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The origin of Eo- and Neo-himalayan granitoids, Eastern Tibet

Aikman, Amos; Harrison, T.M.; Hermann, Joerg


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.

CollectionsANU Research Publications
Date published: 2012
Type: Journal article
Source: Journal of Asian Earth Sciences
DOI: 10.1016/j.jseaes.2012.05.018


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