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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Bibliographic Details
Main Author: Akai, Junji
Language:English
Published: National Institute of Polar Research 1990
Subjects:
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