Paleotethyan subduction process revealed from Triassic blueschists in the Lancang tectonic belt of Southwest China-Reference-Cited by-同舟云学术

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Paleotethyan subduction process revealed from Triassic blueschists in the Lancang tectonic belt of Southwest China

Published:2015-11 Issue: Volume:662 Page:95-108
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Fan Weiming,Wang Yuejun,Zhang Yanhua,Zhang Yuzhi,Jourdan Fred,Zi Jianwei,Liu Huichuan

Funder

National Natural Science Foundation of China

National Basic Research Program of China

State Key Laboratory of Ore Deport Geochemistry, CAS

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference96 articles.

1. Late Cretaceous blueschist metamorphism in the Indus Suture Zone, Shangla region, Pakistan Himalaya;Anczkiewicz;Tectonophysics,2000

2. Initial water budget: the key to detaching large volumes of eclogitized oceanic crust along the subduction channel;Angiboust;Lithos,2010

3. Eclogitization of the Monviso ophiolite (W. Alps) and implications on subduction dynamics;Angiboust;J. Metamorph. Geol.,2012

4. Metamorphism of metasediments in the scale of an orogen: a key to the Tertiary geodynamic evolution of the Alps;Bousquet,2008

5. Comparison of the mineralogy and phase relations of blueschists from the North Cascades, Washington and greenschist from Otago, New Zealand;Brown;Bull. Geol. Soc. Am.,1974

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