Formation of late Miocene silicic volcanic rocks in the central Tibetan Plateau by crustal anatexis of granulites

Author:

Ou Quan,Wang Qiang,Wyman Derek A.,Zhang Xiu-Zheng,Hao Lu-Lu,Zeng Ji-Peng,Yang Jin-Hui,Zhang Hai-Xiang,Hou Ming-Cai,Qi Yue,Liu Zhao

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference81 articles.

1. Mechanisms of crustal anatexis: a geochemical study of partially melted metapelitic enclaves and host dacite, SE Spain;Acosta–Vigil;J. Petrol.,2010

2. Chemical, petrological and mass balance constraints on the textural evolution of pelitic enclaves;Álvarez–Valero;Lithos,2010

3. Correction of common lead in U–Pb analyses that do not report 204Pb;Andersen;Chem. Geol.,2002

4. Peritectic assemblage entrainment as the main compositional driver in the I–type Vredenburg Granite, north–western Pan–African Saldania Belt, South Africa: a whole–rock chemical perspective;Bailie;Lithos,2020

5. Retrograde Processes in migmatites and granulites revisited;Brown;J. Metamorph. Geol.,2002

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