GIG OpenIR

A fair use statement regarding the full text of the request

Your requested [Low-δ18O A-type granites in SW China: Evidence for the interaction between the subducted Paleotethyan slab and the Emeishan mantle plume] is currently limited to Guangzhou Institute of Geochemistry,Chinese Academy of Sciences internal sharing.


To solicit author authorization, you need to provide the following information: name, organization, personal e-mail, reason for request. The information you provide will be reviewed and you are committed to the truth of the information provided. The personal information you provide will be protected according to law.

Low-δ18O A-type granites in SW China: Evidence for the interaction between the subducted Paleotethyan slab and the Emeishan mantle plume
Refresh

You agree and are willing to abide by the above requirements.