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

Clemens JD ; Finger F (2012)



Please help us populate SUNScholar with the post print version of this article. It can be e-mailed to:

Journal Articles (subsidised)

Please refer to this item in SUNScholar by using the following persistent URL:
This item appears in the following collections: