GEOCHEMISTRY OF POST-OROGENIC MAFIC DIKE ROCKS FROM THE EASTERN QUEEN MAUD LAND, EAST ANTARCTICA
P(論文) Two types of mafic dike rocks intruded the late Proterozoic metamorphic terrains of eastern Queen Maud Land : thermally metamorphosed rocks and unmetamorphosed rocks. The former is metamorphosed by ca. 500Ma granite intrusions, whereas the latter is Jurassic in age. The metadike rocks are cont...
Main Authors: | , , , , , |
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Language: | English |
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National Institute of Polar Research
1988
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Online Access: | https://nipr.repo.nii.ac.jp/record/2567/files/KJ00002368157.pdf https://doi.org/10.15094/00002567 https://nipr.repo.nii.ac.jp/records/2567 |