Program to Technical Sessions Thirty-Fourth Lunar and Planetary Science Conference March 17-21, 2003
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Comprehensive Bibliography on Martian Meteorites (Compiled by C
Comprehensive Bibliography on Martian Meteorites (compiled by C. Meyer, March 2008) Abu Aghreb A.E., Ghadi A.M., Schlüter J., Schultz L. and Thiedig F. (2003) Hamadah al Hamra and Dar al Gani: A comparison of two meteorite fields in the Libyan Sahara (abs). Meteoritics & Planet. Sci. 38, A48. Agee Carl B. (2002) Garnet and majorite fractionation in the early Earth and Mars (abs#1862). Lunar Planet. Sci. XXXIII Lunar Planetary Institute, Houston. (CD-ROM). (see address of LPI in Appendix III) Agee C.B., Bogard Don D., Draper D.S., Jones J.H., Meyer Chuck and Mittlefehldt D.W. (2000) Proposed science requirements and acquisition priorities for the first Mars sample return (abs). In Concept and Approaches for Mars Exploration. Part 1 (ed. S. Hubbard) LPI Contribution # 1062. Lunar Planetary Institute, Houston. Agee C.B. and Draper Dave S. (2003) Melting of model Martian mantle at high pressure: Implications for the composition of the Martian basalt source region (abs#1408). Lunar Planet. Sci. Conf. 34th, Lunar Planetary Institute, Houston (CD-ROM). Agerkvist D.P. and Vistisen L. (1993) Mössbauer spectroscopy of the SNC meteorite Zagami (abs). Lunar Planet. Sci. XXIV, 1-2. Lunar Planetary Institute, Houston. Zagami Agerkvist D.P., Vistisen L., Madsen M.B. and Knudsen J.M. (1994) Magnetic properties of Zagami and Nakhla (abs). Lunar Planet. Sci. XXV, 1-2. Lunar Planetary Institute, Houston. Zagami Nakhla Akai J. (1997) Characteristics of iron-oxide and iron-sulfide grains in meteorites and terrestrial sediments, with special references to magnetite grains in Allan Hills 84001 (abs). Meteoritics & Planet. Sci. -
Scientific Rationale and Requirements for a Global Seismic Network on Mars
SCIENTIFIC RATIONALE AND REQUIREMENTS FOR A GLOBAL SEISMIC NETWORK ON MARS MARS Model AR 90 EARTH 180 (NASA-CR-188806) SCIENTIFIC RATIONALE AND N92-14949 REQUIREMENTS FOR A GLOBAL SEISMIC NETWORK ON MARS (Lunar and Planetary Inst.) 48 p CSCL 03B Unclas G3/91 0040098 LPI Technical Report Number 91-02 LUNAR AND PLANETARY INSTITUTE 3303 NASA ROAD 1 HOUSTON TX 77058-4399 LPI/TR-91-02 SCIENTIFIC RATIONALE AND REQUIREMENTS FOR A GLOBAL SEISMIC NETWORK ON MARS Sean C. Solomon, Don L. Anderson, W. Bruce Banerdt, Rhett G. Butler, Paul M. Davis, Frederick K. Duennebier, Yosio Nakamura, Emile A. Okal, and Roger J. Phillips Report of a Workshop Held at Morro Bay, California May 7-9, 1990 Lunar and Planetary Institute 3303 NASA Road 1 Houston TX 77058 LPI Technical Report Number 91-02 LPI/TR-91-02 Compiled in 1991 by the LUNAR AND PLANETARY INSTITUTE The Institute is operated by Universities Space Research Association under Contract NASW-4574 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: Solomon S. C. et al. (1991) Scientific Rationale and Requirements far a Global Seismic Network on Mars. LPI Tech. Rpt. 91-02, Lunar and Planetary Institute, Houston. 51 pp. 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. -
Disequilibrium Melting and Melt Migration Driven by Impacts: Implications for Rapid Planetesimal Core Formation
Available online at www.sciencedirect.com Geochimica et Cosmochimica Acta 100 (2013) 41–59 www.elsevier.com/locate/gca Disequilibrium melting and melt migration driven by impacts: Implications for rapid planetesimal core formation Andrew G. Tomkins ⇑, Roberto F. Weinberg, Bruce F. Schaefer 1, Andrew Langendam School of Geosciences, P.O. Box 28E, Monash University, Melbourne, Victoria 3800, Australia Received 20 January 2012; accepted in revised form 24 September 2012; available online 12 October 2012 Abstract The e182W ages of magmatic iron meteorites are largely within error of the oldest solar system particles, apparently requir- ing a mechanism for segregation of metals to the cores of planetesimals within 1.5 million years of initial condensation. Cur- rently favoured models involve equilibrium melting and gravitational segregation in a static, quiescent environment, which requires very high early heat production in small bodies via decay of short-lived radionuclides. However, the rapid accretion needed to do this implies a violent early accretionary history, raising the question of whether attainment of equilibrium is a valid assumption. Since our use of the Hf–W isotopic system is predicated on achievement of chemical equilibrium during core formation, our understanding of the timing of this key early solar system process is dependent on our knowledge of the seg- regation mechanism. Here, we investigate impact-related textures and microstructures in chondritic meteorites, and show that impact-generated deformation promoted separation of liquid FeNi into enlarged sulfide-depleted accumulations, and that this happened under conditions of thermochemical disequilibrium. These observations imply that similar enlarged metal accumu- lations developed as the earliest planetesimals grew by rapid collisional accretion. -
Meteorologia
MINISTÉRIO DA DEFESA COMANDO DA AERONÁUTICA METEOROLOGIA ICA 105-1 DIVULGAÇÃO DE INFORMAÇÕES METEOROLÓGICAS 2006 MINISTÉRIO DA DEFESA COMANDO DA AERONÁUTICA DEPARTAMENTO DE CONTROLE DO ESPAÇO AÉREO METEOROLOGIA ICA 105-1 DIVULGAÇÃO DE INFORMAÇÕES METEOROLÓGICAS 2006 MINISTÉRIO DA DEFESA COMANDO DA AERONÁUTICA DEPARTAMENTO DE CONTROLE DO ESPAÇO AÉREO PORTARIA DECEA N° 15/SDOP, DE 25 DE JULHO DE 2006. Aprova a reedição da Instrução sobre Divulgação de Informações Meteorológicas. O CHEFE DO SUBDEPARTAMENTO DE OPERAÇÕES DO DEPARTAMENTO DE CONTROLE DO ESPAÇO AÉREO, no uso das atribuições que lhe confere o Artigo 1°, inciso IV, da Portaria DECEA n°136-T/DGCEA, de 28 de novembro de 2005, RESOLVE: Art. 1o Aprovar a reedição da ICA 105-1 “Divulgação de Informações Meteorológicas”, que com esta baixa. Art. 2o Esta Instrução entra em vigor em 1º de setembro de 2006. Art. 3o Revoga-se a Portaria DECEA nº 131/SDOP, de 1º de julho de 2003, publicada no Boletim Interno do DECEA nº 124, de 08 de julho de 2003. (a) Brig Ar RICARDO DA SILVA SERVAN Chefe do Subdepartamento de Operações do DECEA (Publicada no BCA nº 146, de 07 de agosto de 2006) MINISTÉRIO DA DEFESA COMANDO DA AERONÁUTICA DEPARTAMENTO DE CONTROLE DO ESPAÇO AÉREO PORTARIA DECEA N° 33 /SDOP, DE 13 DE SETEMBRO DE 2007. Aprova a edição da emenda à Instrução sobre Divulgação de Informações Meteorológicas. O CHEFE DO SUBDEPARTAMENTO DE OPERAÇÕES DO DEPARTAMENTO DE CONTROLE DO ESPAÇO AÉREO, no uso das atribuições que lhe confere o Artigo 1°, alínea g, da Portaria DECEA n°34-T/DGCEA, de 15 de março de 2007, RESOLVE: Art. -
Sinuous Ridges in Chukhung Crater, Tempe Terra, Mars: Implications for Fluvial, Glacial, and Glaciofluvial Activity
This is a repository copy of Sinuous ridges in Chukhung crater, Tempe Terra, Mars: Implications for fluvial, glacial, and glaciofluvial activity. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/166644/ Version: Published Version Article: Butcher, F.E.G. orcid.org/0000-0002-5392-7286, Balme, M.R., Conway, S.J. et al. (6 more authors) (2021) Sinuous ridges in Chukhung crater, Tempe Terra, Mars: Implications for fluvial, glacial, and glaciofluvial activity. Icarus, 357. 114131. ISSN 0019-1035 https://doi.org/10.1016/j.icarus.2020.114131 Reuse This article is distributed under the terms of the Creative Commons Attribution (CC BY) licence. This licence allows you to distribute, remix, tweak, and build upon the work, even commercially, as long as you credit the authors for the original work. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ Journal Pre-proof Sinuous ridges in Chukhung crater, Tempe Terra, Mars: Implications for fluvial, glacial, and glaciofluvial activity Frances E.G. Butcher, Matthew R. Balme, Susan J. Conway, Colman Gallagher, Neil S. Arnold, Robert D. Storrar, Stephen R. Lewis, Axel Hagermann, Joel M. Davis PII: S0019-1035(20)30473-5 DOI: https://doi.org/10.1016/j.icarus.2020.114131 Reference: YICAR 114131 To appear in: Icarus Received date: 2 June 2020 Revised date: 19 August 2020 Accepted date: 28 September 2020 Please cite this article as: F.E.G. -
FFA-Cup-2019 Competition-Guide
1 FFA Cup 2019 Competition Guide CONTENTS Page Information, fixtures, results 2 Clubs 5 History and records 25 FFA CUP Web: www.theffacup.com.au Facebook: facebook.com/ffacup Twitter: @FFACup The FFA Cup is a national knockout competition run by Football Federation Australia (FFA) in conjunction with the State and Territory Member Federations. A total of 737 clubs entered the FFA Cup 2019, a number that has significantly grown from the first edition of the FFA Cup in 2014, when 617 clubs entered. The FFA Cup 2019 started in February with the Preliminary Rounds to determine the 21 clubs from the semi-professional and amateur tiers. These clubs joined ten of the Hyundai A-League clubs (Western United FC will not participate in this edition) and the reigning National Premier Leagues Champions (Campbelltown City SC) in the Final Rounds. The FFA Cup Final 2019 will be played on Wednesday 23 October with the host city to be determined by a live draw. Each cup tie must be decided on the day, with extra time to decide results of matches drawn after 90 minutes, followed by penalties if required. At least one Member Federation club is guaranteed to progress to the Semi Finals. Previous winners of the FFA Cup are Adelaide United (2014 and 2018), Melbourne Victory (2015), Melbourne City FC (2016) and Sydney FC (2017). Broadcast partners – FOX SPORTS FOX SPORTS will again provide comprehensive coverage of the FFA Cup 2019 Final Rounds. The FFA Cup’s official broadcaster will show one LIVE match per match night from the Round of 32 onwards, while providing coverage and updates, as well as live streams, of non-broadcast matches. -
Bibliographyof Space Books Andarticlesfrom Non
https://ntrs.nasa.gov/search.jsp?R=19800016707N 2020-03-11T18:02:45+00:00Zi_sB--rM-._lO&-{/£ 3 1176 00167 6031 HHR-51 NASA-TM-81068 ]9800016707 BibliographyOf Space Books And ArticlesFrom Non-AerospaceJournals 1957-1977 _'C>_.Ft_iEFERENC_ I0_,'-i p,,.,,gvi ,:,.2, , t ,£}J L,_:,._._ •..... , , .2 ,IFER History Office ...;_.o.v,. ._,.,- NASA Headquarters Washington, DC 20546 1979 i HHR-51 BIBLIOGRAPHYOF SPACEBOOKS AND ARTICLES FROM NON-AEROSPACE JOURNALS 1957-1977 John J. Looney History Office NASA Headquarters Washlngton 9 DC 20546 . 1979 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 033-000-0078t-1 Kc6o<2_o00 CONTENTS Introduction.................................................... v I. Space Activity A. General ..................................................... i B. Peaceful Uses ............................................... 9 C. Military Uses ............................................... Ii 2. Spaceflight: Earliest Times to Creation of NASA ................ 19 3. Organlzation_ Admlnlstration 9 and Management of NASA ............ 30 4. Aeronautics..................................................... 36 5. BoostersandRockets............................................ 38 6. Technology of Spaceflight....................................... 45 7. Manned Spaceflight.............................................. 77 8. Space Science A. Disciplines Other than Space Medicine ....................... 96 B. Space Medicine ..............................................119 C. -
Using Oxygen and Carbon Stable Isotopes, 53Mn-53Cr Isotope Systematics, and Petrology to Constrain the History of Carbonates
University of New Mexico UNM Digital Repository Earth and Planetary Sciences ETDs Electronic Theses and Dissertations 7-10-2013 Using oxygen and carbon stable isotopes, 53Mn-53Cr isotope systematics, and petrology to constrain the history of carbonates and water in the CR and CM chondrite parent bodies Mark Tyra Follow this and additional works at: https://digitalrepository.unm.edu/eps_etds Recommended Citation Tyra, Mark. "Using oxygen and carbon stable isotopes, 53Mn-53Cr isotope systematics, and petrology to constrain the history of carbonates and water in the CR and CM chondrite parent bodies." (2013). https://digitalrepository.unm.edu/eps_etds/93 This Dissertation is brought to you for free and open access by the Electronic Theses and Dissertations at UNM Digital Repository. It has been accepted for inclusion in Earth and Planetary Sciences ETDs by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. Mark Anthony Tyra Candidate Earth and Planetary Sciences Department This dissertation is approved, and it is acceptable in quality and form for publication: Approved by the Dissertation Committee: Adrian J. Brearley , Chairperson Ian D. Hutcheon Rhian H. Jones Zachary D. Sharp Charles K. Shearer i USING OXYGEN AND CARBON STABLE ISOTOPES, 53MN-53CR ISOTOPE SYSTEMATICS, AND PETROLOGY TO CONSTRAIN THE HISTORY OF CARBONATES AND WATER IN THE CR AND CM CHONDRITE PARENT BODIES by MARK ANTHONY TYRA B.S., Geology, University of Kentucky, 2000 M.S., Geology, University of Maryland, 2005 DISSERTATION Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in Earth and Planetary Sciences The University of New Mexico Albuquerque, New Mexico May, 2013 ii DEDICATION Education, on the other hand, means emancipation. -
Player Release Analysis CONTENTS
Player Release Analysis CONTENTS INTRODUCTION 04 KEY FACTS & FIGURES 08 CONFEDERATION ANALYSIS 12 CLUB ANALYSIS 18 APPENDIX 22 03 INTRODUCTION INTRODUCTION The AFC Asian Cup Australia 2015TM Player Release Analysis is a research study undertaken by the Research & Support Services unit from Competition Division on the AFC Asian Cup Australia 2015TM. The purpose of this particular research is to highlight the number and origin of clubs involved in releasing players for the AFC Asian Cup Australia 2015TM. *This analysis was generated at the time of player registration. 06 AFC Asian Cup Australia 2015TM - Player Release Analysis 07 KEY FACTS & FIGURES CLUBS INVOLVED IN RELEASING PLAYERS KEY FACTS & FIGURES OVERVIEW All players from China PR, Qatar, Saudi TOTAL Arabia and UAE are registered with their local clubs. Al Shorta (IRQ) has the biggest number of players released by a club (10 players) Asian 315 of players out of 367 were released from While the smallest number of European Asian Clubs players of an MA are registered with its MA League (Korea Rep. -6) 1. FSV Mainz 05 released 3 players of 2 dierent North American nationalities (1 JPN, 2 KOR) African 10 AFC Asian Cup Australia 2015TM - Player Release Analysis CONFEDERATION ANALYSIS CONFEDERATION CLUBS REPRESENTATION OVERVIEW NUMBER OF PLAYERS 315 players 48 players 2 players 1player 117 41 2 1 clubs clubs clubs club The national teams COMPETING in the AFC Asian Cup Australia 2015TM 15 CONFEDERATION REPRESENTATION % OVERVIEW 13.08 (48 players) EUROPEAN 7 36 PLAYERS registered in the Asian Cup 2015 Australia % 0.55 (2 players) NORTH % AMERICAN 85.83 (315 players) ASIAN % 0.27(1 player) AFRICAN 16 AFC Asian Cup Australia 2015TM - Player Release Analysis 17 CLUB ANALYSIS MOST REPRESENTED CLUBS EUROPEAN OVERVIEW Clubs No. -
Magnetite Plaquettes Are Naturally Asymmetric Materials in Meteorites
1 (Revision 2) 2 Magnetite plaquettes are naturally asymmetric materials in meteorites 3 Queenie H. S. Chan1, Michael E. Zolensky1, James E. Martinez2, Akira Tsuchiyama3, and Akira 4 Miyake3 5 1ARES, NASA Johnson Space Center, Houston, Texas 77058, USA. 6 2Jacobs Engineering, Houston, Texas 77058, USA. 7 3Graduate School of Science, Kyoto University, Kitashirakawa Oiwake-cho, Sakyo-ku, Kyoto 8 606-8502, Japan. 9 10 Correspondence to: Queenie H. S. Chan. Correspondence and requests for materials should be 11 addressed to Q.H.S.C. (Email: [email protected]) 12 13 Abstract 14 Life on Earth shows preference towards the set of organics with particular spatial configurations. 15 Enantiomeric excesses have been observed for α-methyl amino acids in meteorites, which 16 suggests that chiral asymmetry might have an abiotic origin. A possible abiotic mechanism that 17 could produce chiral asymmetry in meteoritic amino acids is their formation under the influence 18 of asymmetric catalysts, as mineral crystallization can produce spatially asymmetric structures. 19 Although magnetite plaquettes have been proposed to be a possible candidate for an asymmetric 20 catalyst, based on the suggestion that they have a spiral structure, a comprehensive description of 21 their morphology and interpretation of the mechanism associated with symmetry-breaking in 22 biomolecules remain elusive. Here we report observations of magnetite plaquettes in 1 23 carbonaceous chondrites (CCs) which were made with scanning electron microscopy and 24 synchrotron X-ray computed microtomography (SXRCT). We obtained the crystal orientation of 25 the plaquettes using electron backscatter diffraction (EBSD) analysis. SXRCT permits 26 visualization of the internal features of the plaquettes. -
Massachusetts Inst. of Thch.) 666 P HC A9NATIF A0L AEOA, CSCD 03F Unclas
lo2 to the " NATIONAL AERONAUTICS AND SPACE ADMINISTRATION Contract NAS9-12334 -APOLLOPASSIVE SEISMICEXPERIMENT PARTICIPATION 'I NASA-CR-151882) LUNAR SEISMOLOGY: THE 1479-17782 INTERNAL STRUCTURE ORHE LOt Ph. Thesis (Massachusetts Inst. of Thch.) 666 p HC A9NATIF A0L AEOA, CSCD 03f Unclas 1 Januarya-19-12 -o 3.0 September .1978 G3/91' 1351 0 M. Nafi Toksbz- Principal Investigator Department of Earth and Planetar SciencesO Massachusetts Institute of Technology Cambridge, Massachusetts 02139 LUNAR SEISMOLOGY: THE INTERNAL STRUCTURE OF THE MOON by -Neal Rodney Goins Submitted to the Department of-Earth -and Planetary Sciences on May 24,.1978, in parti&l .flfillment of the requirements for the degree of Doctor of Philosophy.. ABSTRACT, A primary goal of-the Apollo missions was the exploration and scientific study of the moon. The nature of the lunar interior is of particular interest for comparison with the earth and in studying comparative planetology. The principal experiment designed to study the lunar interior was the passive seismic experiment (PSE) included as part of the science package on missions 12, 14, 15, and 16. Thus seis mologists were provided with a uniqueopportunity ta study the seismicity and seismic characteristics of a second planetary 'bdy and ascertain if analysis methods developed on earth could illuminate the structure of the lunar interior. The lunar seismic data differ from terrestrial data in three major respects. First, the seismic sources are much smaller than on earth, so that no significant information has -been yet obtained for the 4v/ry deep lunar interior. Second, a strong, high Q scattering layer exists on the surface of the moon, resulting in very emergent seismic arrivals, long ringing-codas that obscure secondary (later arriving)-phases., and 'the-destruction of coherent dispersed surface wave trains. -
DETAILED GEOMORPHOLOGIC-TECTONIC MAPPING of the TEMPE TERRA REGION, MARS UNDER CONSIDERATION of CHRONOSTRATIGRAPHIC ASPECTS A. Neesemann1, S
45th Lunar and Planetary Science Conference (2014) 2313.pdf DETAILED GEOMORPHOLOGIC-TECTONIC MAPPING OF THE TEMPE TERRA REGION, MARS UNDER CONSIDERATION OF CHRONOSTRATIGRAPHIC ASPECTS A. Neesemann1, S. van Gasselt1, S. Walter1, 1Inst. of Geological Sciences, Freie Universitaet Berlin, Planetary Sciences and Remote Sensing Group, Dep. of Earth Sciences, Malteserstr. 74-100, 12249 Berlin, (Germany); [email protected]; Introduction: We have completed a new fice of 3.51 Ga which is highly consistent with own age 1:3,000,000 geomorphologic-tectonic map of Tempe determinations of 3.53 Ga. However, our detailed in- Terra along with parts of sorrounding units based on vestigation of the volcano using CTX data reveals new -1 Context Camera [1] (CTX) image data at ˜6 mpx insights into relative and absolute stratigraphic relations resolution. CTX data gaps that only make out a few between volcanic emplacement and rifting. Narrow lava percent of the mapping area were filled with data flows (Fig.1a) which represent later eruptions and acquired by the High Resolution Stereo Camera [2, 3] should therefore be younger than 3.53 Ga (or 3.51 Ga) (HRSC) at resolutions between 12.5 to 25 mpx-1. While are cut by major curvlinear border faults of Tempe Fos- the focus of this map lies on the study of recent surface sae and linear, narrow faults of Mareotis Fossae. Thus, processes and the complex volcano-tectonic history rifting or at least faulting seems to have been active after that has sustainably shaped Tempe Terra, adjacent the latest eruptions. units associated with the formation of major geologic Ancient lakes and river beds: In the eastern part regions (Arcadia Planitia, Kasei Valles, Tharsis) were of Tempe Terra, Nochian cratered units are often carved also included to get a comprehensive insight in the by irregular, often labyrinth-like, flat-floored and rim- regional geology.