Rb-Sr and Sm-Nd mineral isochron ages of a pegmatitic gneiss from Oku-iwa Rock, Lutzow-Holm Complex, East Antarctica

Oku-iwa Rock is located in the transitional zone between granulite- and amphibolite-facies metamorphic zones in the Lutzow-Holm Complex (LHC), East Antarctica. Hornblende biotite (HB) gneiss widely outcrops in the northern part of this area. Sm-Nd and Rb-Sr mineral isochron ages obtained from pegmat...

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Bibliographic Details
Main Authors: Yoshinobu Kawano, Naoko Nishi, Hiroo Kagami
Format: Report
Language:English
Published: Center for Research and Development of Higher Education, Saga University 2006
Subjects:
Rb-Sr and Sm-Nd geochronology
hornblende biotite gneiss
Oku-iwa 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=3166
http://id.nii.ac.jp/1291/00003166/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3166&item_no=1&attribute_id=18&file_no=1

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