Restoration of the Western Himalaya： implications for metamorphic protoliths, thrust and normal faulting, and channel flow models
Restoration of the Western Himalaya： implications for metamorphic protoliths, thrust and normal faulting, and channel flow models
摘要
The Greater Himalayan Sequence （GHS） is composed of a sequence of Barrovianfacies 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 bounded below by a large-scale SW-vergent ductile shear zone-thrust fault （Main Central Thrust; MCT）, and above by a NE-dipping low-angle normal sense shear zone and fault （Zanskar Shear Zone; ZSZ）,
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