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

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 pelitic...

Full description

Bibliographic Details
Main Authors: モトヨシ ヨウイチ, Yoichi MOTOYOSHI, D.E. THOST, B.J. HENSEN
Format: Report
Language:English
Published: ABSTRACT 1990
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2644
http://id.nii.ac.jp/1291/00002644/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2644&item_no=1&attribute_id=18&file_no=1