Mineralogical evidence of heating events in Antarctic carbonaceous chondrites, Y-86720 and Y-82162
P(論文) Antarctic carbonaceous chondrites, Y-82162 and Y-86720 were examined by transmission electron microscopy. Matrix phyllosilicates in both meteorites are probably serpentine and saponite. There is evidence that these phyllosilicates were affected by thermal metamorphism. The serpentine was almos...
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Language: | English |
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National Institute of Polar Research
1990
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Online Access: | https://nipr.repo.nii.ac.jp/record/4509/files/KJ00000036315.pdf https://doi.org/10.15094/00004509 https://nipr.repo.nii.ac.jp/records/4509 |