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...
Main Authors: | , , , , |
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Language: | English |
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National Institute of Polar Research
1990
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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 |