Peak temperatures of ultra-high temperature metamorphism of the Napier Complex, Enderby Land, East Antarctica, as deduced from porphyroclastic pyroxenes of meta-ultramafic rocks
P(論文) In the Mt. Riiser-Larsen area of the Archaean Napier Complex, an ultra-high temperature (UHT) metamorphic complex, Enderby Land, East Antarctica, meta-ultramafic rocks occur as blocks and pods embedded in orthopyroxene felsic gneiss or garnet felsic gneiss and as thin layers intercalated with...
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Language: | English |
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National Institute of Polar Research
2002
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Online Access: | https://nipr.repo.nii.ac.jp/record/3105/files/KJ00000044223.pdf https://doi.org/10.15094/00003105 https://nipr.repo.nii.ac.jp/records/3105 |