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...
| Main Authors: | , , , |
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| Format: | Journal Article |
| Published: |
Geological Society of America
2011
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/41790 |