Mineralogy and petrology of Belgica-7904: A new kind of carbonaceous chondrite from Antarctica
A mineralogical and petrological study of Belgica-7904 (B-7904) shows that it can be classified into the CM group. B-7904 has a variety of chondrules and aggregates, where pyroxenes and mesostasis glass are completely replaced by phyllosilicates, but olivine remains little altered. It has a high abu...
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Mineralogical Institute, Faculty of Science, University of Tokyo
1990
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ftnipr:oai:nipr.repo.nii.ac.jp:00004508 2023-05-15T13:49:01+02:00 Mineralogy and petrology of Belgica-7904: A new kind of carbonaceous chondrite from Antarctica Kazushige Tomeoka 1990-10 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=4508 http://id.nii.ac.jp/1291/00004508/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4508&item_no=1&attribute_id=18&file_no=1 en eng Mineralogical Institute, Faculty of Science, University of Tokyo National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=4508 http://id.nii.ac.jp/1291/00004508/ AA10784627 Proceedings of the NIPR Symposium on Antarctic Meteorites, 3, 40-54(1990-10) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4508&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1990 ftnipr 2023-01-28T20:04:07Z A mineralogical and petrological study of Belgica-7904 (B-7904) shows that it can be classified into the CM group. B-7904 has a variety of chondrules and aggregates, where pyroxenes and mesostasis glass are completely replaced by phyllosilicates, but olivine remains little altered. It has a high abundance of troilite; most occur in submicron to micron grains dispersed in the matrix. Minor taenite occurs, but magnetite is rare and tochilinite is absent. The phyllosilicates have relatively high Na contents and lower (Mg+Fe)/(Si+Al) ratios than serpentine; thus, they may be intergrowths of serpentine and a smectite-like phyllosilicate. Microprobe analyses of the phyllosilicates show high analytical totals relative to ordinary phyllosilicates, being consistent with the idea that they were dehydrated by heating. The fine troilite grains in the matrix may have been transformed from a thermally labile phase such as tochilinite during thermal metamorphism. The opaque mineral assemblage suggests that the thermal metamorphism occurred in a reduced condition. B-7904 and Y-86720 are mineralogically similar, although the former is less affected by aqueous alteration than the latter. They were probably derived from similar precursors and experienced aqueous alteration and thermal metamorphism in a common environment. These meteorites and ordinary CM chondrites apparently experienced distinct alteration histories, suggesting that they came from different regions in a parent body or different parent bodies. Report Antarc* Antarctica National Institute of Polar Research Repository, Japan |
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National Institute of Polar Research Repository, Japan |
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ftnipr |
language |
English |
description |
A mineralogical and petrological study of Belgica-7904 (B-7904) shows that it can be classified into the CM group. B-7904 has a variety of chondrules and aggregates, where pyroxenes and mesostasis glass are completely replaced by phyllosilicates, but olivine remains little altered. It has a high abundance of troilite; most occur in submicron to micron grains dispersed in the matrix. Minor taenite occurs, but magnetite is rare and tochilinite is absent. The phyllosilicates have relatively high Na contents and lower (Mg+Fe)/(Si+Al) ratios than serpentine; thus, they may be intergrowths of serpentine and a smectite-like phyllosilicate. Microprobe analyses of the phyllosilicates show high analytical totals relative to ordinary phyllosilicates, being consistent with the idea that they were dehydrated by heating. The fine troilite grains in the matrix may have been transformed from a thermally labile phase such as tochilinite during thermal metamorphism. The opaque mineral assemblage suggests that the thermal metamorphism occurred in a reduced condition. B-7904 and Y-86720 are mineralogically similar, although the former is less affected by aqueous alteration than the latter. They were probably derived from similar precursors and experienced aqueous alteration and thermal metamorphism in a common environment. These meteorites and ordinary CM chondrites apparently experienced distinct alteration histories, suggesting that they came from different regions in a parent body or different parent bodies. |
format |
Report |
author |
Kazushige Tomeoka |
spellingShingle |
Kazushige Tomeoka Mineralogy and petrology of Belgica-7904: A new kind of carbonaceous chondrite from Antarctica |
author_facet |
Kazushige Tomeoka |
author_sort |
Kazushige Tomeoka |
title |
Mineralogy and petrology of Belgica-7904: A new kind of carbonaceous chondrite from Antarctica |
title_short |
Mineralogy and petrology of Belgica-7904: A new kind of carbonaceous chondrite from Antarctica |
title_full |
Mineralogy and petrology of Belgica-7904: A new kind of carbonaceous chondrite from Antarctica |
title_fullStr |
Mineralogy and petrology of Belgica-7904: A new kind of carbonaceous chondrite from Antarctica |
title_full_unstemmed |
Mineralogy and petrology of Belgica-7904: A new kind of carbonaceous chondrite from Antarctica |
title_sort |
mineralogy and petrology of belgica-7904: a new kind of carbonaceous chondrite from antarctica |
publisher |
Mineralogical Institute, Faculty of Science, University of Tokyo |
publishDate |
1990 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=4508 http://id.nii.ac.jp/1291/00004508/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4508&item_no=1&attribute_id=18&file_no=1 |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=4508 http://id.nii.ac.jp/1291/00004508/ AA10784627 Proceedings of the NIPR Symposium on Antarctic Meteorites, 3, 40-54(1990-10) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4508&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766250472348319744 |