Identification of the youngest meteorites and a discussion of the possibility that they came from Mars

The shergottites are a group of basaltic meteorites which are very similar in appearance to terrestrial basalts. On the Earth basalts are formed by volcanic activity. Because the shergottites so resemble terrestrial basalts and because they are apparently very young ( 1.3 billion years), it has been...

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Main Author: Jones, J. H.
Format: Other/Unknown Material
Language:unknown
Published: 1985
Subjects:
Online Access:http://hdl.handle.net/2060/19850018248
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spelling ftnasantrs:oai:casi.ntrs.nasa.gov:19850018248 2023-05-15T13:53:27+02:00 Identification of the youngest meteorites and a discussion of the possibility that they came from Mars Jones, J. H. Unclassified, Unlimited, Publicly available JAN 1, 1985 application/pdf http://hdl.handle.net/2060/19850018248 unknown Document ID: 19850018248 Accession ID: 85N26559 http://hdl.handle.net/2060/19850018248 No Copyright CASI LUNAR AND PLANETARY EXPLORATION Lunar and Planetary Inst. 16th Lunar and Planetary Sci. Conf.; p 38-41 1985 ftnasantrs 2016-06-11T22:53:13Z The shergottites are a group of basaltic meteorites which are very similar in appearance to terrestrial basalts. On the Earth basalts are formed by volcanic activity. Because the shergottites so resemble terrestrial basalts and because they are apparently very young ( 1.3 billion years), it has been inferred that they come from a large planet. Small planets and asteroids lose heat from their interiors quickly and stop producing hot basaltic liquids early in their history. It appears that gases trapped in one shergotite found in Antarctica (BETA 79001) are chemically similar to the martian atmosphere (as measured by the Viking mission). The controversial speculation that the shergotites are samples of mars is examined in detail. Other/Unknown Material Antarc* Antarctica NASA Technical Reports Server (NTRS)
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic LUNAR AND PLANETARY EXPLORATION
spellingShingle LUNAR AND PLANETARY EXPLORATION
Jones, J. H.
Identification of the youngest meteorites and a discussion of the possibility that they came from Mars
topic_facet LUNAR AND PLANETARY EXPLORATION
description The shergottites are a group of basaltic meteorites which are very similar in appearance to terrestrial basalts. On the Earth basalts are formed by volcanic activity. Because the shergottites so resemble terrestrial basalts and because they are apparently very young ( 1.3 billion years), it has been inferred that they come from a large planet. Small planets and asteroids lose heat from their interiors quickly and stop producing hot basaltic liquids early in their history. It appears that gases trapped in one shergotite found in Antarctica (BETA 79001) are chemically similar to the martian atmosphere (as measured by the Viking mission). The controversial speculation that the shergotites are samples of mars is examined in detail.
format Other/Unknown Material
author Jones, J. H.
author_facet Jones, J. H.
author_sort Jones, J. H.
title Identification of the youngest meteorites and a discussion of the possibility that they came from Mars
title_short Identification of the youngest meteorites and a discussion of the possibility that they came from Mars
title_full Identification of the youngest meteorites and a discussion of the possibility that they came from Mars
title_fullStr Identification of the youngest meteorites and a discussion of the possibility that they came from Mars
title_full_unstemmed Identification of the youngest meteorites and a discussion of the possibility that they came from Mars
title_sort identification of the youngest meteorites and a discussion of the possibility that they came from mars
publishDate 1985
url http://hdl.handle.net/2060/19850018248
op_coverage Unclassified, Unlimited, Publicly available
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source CASI
op_relation Document ID: 19850018248
Accession ID: 85N26559
http://hdl.handle.net/2060/19850018248
op_rights No Copyright
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