The origin of Eo- and Neo-himalayan granitoids, Eastern Tibet
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Aikman, Amos
Harrison, T.M.
Hermann, Joerg
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Pergamon-Elsevier Ltd
Abstract
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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Journal of Asian Earth Sciences
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2037-12-31
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