Formation of high δ18O fayalite-bearing A-type granite by high temperature melting of granulitic metasedimentary rocks, southern China

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Formation of high δ18O fayalite-bearing A-type granite by high temperature melting of granulitic metasedimentary rocks, southern China

The genesis of A-type granites has been controversial. Fayalite granite is a member of the most reduced A-type granites, commonly thought to have been primarily sourced from tholeiitic rocks. In this paper we report petrography, whole-rock geochemistry, Sr-Nd isotope, and in situ zircon Hf-O isotope...

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Bibliographic Details
Main Authors:	Huang, H., Li, X., Li, W., Li, Zheng-Xiang
Format:	Journal Article
Published:	Geological Society of America 2011
Subjects:	Jiuyishan A-type granite oxygen fugacity fractional crystallization Fayalite
Online Access:	http://hdl.handle.net/20.500.11937/41790

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