Retrograde metamorphism in the Yamato Mountains, East Antarctica

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 zoned...

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Bibliographic Details
Main Authors: Masao Asami, Kazuyuki Shiraishi
Format: Report
Language:English
Published: Department of Geological Sciences, College of Liberal Arts, Okayama University/National Institute of Polar Research 1985
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1790
http://id.nii.ac.jp/1291/00001790/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1790&item_no=1&attribute_id=18&file_no=1