The origin of Eo- and Neo-himalayan granitoids, Eastern Tibet
Two distinctive modes of post-collisional magmatism are evident along a transect through the eastern Himalaya at ca. 92°E. The first comprises Eocene igneous complexes emplaced into the central Tethyan Himalaya Series (THS) (Dala granitoids, 44.1. ±. 1.
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|Source:||Journal of Asian Earth Sciences|
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