Martian volatiles in shergottite EETA 79001 - New evidence from oxidized sulfur and sulfur-rich aluminosilicates
Two equivalent chips of lithology A (lith-A) and lithology C (lith-C) taken from the same interior portion of EETA 79001 shergottite have been analyzed for volatile species produced by high-vacuum pyrolysis. The lith-C was found to contain an oxidized sulfur component that does not occur in lith-A....
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1986
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ftnasantrs:oai:casi.ntrs.nasa.gov:19860063605 2023-05-15T13:49:36+02:00 Martian volatiles in shergottite EETA 79001 - New evidence from oxidized sulfur and sulfur-rich aluminosilicates Gooding, J. L. Muenow, D. W. Unclassified, Unlimited, Publicly available Jun 1, 1986 http://ntrs.nasa.gov/search.jsp?R=19860063605 unknown http://ntrs.nasa.gov/search.jsp?R=19860063605 Accession ID: 86A48343 Copyright Other Sources 91 Geochimica et Cosmochimica Acta; 50; 1049-105 1986 ftnasantrs 2012-02-15T16:51:20Z Two equivalent chips of lithology A (lith-A) and lithology C (lith-C) taken from the same interior portion of EETA 79001 shergottite have been analyzed for volatile species produced by high-vacuum pyrolysis. The lith-C was found to contain an oxidized sulfur component that does not occur in lith-A. The preterrestrial origin of this component in lith-C is supported by the occurrence in lith-C of sulfur- and chlorine-rich aluminosilicates that are not the same as Antarctic weathering products found in the control samples. The oxidation state and distribution of sulfur found in lith-C are consistent with the interpretation of EETA 79001 as a rock from Mars. Other/Unknown Material Antarc* Antarctic NASA Technical Reports Server (NTRS) Antarctic |
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NASA Technical Reports Server (NTRS) |
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91 |
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91 Gooding, J. L. Muenow, D. W. Martian volatiles in shergottite EETA 79001 - New evidence from oxidized sulfur and sulfur-rich aluminosilicates |
topic_facet |
91 |
description |
Two equivalent chips of lithology A (lith-A) and lithology C (lith-C) taken from the same interior portion of EETA 79001 shergottite have been analyzed for volatile species produced by high-vacuum pyrolysis. The lith-C was found to contain an oxidized sulfur component that does not occur in lith-A. The preterrestrial origin of this component in lith-C is supported by the occurrence in lith-C of sulfur- and chlorine-rich aluminosilicates that are not the same as Antarctic weathering products found in the control samples. The oxidation state and distribution of sulfur found in lith-C are consistent with the interpretation of EETA 79001 as a rock from Mars. |
format |
Other/Unknown Material |
author |
Gooding, J. L. Muenow, D. W. |
author_facet |
Gooding, J. L. Muenow, D. W. |
author_sort |
Gooding, J. L. |
title |
Martian volatiles in shergottite EETA 79001 - New evidence from oxidized sulfur and sulfur-rich aluminosilicates |
title_short |
Martian volatiles in shergottite EETA 79001 - New evidence from oxidized sulfur and sulfur-rich aluminosilicates |
title_full |
Martian volatiles in shergottite EETA 79001 - New evidence from oxidized sulfur and sulfur-rich aluminosilicates |
title_fullStr |
Martian volatiles in shergottite EETA 79001 - New evidence from oxidized sulfur and sulfur-rich aluminosilicates |
title_full_unstemmed |
Martian volatiles in shergottite EETA 79001 - New evidence from oxidized sulfur and sulfur-rich aluminosilicates |
title_sort |
martian volatiles in shergottite eeta 79001 - new evidence from oxidized sulfur and sulfur-rich aluminosilicates |
publishDate |
1986 |
url |
http://ntrs.nasa.gov/search.jsp?R=19860063605 |
op_coverage |
Unclassified, Unlimited, Publicly available |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Other Sources |
op_relation |
http://ntrs.nasa.gov/search.jsp?R=19860063605 Accession ID: 86A48343 |
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Copyright |
_version_ |
1766251850249535488 |