Partial melting caused by subduction of young, hot oceanic crust in shallow high-temperature and low-pressure environments: Indications from Middle and Late Jurassic oceanic plagiogranite in Shiquanhe, Central Tibet-Reference-Cited by-同舟云学术

Partial melting caused by subduction of young, hot oceanic crust in shallow high-temperature and low-pressure environments: Indications from Middle and Late Jurassic oceanic plagiogranite in Shiquanhe, Central Tibet

Published:2022-07 Issue: Volume:420-421 Page:106698
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Hang Li,Ming Wang,Xiao-Wen Zeng,An-Bo Luo,Bo-Chuan Zhang,Di Shen

Funder

National Natural Science Foundation of China

China Postdoctoral Science Foundation

China Geological Survey

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference77 articles.

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4. Magma mixing and mingling textures in granitoids: examples from the Galway Granite, Connemara, Ireland;Baxter;Mineral. Petrol.,2002

5. Enclaves from the A-type granite of the Mégantic complex, White Mountain Magma Series: Clues to granite magmagenesis;Bédard;J. Geophys. Res. Solid Earth,1990

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