Restoration of the Western Himalaya: implications for metamorphic protoliths, thrust and normal faulting, and channel flow models
The Greater Himalayan Sequence (GHS) is composed of a sequence of Barrovian facies metamorphic rocks up to kyanite or sillimanite+K-feldspar grade, migmatites, layered stromatic migmatites and leucogranite sheets. These rocks were metamorphosed during the late Eocene to early Miocene, and are bounde...
| Main Authors: | , , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
2007
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