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安徽大别山造山带出露的大面积超高压(UHP)变质带是陆—陆碰撞造山作用的直接产物,成为窥视大陆造山带深部地质的窗口和认识超高压变质岩形成、折返的场所。随着地表地质研究的深入和榴辉岩中柯石英与金刚石包体的确认,研究重点逐渐转移到大别造山带的
The UHP metamorphic belt exposed by the Dabie orogen in Anhui Province is a direct product of the continental-continental collision orogeny and becomes a window to peep into the deep geology of the continental orogenic belt and to recognize the formation and reenforcement of UHP metamorphic rocks. With the in-depth study of surface geology and the confirmation of coesite and diamond inclusions in eclogites, the research focus gradually shifted to the Dabie orogenic belt