Cosmogenic Mn-53 in meteorites

The distributions of the Mn-53 contents in 106 nonantarctic and 112 antarctic chondrites were analyzed. A correlation analysis of these distributions showed that the correlation coefficient is a maximum r sub max = 0.75 plus or minus 0.03) when the histogram for antarctic chondrites is displaced by...

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Main Authors: Lavrukhina, A. K., Alexeev, V. A.
Format: Other/Unknown Material
Language:unknown
Published: 1985
Subjects:
Online Access:http://hdl.handle.net/2060/19850026794
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spelling ftnasantrs:oai:casi.ntrs.nasa.gov:19850026794 2023-05-15T13:58:36+02:00 Cosmogenic Mn-53 in meteorites Lavrukhina, A. K. Alexeev, V. A. Unclassified, Unlimited, Publicly available Aug 1, 1985 application/pdf http://hdl.handle.net/2060/19850026794 unknown Document ID: 19850026794 Accession ID: 85N35107 http://hdl.handle.net/2060/19850026794 No Copyright CASI SPACE RADIATION SH-7.1-17 19th Intern. Cosmic Ray Conf - Vol. 5; p 418-421; NASA-CP-2376-VOL-5 1985 ftnasantrs 2019-07-21T09:45:09Z The distributions of the Mn-53 contents in 106 nonantarctic and 112 antarctic chondrites were analyzed. A correlation analysis of these distributions showed that the correlation coefficient is a maximum r sub max = 0.75 plus or minus 0.03) when the histogram for antarctic chondrites is displaced by 40 plus or minus 8 dpm kg-1Fe towards lower Mn-53 contents. The distribution of Mn-53 saturated contents in nonantarctic ordinary chondrites was investigated as a function of their radiation age (T). It is found that the Mn-53 average content is higher by (21 plus or minus 9)% in H-chondrites with radiation age T approximately 12 Myr than in thse with T 12 Myr. This effect can be attributed to the fact that a considerable proportion of H-chondrites with T 12 Myr originates from a comet or from the objects of Chiron like, with the orbits more inclined to the ecliptic plane and/or more extended, which caused their irradiation by cosmic rays of higher intensity. Other/Unknown Material Antarc* Antarctic NASA Technical Reports Server (NTRS) Antarctic
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic SPACE RADIATION
spellingShingle SPACE RADIATION
Lavrukhina, A. K.
Alexeev, V. A.
Cosmogenic Mn-53 in meteorites
topic_facet SPACE RADIATION
description The distributions of the Mn-53 contents in 106 nonantarctic and 112 antarctic chondrites were analyzed. A correlation analysis of these distributions showed that the correlation coefficient is a maximum r sub max = 0.75 plus or minus 0.03) when the histogram for antarctic chondrites is displaced by 40 plus or minus 8 dpm kg-1Fe towards lower Mn-53 contents. The distribution of Mn-53 saturated contents in nonantarctic ordinary chondrites was investigated as a function of their radiation age (T). It is found that the Mn-53 average content is higher by (21 plus or minus 9)% in H-chondrites with radiation age T approximately 12 Myr than in thse with T 12 Myr. This effect can be attributed to the fact that a considerable proportion of H-chondrites with T 12 Myr originates from a comet or from the objects of Chiron like, with the orbits more inclined to the ecliptic plane and/or more extended, which caused their irradiation by cosmic rays of higher intensity.
format Other/Unknown Material
author Lavrukhina, A. K.
Alexeev, V. A.
author_facet Lavrukhina, A. K.
Alexeev, V. A.
author_sort Lavrukhina, A. K.
title Cosmogenic Mn-53 in meteorites
title_short Cosmogenic Mn-53 in meteorites
title_full Cosmogenic Mn-53 in meteorites
title_fullStr Cosmogenic Mn-53 in meteorites
title_full_unstemmed Cosmogenic Mn-53 in meteorites
title_sort cosmogenic mn-53 in meteorites
publishDate 1985
url http://hdl.handle.net/2060/19850026794
op_coverage Unclassified, Unlimited, Publicly available
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source CASI
op_relation Document ID: 19850026794
Accession ID: 85N35107
http://hdl.handle.net/2060/19850026794
op_rights No Copyright
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