LOW-PRESSURE GRANULITE-FACIES METAMORPHISM IN THE PRYDZ BAY REGION, EAST ANTARCTICA

P(論文) The terrain along the coastal line of Prydz Bay is underlain by granulite-facies rocks of various kinds including pelitic to psammitic gneisses, basic to intermediate gneisses and subordinate amounts of calc-silicate rocks and ultramafic rocks. Extensive partial melting has been observed in pe...

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Bibliographic Details
Main Authors: モトヨシ, ヨウイチ, /, MOTOYOSHI, Yoichi, THOST, D.E., HENSEN, B.J.
Language:English
Published: National Institute of Polar Research 1990
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/2644/files/KJ00002368256.pdf
https://doi.org/10.15094/00002644
https://nipr.repo.nii.ac.jp/records/2644