Petrology and Geothermometry of the Clinopyroxene-Garnet Rock from Cape Ryugu, East Antarctica

P(論文) In Cape Ryugu, the most abundant rocks are biotite gneiss, garnet-biotite gneiss and hornblende-biotite gneiss, none of which show any obvious indication of their more detail metamorphic condition from their mineral parageneses. Petrology of the clinopyroxene-garnet rock occurring as thin inte...

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Bibliographic Details
Main Authors: Yoshikura, Shin-ichi, Nakai, Yutaka, Kano, Takashi
Language:English
Published: 1979
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/1031/files/KJ00000011575.pdf