Thesis, Revised
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Template for Two-Page Abstracts in Word 97 (PC)
GEOLOGIC MAPPING OF THE LUNAR SOUTH POLE QUADRANGLE (LQ-30). S.C. Mest1,2, D.C. Ber- man1, and N.E. Petro2, 1Planetary Science Institute, 1700 E. Ft. Lowell, Suite 106, Tucson, AZ 85719-2395 ([email protected]); 2Planetary Geodynamics Laboratory, Code 698, NASA GSFC, Greenbelt, MD 20771. Introduction: In this study we use recent image, the surface [7]. Impact craters display morphologies spectral and topographic data to map the geology of the ranging from simple to complex [7-9,24] and most lunar South Pole quadrangle (LQ-30) at 1:2.5M scale contain floor deposits distinct from surrounding mate- [1-7]. The overall objective of this research is to con- rials. Most of these deposits likely consist of impact strain the geologic evolution of LQ-30 (60°-90°S, 0°- melt; however, some deposits, especially on the floors ±180°) with specific emphasis on evaluation of a) the of the larger craters and basins (e.g., Antoniadi), ex- regional effects of impact basin formation, and b) the hibit low albedo and smooth surfaces and may contain spatial distribution of ejecta, in particular resulting mare. Higher albedo deposits tend to contain a higher from formation of the South Pole-Aitken (SPA) basin density of superposed impact craters. and other large basins. Key scientific objectives in- Antoniadi Crater. Antoniadi crater (D=150 km; clude: 1) Determining the geologic history of LQ-30 69.5°S, 172°W) is unique for several reasons. First, and examining the spatial and temporal variability of Antoniadi is the only lunar crater that contains both a geologic processes within the map area. -
Martian Crater Morphology
ANALYSIS OF THE DEPTH-DIAMETER RELATIONSHIP OF MARTIAN CRATERS A Capstone Experience Thesis Presented by Jared Howenstine Completion Date: May 2006 Approved By: Professor M. Darby Dyar, Astronomy Professor Christopher Condit, Geology Professor Judith Young, Astronomy Abstract Title: Analysis of the Depth-Diameter Relationship of Martian Craters Author: Jared Howenstine, Astronomy Approved By: Judith Young, Astronomy Approved By: M. Darby Dyar, Astronomy Approved By: Christopher Condit, Geology CE Type: Departmental Honors Project Using a gridded version of maritan topography with the computer program Gridview, this project studied the depth-diameter relationship of martian impact craters. The work encompasses 361 profiles of impacts with diameters larger than 15 kilometers and is a continuation of work that was started at the Lunar and Planetary Institute in Houston, Texas under the guidance of Dr. Walter S. Keifer. Using the most ‘pristine,’ or deepest craters in the data a depth-diameter relationship was determined: d = 0.610D 0.327 , where d is the depth of the crater and D is the diameter of the crater, both in kilometers. This relationship can then be used to estimate the theoretical depth of any impact radius, and therefore can be used to estimate the pristine shape of the crater. With a depth-diameter ratio for a particular crater, the measured depth can then be compared to this theoretical value and an estimate of the amount of material within the crater, or fill, can then be calculated. The data includes 140 named impact craters, 3 basins, and 218 other impacts. The named data encompasses all named impact structures of greater than 100 kilometers in diameter. -
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, -
Relative Ages
CONTENTS Page Introduction ...................................................... 123 Stratigraphic nomenclature ........................................ 123 Superpositions ................................................... 125 Mare-crater relations .......................................... 125 Crater-crater relations .......................................... 127 Basin-crater relations .......................................... 127 Mapping conventions .......................................... 127 Crater dating .................................................... 129 General principles ............................................. 129 Size-frequency relations ........................................ 129 Morphology of large craters .................................... 129 Morphology of small craters, by Newell J. Fask .................. 131 D, method .................................................... 133 Summary ........................................................ 133 table 7.1). The first three of these sequences, which are older than INTRODUCTION the visible mare materials, are also dominated internally by the The goals of both terrestrial and lunar stratigraphy are to inte- deposits of basins. The fourth (youngest) sequence consists of mare grate geologic units into a stratigraphic column applicable over the and crater materials. This chapter explains the general methods of whole planet and to calibrate this column with absolute ages. The stratigraphic analysis that are employed in the next six chapters first step in reconstructing -
Discoveries of Mass Independent Isotope Effects in the Solar System: Past, Present and Future Mark H
Reviews in Mineralogy & Geochemistry Vol. 86 pp. 35–95, 2021 2 Copyright © Mineralogical Society of America Discoveries of Mass Independent Isotope Effects in the Solar System: Past, Present and Future Mark H. Thiemens Department of Chemistry and Biochemistry University of California San Diego La Jolla, California 92093 USA [email protected] Mang Lin State Key Laboratory of Isotope Geochemistry Guangzhou Institute of Geochemistry, Chinese Academy of Sciences Guangzhou, Guangdong 510640 China University of Chinese Academy of Sciences Beijing 100049 China [email protected] THE BEGINNING OF ISOTOPES Discovery and chemical physics The history of the discovery of stable isotopes and later, their influence of chemical and physical phenomena originates in the 19th century with discovery of radioactivity by Becquerel in 1896 (Becquerel 1896a–g). The discovery catalyzed a range of studies in physics to develop an understanding of the nucleus and the properties influencing its stability and instability that give rise to various decay modes and associated energies. Rutherford and Soddy (1903) later suggested that radioactive change from different types of decay are linked to chemical change. Soddy later found that this is a general phenomenon and radioactive decay of different energies and types are linked to the same element. Soddy (1913) in his paper on intra-atomic charge pinpointed the observations as requiring the observations of the simultaneous character of chemical change from the same position in the periodic chart with radiative emissions required it to be of the same element (same proton number) but differing atomic weight. This is only energetically accommodated by a change in neutrons and it was this paper that the name “isotope” emerges. -
Appendix I Lunar and Martian Nomenclature
APPENDIX I LUNAR AND MARTIAN NOMENCLATURE LUNAR AND MARTIAN NOMENCLATURE A large number of names of craters and other features on the Moon and Mars, were accepted by the IAU General Assemblies X (Moscow, 1958), XI (Berkeley, 1961), XII (Hamburg, 1964), XIV (Brighton, 1970), and XV (Sydney, 1973). The names were suggested by the appropriate IAU Commissions (16 and 17). In particular the Lunar names accepted at the XIVth and XVth General Assemblies were recommended by the 'Working Group on Lunar Nomenclature' under the Chairmanship of Dr D. H. Menzel. The Martian names were suggested by the 'Working Group on Martian Nomenclature' under the Chairmanship of Dr G. de Vaucouleurs. At the XVth General Assembly a new 'Working Group on Planetary System Nomenclature' was formed (Chairman: Dr P. M. Millman) comprising various Task Groups, one for each particular subject. For further references see: [AU Trans. X, 259-263, 1960; XIB, 236-238, 1962; Xlffi, 203-204, 1966; xnffi, 99-105, 1968; XIVB, 63, 129, 139, 1971; Space Sci. Rev. 12, 136-186, 1971. Because at the recent General Assemblies some small changes, or corrections, were made, the complete list of Lunar and Martian Topographic Features is published here. Table 1 Lunar Craters Abbe 58S,174E Balboa 19N,83W Abbot 6N,55E Baldet 54S, 151W Abel 34S,85E Balmer 20S,70E Abul Wafa 2N,ll7E Banachiewicz 5N,80E Adams 32S,69E Banting 26N,16E Aitken 17S,173E Barbier 248, 158E AI-Biruni 18N,93E Barnard 30S,86E Alden 24S, lllE Barringer 29S,151W Aldrin I.4N,22.1E Bartels 24N,90W Alekhin 68S,131W Becquerei -
1 2.6 Physical Chemistry and Thermal Evolution of Ices at Ganymede 1 C
1 1 2.6 Physical Chemistry and Thermal Evolution of Ices at Ganymede 2 C. Ahrens, NASA Goddard Space Flight Center, Greenbelt, MD; [email protected] 3 A. Solomonidou, Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA; & LEISA 4 – Observatoire de Paris, CNRS, UPMC Univ., Paris 06, Univ. Paris-Diderot, Meudon, France; 5 [email protected] 6 K. Stephan, Institute of Planetary Research, German Aerospace Center (DLR), Berlin, Germany; 7 [email protected] 8 K. Kalousova, Charles University, Faculty of Mathematics and Physics, Department of Geophysics, 9 Prague, Czech Republic; [email protected] 10 N. Ligier, Institut d’Astrophysique Spatiale, Université Paris-Saclay, Orsay, France; 11 [email protected] 12 T. McCord, Bear Fight Institute, Winthrop, WA; [email protected] 13 C. Hibbitts, Applied Physics Laboratory, Johns Hopkins University, Laurel, MD; 14 [email protected] 15 16 Abstract 17 18 Ganymede’s surface is composed mostly of water ice and other icy materials in addition to minor non-ice 19 components. The formation and evolution of Ganymede’s landforms highly depend on the nature of the 20 icy materials as they present various thermal and rheological behaviors. This chapter reviews the 21 currently known thermodynamic parameters of the ice phases and hydrates reported on Ganymede, which 22 seem to affect the evolution of the surface, using mainly results from the Voyager and Galileo missions. 23 24 Keywords: Ganymede; Ices; Ices, Mechanical Properties; Experimental techniques; Geological 25 processes 26 27 1 Introduction 28 29 Icy bodies of the outer solar system, including satellites of the gas giants, harbor surface ices made of 30 volatile molecules, clathrates, and complex molecules like hydrocarbons. -
Palaeoenvironment in North-Western Romania During the Last 15,000 Years
Palaeoenvironment in north-western Romania during the last 15,000 years Angelica Feurdean Dedicated to Ovidiu Feurdean Avhandling i Kvartärgeologi Thesis in Quaternary Geology No. 3 Department of Physical Geography and Quaternary Geology, Stockholm University 2004 1 ISBN 2 Palaeoenvironment in north-western Romania during the last 15,000 years by Angelica Feurdean Department of Physical Geography and Quaternary Geology, Stockholm University, SE-106 91 Stockholm This thesis is based on work carried out as Ph.D. stu- Appendix III: Feurdean A. (in press). Holocene forest dent at the Department of Paleontology, Faculty of Biol- dynamics in north-western Romania. The Holocene. ogy and Geology, Babes-Bolyai University, Cluj-Napoca, Romania between Oct. 1998 and Sept. 2002 and later as Appendix IV: Feurdean A. & Bennike O. Late Quater- Ph.D. student in Quaternary Geology at the Department nary palaeocological and paleoclimatological reconstruc- of Physical Geography and Quaternary Geology, tion in the Gutaiului Mountains, NW Romania. Manu- Stockholm University 2002-2004. The thesis consists of script submitted to Journal of Quaternary Science. four papers and a synthesis. The four papers are listed below and presented in Appendices I-IV. Two of the pa- Fieldwork in Romania has been jointly performed with pers have been published (I, II), one is in press (III) and Barbara Wohlfarth and Leif Björkman (Preluca Tiganului, the fourth has been submitted (IV). The thesis summary Steregoiu, Izvoare) and with Bogdan Onac (Creasta presents an account of earlier pollenstratigraphic work Cocosului). I am responsible for the lithostratigraphic done in Romania and the discussion focuses on tree description of all sediment and peat cores, for sub-sam- dynamics during the Lateglacial and Holocene, based pling and laboratory preparation. -
Arxiv:2008.11207V2 [Astro-Ph.GA] 17 Nov 2020 Milky Way’S “Classical Dwarf” Satellite Galaxies
Draft version November 19, 2020 Typeset using LATEX twocolumn style in AASTeX63 Ultra-faint dwarfs in a Milky Way context: Introducing the Mint Condition DC Justice League Simulations Elaad Applebaum ,1 Alyson M. Brooks ,1 Charlotte R. Christensen ,2 Ferah Munshi ,3 Thomas R. Quinn,4 Sijing Shen ,5 and Michael Tremmel 6 1Department of Physics and Astronomy, Rutgers, The State University of New Jersey, 136 Frelinghuysen Rd., Piscataway, NJ 08854, USA 2Physics Department, Grinnell College, 1116 Eighth Avenue, Grinnell, IA 50112, USA 3Department of Physics & Astronomy, University of Oklahoma, 440 W. Brooks St., Norman, OK 73019, USA 4Department of Astronomy, University of Washington, Box 351580, Seattle, WA, 98115, USA 5Institute of Theoretical Astrophysics, University of Oslo, Postboks 1029, 0315 Oslo, Norway 6Physics Department, Yale Center for Astronomy & Astrophysics, PO Box 208120, New Haven, CT 06520, USA ABSTRACT We present results from the \Mint" resolution DC Justice League suite of Milky Way-like zoom-in cosmological simulations, which extend our study of nearby galaxies down into the ultra-faint dwarf (UFD) regime for the first time. The mass resolution of these simulations is the highest ever published for cosmological Milky Way zoom-in simulations run to z = 0, with initial star (dark matter) particle masses of 994 (17900) M , and a force resolution of 87 pc. We study the surrounding dwarfs and UFDs, and find the simulations match the observed dynamical properties of galaxies with −3 < MV < −19, and reproduce the scatter seen in the size-luminosity plane for rh & 200 pc. We predict the vast majority of nearby galaxies will be observable by the Vera Rubin Observatory's co-added Legacy Survey of Space and Time (LSST). -
Ecologia Balkanica
ECOLOGIA BALKANICA International Scientific Research Journal of Ecology Volume 4, Issue 1 June 2012 UNION OF SCIENTISTS IN BULGARIA – PLOVDIV UNIVERSITY OF PLOVDIV PUBLISHING HOUSE ii International Standard Serial Number Print ISSN 1314-0213; Online ISSN 1313-9940 Aim & Scope „Ecologia Balkanica” is an international scientific journal, in which original research articles in various fields of Ecology are published, including ecology and conservation of microorganisms, plants, aquatic and terrestrial animals, physiological ecology, behavioural ecology, population ecology, population genetics, community ecology, plant-animal interactions, ecosystem ecology, parasitology, animal evolution, ecological monitoring and bioindication, landscape and urban ecology, conservation ecology, as well as new methodical contributions in ecology. Studies conducted on the Balkans are a priority, but studies conducted in Europe or anywhere else in the World is accepted as well. Published by the Union of Scientists in Bulgaria – Plovdiv and the University of Plovdiv Publishing house – twice a year. Language: English. Peer review process All articles included in “Ecologia Balkanica” are peer reviewed. Submitted manuscripts are sent to two or three independent peer reviewers, unless they are either out of scope or below threshold for the journal. These manuscripts will generally be reviewed by experts with the aim of reaching a first decision as soon as possible. The journal uses the double anonymity standard for the peer-review process. Reviewers do not have to sign their reports and they do not know who the author(s) of the submitted manuscript are. We ask all authors to provide the contact details (including e-mail addresses) of at least four potential reviewers of their manuscript. -
Mars Express
sp1240cover 7/7/04 4:17 PM Page 1 SP-1240 SP-1240 M ARS E XPRESS The Scientific Payload MARS EXPRESS The Scientific Payload Contact: ESA Publications Division c/o ESTEC, PO Box 299, 2200 AG Noordwijk, The Netherlands Tel. (31) 71 565 3400 - Fax (31) 71 565 5433 AAsec1.qxd 7/8/04 3:52 PM Page 1 SP-1240 August 2004 MARS EXPRESS The Scientific Payload AAsec1.qxd 7/8/04 3:52 PM Page ii SP-1240 ‘Mars Express: A European Mission to the Red Planet’ ISBN 92-9092-556-6 ISSN 0379-6566 Edited by Andrew Wilson ESA Publications Division Scientific Agustin Chicarro Coordination ESA Research and Scientific Support Department, ESTEC Published by ESA Publications Division ESTEC, Noordwijk, The Netherlands Price €50 Copyright © 2004 European Space Agency ii AAsec1.qxd 7/8/04 3:52 PM Page iii Contents Foreword v Overview The Mars Express Mission: An Overview 3 A. Chicarro, P. Martin & R. Trautner Scientific Instruments HRSC: the High Resolution Stereo Camera of Mars Express 17 G. Neukum, R. Jaumann and the HRSC Co-Investigator and Experiment Team OMEGA: Observatoire pour la Minéralogie, l’Eau, 37 les Glaces et l’Activité J-P. Bibring, A. Soufflot, M. Berthé et al. MARSIS: Mars Advanced Radar for Subsurface 51 and Ionosphere Sounding G. Picardi, D. Biccari, R. Seu et al. PFS: the Planetary Fourier Spectrometer for Mars Express 71 V. Formisano, D. Grassi, R. Orfei et al. SPICAM: Studying the Global Structure and 95 Composition of the Martian Atmosphere J.-L. Bertaux, D. Fonteyn, O. Korablev et al. -
Topographic Characterization of Lunar Complex Craters Jessica Kalynn,1 Catherine L
GEOPHYSICAL RESEARCH LETTERS, VOL. 40, 38–42, doi:10.1029/2012GL053608, 2013 Topographic characterization of lunar complex craters Jessica Kalynn,1 Catherine L. Johnson,1,2 Gordon R. Osinski,3 and Olivier Barnouin4 Received 20 August 2012; revised 19 November 2012; accepted 26 November 2012; published 16 January 2013. [1] We use Lunar Orbiter Laser Altimeter topography data [Baldwin 1963, 1965; Pike, 1974, 1980, 1981]. These studies to revisit the depth (d)-diameter (D), and central peak height yielded three main results. First, depth increases with diam- B (hcp)-diameter relationships for fresh complex lunar craters. eter and is described by a power law relationship, d =AD , We assembled a data set of young craters with D ≥ 15 km where A and B are constants determined by a linear least and ensured the craters were unmodified and fresh using squares fit of log(d) versus log(D). Second, a change in the Lunar Reconnaissance Orbiter Wide-Angle Camera images. d-D relationship is seen at diameters of ~15 km, roughly We used Lunar Orbiter Laser Altimeter gridded data to coincident with the morphological transition from simple to determine the rim-to-floor crater depths, as well as the height complex craters. Third, craters in the highlands are typically of the central peak above the crater floor. We established deeper than those formed in the mare at a given diameter. power-law d-D and hcp-D relationships for complex craters At larger spatial scales, Clementine [Williams and Zuber, on mare and highlands terrain. Our results indicate that 1998] and more recently, Lunar Orbiter Laser Altimeter craters on highland terrain are, on average, deeper and have (LOLA) [Baker et al., 2012] topography data indicate that higher central peaks than craters on mare terrain.