Structural and metamorphic evolution of the Karakoram and Pamir following India–Kohistan–Asia collision
Following the c. 50 Ma India–Kohistan arc–Asia collision, crustal thickening uplifted the Himalaya (Indian Plate), and the Karakoram, Pamir and Tibetan Plateau (Asian Plate). Whereas surface geology of Tibet shows limited Cenozoic metamorphism and deformation, and only localized crustal melting, the...
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| Format: | Journal article |
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Geologic Society of London
2018
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