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

P(論文) 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...

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Bibliographic Details
Main Authors: Kawano, Yoshinobu, Nishi, Naoko, Kagami, Hiroo
Language:English
Published: National Institute of Polar Research 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/record/3166/files/KJ00004346779.pdf
https://doi.org/10.15094/00003166
https://nipr.repo.nii.ac.jp/records/3166

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