Geochronological study of post-metamorphic granite from Kasumi Rock, Lutzow-Holm Complex, East Antarctica

Kasumi Rock is situated in the amphibolite-facies metamorphic zone in the Lutzow-Holm Complex, East Antarctica. In this area, granitic rocks occur as steeply dipping linear dykes with sharp intrusive contacts, and cross-cut the foliation of layered metamorphic rocks. A geochronological study of this...

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Bibliographic Details
Main Authors: Ajishi,Hideaki, Kawano,Yoshinobu, Kawakami,Tetsuo, Ikeda,Takeshi
Format: Report
Language:English
Published: Graduate School of Education, Saga University/Faculty of Culture and Education, Saga University/Faculty of Education, Okayama University/Department of Earth and Planetary Sciences, Graduate School of Science, Kyushu University 2004
Subjects:
Rb-Sr whole rock isochron
Sm-Nd whole rock isochron
post-metamorphic granite
Kasumi Rock
Lutzow-Holm Complex
East Antarctica
Oku-iwa
Antarc*
Antarctica
Polar geoscience
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3135
http://id.nii.ac.jp/1291/00003135/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3135&item_no=1&attribute_id=18&file_no=1

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