Restoration of the Western Himalaya:implications for metamorphic protoliths,thrust and normal faulting,and channel flow models
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摘要:
The Greater Himalayan Sequence(GHS)is composed of a sequence of Barrovian facies metamorphic rocks up to kyanite or sillimanite+K-feldspar grade,migrmatites,layered stromatic migmatites and leucogranite sheets.