The protoliths to the sillimanite gneisses from the Larsemann Hills and geological implication in their formation

The source rock from which the sillimanite gneisses derive mainly was the biotite plagioclase gneiss in the Larsemann Hills. It is the deformation-metamorphism process under special pressure and temperature condition, not the original rock compositions, that controls the presence of sillimanite. To...

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Bibliographic Details
Main Authors: Liudong, Ren, Chonghui, Yang, Yanbin, Wang, Ping, Liu, Yue, Zhao
Format: Article in Journal/Newspaper
Language:English
Published: Polar Research Institute of China - PRIC 2009
Subjects:
Online Access:http://library.arcticportal.org/2367/
http://library.arcticportal.org/2367/1/A0090101.pdf