Knowledge Management System Of Guangzhou Institute of Geochemistry，CAS
Your requested [Anticlockwise P-T evolution at similar to 280 Ma recorded from ultrahigh-temperature metapelitic granulite in the Chinese Altai orogenic belt, a possible link With the Tarim 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.