Early Cretaceous intrusive rocks in the Gangdese arc of southern Tibet do not support shallow subduction of the Neo-Tethyan oceanic lithosphere-Reference-Cited by-同舟云学术

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Early Cretaceous intrusive rocks in the Gangdese arc of southern Tibet do not support shallow subduction of the Neo-Tethyan oceanic lithosphere

Published:2024-05 Issue: Volume:472-473 Page:107551
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Wang Feng,Wang Qing,Zhu Di-Cheng,Li Shi-Min,Cawood Peter A.,Wang Rui-Qiang,Yi Jian-Kang,Zhang Liang-Liang,Xie Jin-Cheng

Funder

Fundamental Research Funds for the Central Universities

Australian Research Council

National Natural Science Foundation of China

Higher Education Discipline Innovation Project

Publisher

Elsevier BV

Reference77 articles.

1. Igneous garnet and amphibole fractionation in the roots of island arcs: experimental constraints on andesitic liquids;Alonso-Perez;Contrib. Mineral. Petrol.,2009

2. Xigaze forearc basin revisited (South Tibet): Provenance changes and origin of the Xigaze Ophiolite;An;GSA Bull.,2014

3. Theory of the Earth;Anderson,1989

4. Temperature-induced Al-zoning in hornblendes of the fish Canyon magma, Colorado;Bachmann;Am. Mineral.,2002

5. The formation of high-Sr/Y plutons in cordilleran-arc crust by crystal accumulation and melt loss;Brackman;Geosphere,2022

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