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

Date

Authors

Aikman, Amos

Harrison, T.M.

Hermann, Joerg

Publisher

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.

Keywords

Keywords: emplacement; Eocene; granitoid; igneous intrusion; leucogranite; magmatism; metasediment; neodymium isotope; partial melting; pluton; strontium isotope; trace element; zircon; China; Himalayas; Xizang Himalaya; Magmatism; Water-saturated melting; Zircon

URI

http://hdl.handle.net/1885/66630

Collections

ANU Research Publications

Source

Journal of Asian Earth Sciences

Type

Journal article

DOI

10.1016/j.jseaes.2012.05.018

Restricted until

2037-12-31

Downloads

File

Description

01_Aikman_The_origin_of_Eo-_and_2012.pdf (1.39 MB)

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