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...
Main Authors: | , , |
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Language: | English |
Published: |
1979
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Subjects: | |
Online Access: | https://nipr.repo.nii.ac.jp/record/1031/files/KJ00000011575.pdf |