Retrograde metamorphism in the Yamato Mountains, East Antarctica

P(論文) Retrograde metamorphism which affected the granulite-facies garnetbiotite gneiss and calc-silicate gneiss from Massif A in the Yamato Mountains was petrographically revealed. In the garnet-biotite gneiss, the association of ferruginous matrix biotite (Type I biotite) and magnesian interior of...

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Bibliographic Details
Main Authors: Asami, Masao, Shiraishi, Kazuyuki
Language:English
Published: 1985
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/1790/files/KJ00000012422.pdf
https://nipr.repo.nii.ac.jp/records/1790