576 Iron, IAB-MG 2550 g 4 36 Dronino Russia 2000 Iron, ungrouped 22 g 1 88 Morasko Poland 1914 Iron, IAB-MG 164 g 1 Jiddat al Harasis 055 Oman 2004 L4-5 132 g 1 88 Tamdakht Morocco 2008 H5 18 gr 1 Holbrook USA 1912 L/LL5 2,9g 1 El Hammami Mauritani 1997 H5 19,8g 1 82 Gao-Guenie Burkina Faso 1960 H5 18.7 g 1 83 Sulagiri India 2008 LL6 2.9g 1 96 Gebel Kamil Egypt 2009 Iron ungrouped 95 g 2 98 Uruacu Brazil 1992 Iron, IAB-MG 330g 1 86 NWA 859 (Taza) NWA 2001 Iron ungrouped 18,9g 1 86 Dhofar 224 Oman 2001 H4 33g 1 86 Kharabali Russia 2001 H5 85g 2 102 Chelyabinsk -
WORKSHOP on the ARCHEAN MANTLE D/,,5 #O 4
WORKSHOP ON THE ARCHEAN MANTLE d/,,5_ #o _4, T-IQO0-2000°C not tohorizontal scale (NASA-CR-18_ISb) WnRKSHOP ON THE APCHEAN N90-t47_o MANTLF (Lunar and Planotary Inst.) 105 p CcCL 08G Unc13s n3I_6 0253134 LPI Technical Report Number 89-05 LUNAR AND PLANETARY INSTITUTE 33c3 NASA ROAD HOUSTON, TEXAS 77058-4399 WORKSHOP ON THE ARCHEAN MANTLE Edited by L. D. Ashwal Organizing Committee L. D. Ashwal, K. Burke, I.D. MacGregor, A. J. Naldrett, W. C. Phinney, F. Richter, and S. B. Shirey Sponsored by Lunar and Planetary Institute NASA Johnson Space Center January 11-13, 1989 Houston, Texas Lunar and Planetary Institute 3303 NASA Road 1 Houston, Texas 77058-4399 LPI Technical Report Number 89-05 Compiled in 1989 by the LUNAR AND PLANETARY INSTITUTE The Institute is operated by Universities Space Research Association under Contract NASW-4066 with the National Aeronautics and Space Administration. Material in this document may be copied without restraint for library, abstract service, educational, or personal research purposes; however, republication of any portion requires the written permission of the authors as well as appropriate acknowledgment of this publication. This report may be cited as: Ashwal L. D., ed. (1989) Workshop on The Archean Mant/e. LPI Tech. Rpt. 89-05. Lunar and Planetary Institute, Houston. 104 pp. Papers in this report may be cited as: Author A. A. (1989) Title of paper. In Workshop on The Archean Mant/e (L. D. Ashwal, ed.), pp. xx-yy. LPI Tech Rpt. 89-05. Lunar and Planetary Institute, Houston. This report is distributed by: ORDER DEPARTMENT Lunar and Planetary Institute 3303 NASA Road 1 Houston, TX 77058-4399 Mail order requestors will be invoiced for the cost of shipping and handling.