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...
Main Authors: | , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Polar Research Institute of China - PRIC
2009
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Subjects: | |
Online Access: | http://library.arcticportal.org/2367/ http://library.arcticportal.org/2367/1/A0090101.pdf |