Comparative study on the major element chemical compositions of Antarctic chondrites to those of non-Antarctic falls with reference to terrestrial weathering
Antarctic ordinary chondrites contain variable amounts of Fe_2O_3 and water as terrestrial weathering products. The Fe_2O_3 contents have a positive correlation with water contents, and a negative correlation with metallic Fe. Therefore, oxygen and water were added to Antarctic chondrites during wea...
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ftnipr:oai:nipr.repo.nii.ac.jp:00005896 2023-05-15T13:46:39+02:00 Comparative study on the major element chemical compositions of Antarctic chondrites to those of non-Antarctic falls with reference to terrestrial weathering Tetsuya Nobuyoshi Hiroshi Haramura Yukio Ikeda Makoto Kimura Hideyasu Kojima Naoya Imae Min Sung Lee 1997-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=5896 http://id.nii.ac.jp/1291/00005896/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=5896&item_no=1&attribute_id=18&file_no=1 en eng Department of Earth Sciences, Ibaraki University/Department of Meteorites, National Institute of Polar Research/Department of Earth Sciences, Ibaraki University/Department of Earth Sciences, Ibaraki University/Department of Meteorites, National Institute of Polar Research/Department of Meteorites, National Institute of Polar Research/Department of Earth Sciences, Seoul University National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=5896 http://id.nii.ac.jp/1291/00005896/ AA11182426 Antarctic meteorite research, 10, 165-180(1997-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=5896&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1997 ftnipr 2023-02-25T20:13:36Z Antarctic ordinary chondrites contain variable amounts of Fe_2O_3 and water as terrestrial weathering products. The Fe_2O_3 contents have a positive correlation with water contents, and a negative correlation with metallic Fe. Therefore, oxygen and water were added to Antarctic chondrites during weathering to form limonitic alteration from metallic iron. Other major elements and total Fe slightly decrease with increasing Fe_2O_3. This decrease is caused by the "dilution" effect due to additional water and oxygen, suggesting that most of the Antarctic chondrites seem to have undergone terrestrial weathering in a quasi-closed system insofar as major elements are concerned. Weathering index has minimal or no relation with the Fe_2O_3 contents of chondrites. Extensive weathering obscures petrographic features of some chondrites, leading to the misclassification, and they are revised on the basis of UC diagram. The major element compositions of Antarctic ordinary chondrites are the same as those of non-Antarctic falls, and they show slight difference in Mg and Na contents among H, L, and LL chondrites; H chondrites have the highest Mg/Si ratio and the lowest Na/Si ratio on average. Some LL chondrite breccias have higher K contents than non-brecciated LL chondrites. Report Antarc* Antarctic National Institute of Polar Research Repository, Japan Antarctic The Antarctic |
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Open Polar |
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National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
description |
Antarctic ordinary chondrites contain variable amounts of Fe_2O_3 and water as terrestrial weathering products. The Fe_2O_3 contents have a positive correlation with water contents, and a negative correlation with metallic Fe. Therefore, oxygen and water were added to Antarctic chondrites during weathering to form limonitic alteration from metallic iron. Other major elements and total Fe slightly decrease with increasing Fe_2O_3. This decrease is caused by the "dilution" effect due to additional water and oxygen, suggesting that most of the Antarctic chondrites seem to have undergone terrestrial weathering in a quasi-closed system insofar as major elements are concerned. Weathering index has minimal or no relation with the Fe_2O_3 contents of chondrites. Extensive weathering obscures petrographic features of some chondrites, leading to the misclassification, and they are revised on the basis of UC diagram. The major element compositions of Antarctic ordinary chondrites are the same as those of non-Antarctic falls, and they show slight difference in Mg and Na contents among H, L, and LL chondrites; H chondrites have the highest Mg/Si ratio and the lowest Na/Si ratio on average. Some LL chondrite breccias have higher K contents than non-brecciated LL chondrites. |
format |
Report |
author |
Tetsuya Nobuyoshi Hiroshi Haramura Yukio Ikeda Makoto Kimura Hideyasu Kojima Naoya Imae Min Sung Lee |
spellingShingle |
Tetsuya Nobuyoshi Hiroshi Haramura Yukio Ikeda Makoto Kimura Hideyasu Kojima Naoya Imae Min Sung Lee Comparative study on the major element chemical compositions of Antarctic chondrites to those of non-Antarctic falls with reference to terrestrial weathering |
author_facet |
Tetsuya Nobuyoshi Hiroshi Haramura Yukio Ikeda Makoto Kimura Hideyasu Kojima Naoya Imae Min Sung Lee |
author_sort |
Tetsuya Nobuyoshi |
title |
Comparative study on the major element chemical compositions of Antarctic chondrites to those of non-Antarctic falls with reference to terrestrial weathering |
title_short |
Comparative study on the major element chemical compositions of Antarctic chondrites to those of non-Antarctic falls with reference to terrestrial weathering |
title_full |
Comparative study on the major element chemical compositions of Antarctic chondrites to those of non-Antarctic falls with reference to terrestrial weathering |
title_fullStr |
Comparative study on the major element chemical compositions of Antarctic chondrites to those of non-Antarctic falls with reference to terrestrial weathering |
title_full_unstemmed |
Comparative study on the major element chemical compositions of Antarctic chondrites to those of non-Antarctic falls with reference to terrestrial weathering |
title_sort |
comparative study on the major element chemical compositions of antarctic chondrites to those of non-antarctic falls with reference to terrestrial weathering |
publisher |
Department of Earth Sciences, Ibaraki University/Department of Meteorites, National Institute of Polar Research/Department of Earth Sciences, Ibaraki University/Department of Earth Sciences, Ibaraki University/Department of Meteorites, National Institute of Polar Research/Department of Meteorites, National Institute of Polar Research/Department of Earth Sciences, Seoul University |
publishDate |
1997 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=5896 http://id.nii.ac.jp/1291/00005896/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=5896&item_no=1&attribute_id=18&file_no=1 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=5896 http://id.nii.ac.jp/1291/00005896/ AA11182426 Antarctic meteorite research, 10, 165-180(1997-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=5896&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766244986331856896 |