Terrestrial Ages of Antarctic Meteorites Based on the Thermoluminescence Levels Induced in the Fusion Crust
The fusion crust of eight Antarctic meteorite finds show natural thermoluminescence (TL) levels about 100 times higher than the levels in the fusion crust of freshly fallen meteorites, Dhajala, Jilin and Bansur. If it is assumed that this TL is due to cosmic ray received on the surface of Antarctica...
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Sociedade Brasileira de Física
1997
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ftjscielo:oai:scielo:S0103-97331997000300001 2023-05-15T14:03:03+02:00 Terrestrial Ages of Antarctic Meteorites Based on the Thermoluminescence Levels Induced in the Fusion Crust Sengupta,D. Bhandari,N. Watanabe,S. 1997-09-01 text/html http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0103-97331997000300001 en eng Sociedade Brasileira de Física Brazilian Journal of Physics v.27 n.3 1997 journal article 1997 ftjscielo 2015-10-26T21:21:09Z The fusion crust of eight Antarctic meteorite finds show natural thermoluminescence (TL) levels about 100 times higher than the levels in the fusion crust of freshly fallen meteorites, Dhajala, Jilin and Bansur. If it is assumed that this TL is due to cosmic ray received on the surface of Antarctica, the terrestrial residence times of the meteorites is calculated to lie between 104 - 105 years. Strictly, these periods represent lower limits of terrestrial ages of these meteorites, and are generally consistent with terrestrial ages calculated from cosmogenic radionuclides Article in Journal/Newspaper Antarc* Antarctic Antarctica SciELO Brazil (Scientific Electronic Library Online) Antarctic |
institution |
Open Polar |
collection |
SciELO Brazil (Scientific Electronic Library Online) |
op_collection_id |
ftjscielo |
language |
English |
description |
The fusion crust of eight Antarctic meteorite finds show natural thermoluminescence (TL) levels about 100 times higher than the levels in the fusion crust of freshly fallen meteorites, Dhajala, Jilin and Bansur. If it is assumed that this TL is due to cosmic ray received on the surface of Antarctica, the terrestrial residence times of the meteorites is calculated to lie between 104 - 105 years. Strictly, these periods represent lower limits of terrestrial ages of these meteorites, and are generally consistent with terrestrial ages calculated from cosmogenic radionuclides |
format |
Article in Journal/Newspaper |
author |
Sengupta,D. Bhandari,N. Watanabe,S. |
spellingShingle |
Sengupta,D. Bhandari,N. Watanabe,S. Terrestrial Ages of Antarctic Meteorites Based on the Thermoluminescence Levels Induced in the Fusion Crust |
author_facet |
Sengupta,D. Bhandari,N. Watanabe,S. |
author_sort |
Sengupta,D. |
title |
Terrestrial Ages of Antarctic Meteorites Based on the Thermoluminescence Levels Induced in the Fusion Crust |
title_short |
Terrestrial Ages of Antarctic Meteorites Based on the Thermoluminescence Levels Induced in the Fusion Crust |
title_full |
Terrestrial Ages of Antarctic Meteorites Based on the Thermoluminescence Levels Induced in the Fusion Crust |
title_fullStr |
Terrestrial Ages of Antarctic Meteorites Based on the Thermoluminescence Levels Induced in the Fusion Crust |
title_full_unstemmed |
Terrestrial Ages of Antarctic Meteorites Based on the Thermoluminescence Levels Induced in the Fusion Crust |
title_sort |
terrestrial ages of antarctic meteorites based on the thermoluminescence levels induced in the fusion crust |
publisher |
Sociedade Brasileira de Física |
publishDate |
1997 |
url |
http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0103-97331997000300001 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Antarctica |
genre_facet |
Antarc* Antarctic Antarctica |
op_source |
Brazilian Journal of Physics v.27 n.3 1997 |
_version_ |
1766273546965745664 |