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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Language: | English |
Published: |
1985
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Online Access: | https://nipr.repo.nii.ac.jp/record/1790/files/KJ00000012422.pdf https://nipr.repo.nii.ac.jp/records/1790 |