Partial melting of thickened lower crust in post‐collisional setting: Evidence from high silicon adakitic granites in the North Qilian orogen
Abstract
During orogenic extension, partial melting of the continental crust usually produces post-collisional granitoids, and the characteristics of their petrogenesis can provide crucial constraints on the geodynamics of tectonic regimes and post-collisional lithospheric processes. A case study for this issue is the high-silicon adakitic granites from the Jingtieshan area, North Qilian orogenic belt. In this study, we present a range of evidences on...
Paper Details
Title
Partial melting of thickened lower crust in post‐collisional setting: Evidence from high silicon adakitic granites in the North Qilian orogen
Published Date
Sep 8, 2019
Journal
Volume
55
Issue
5
Pages
3990 - 4007
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