Rapid forearc spreading between 130 and 120Ma: Evidence from geochronology and geochemistry of the Xigaze ophiolite, southern Tibet-Reference-Cited by-同舟云学术

Rapid forearc spreading between 130 and 120Ma: Evidence from geochronology and geochemistry of the Xigaze ophiolite, southern Tibet

Published:2013-07 Issue: Volume:172-173 Page:1-16
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Dai Jingen,Wang Chengshan,Polat Ali,Santosh M.,Li Yalin,Ge Yukui

Funder

National Basic Research Program of China

111 Project of China Grant

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference117 articles.

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3. Structure and evolution of the Himalaya–Tibet orogenic belt;Allègre;Nature,1984

4. Correction of common lead in U–Pb analyses that do not report 204Pb;Andersen;Chemical Geology,2002

5. Petrology and geochemistry of the Saga and Sangsang ophiolitic massifs, Yarlung Zangbo Suture Zone, Southern Tibet: evidence for an arc–back-arc origin;Bédard;Lithos,2009

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