High-grade metamorphic rocks from Christmas Point in the Napier Complex, East Antarctica
The Christmas Point area is dominated by well-layered gneisses, of which garnet-orthopyroxene gneiss and garnet felsic gneiss are the most abundant types. Orthopyroxene-bearing quartz-rich granulite, layering of which is indistinct to massive, is present as layers within the garnet felsic gneiss. Ga...
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Bibliographic Details
Main Authors: |
Yasutaka Yoshimura,
Tomoharu Miyamoto,
Edward S. Grew,
Christopher J. Carson,
Daniel J. Dunkley,
Yoichi Motoyoshi |
Format: | Report
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Language: | English |
Published: |
Department of Natural Environmental Science, Kochi University/Department of Earth and Planetary Science, Kyushu University/Department of Geological Science, University of Maine/Department of Geology and Geophysics, Kline Geology Laboratory, Yale University/School of Geosciences, Edgeworth David Building, University of Sydney/National Institute of Polar Research
2001
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Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3085
http://id.nii.ac.jp/1291/00003085/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3085&item_no=1&attribute_id=18&file_no=1
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