META-ULTRAMAFIC ROCK FROM THE AUSTKAMPANE AREA OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA

P(論文) In the Austkampane area of the S∅r Rondane Mountains, East Antarctica, a meta-ultramafic rock occurs as a lenticular block enclosed within the host garnet-biotite gneiss of the granulite facies. The rock consists of olivine, orthopyroxene, amphibole, spinel, apatite, ilmenite, magnetite, chalc...

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Bibliographic Details
Main Authors: イシズカ, ヒデオ, スズキ, サトコ, コジマ, ヒデヤス, ISHIZUKA, Hideo, SUZUKI, Satoko, KOJIMA, Hideyasu
Language:English
Published: National Institute of Polar Research 1996
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/2822/files/KJ00002409869.pdf
https://doi.org/10.15094/00002822
https://nipr.repo.nii.ac.jp/records/2822