GEOCHEMISTRY OF POST-OROGENIC MAFIC DIKE ROCKS FROM THE EASTERN QUEEN MAUD LAND, EAST ANTARCTICA
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 continenta...
Main Authors: | , , , , , |
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Format: | Report |
Language: | English |
Published: |
National Institute of Polar Research
1988
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Subjects: | |
Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2567 http://id.nii.ac.jp/1291/00002567/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2567&item_no=1&attribute_id=18&file_no=1 |