Adakitic Rocks Resulting from Partial Melting of Metabasite at High-Pressure Granulite-Facies Condition during Continental Collision.

The article focuses on findings of a study on adakitic rocks resulting from partial melting of metabasite at high-pressure granulite-facies condition during continental collision. Topics include analysis of high-pressure (HP) granulites and related anatectic adakitic rocks in the North Qaidam Mountains; ultrahigh-pressure metamorphic terrane, which comprises mafic HP granulite; and derivation of adakitic rocks from partial melting of newly emplaced metagabbro.