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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...
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