对大别山造山带和合肥盆地的地质、地球物理、地球化学综合研究表明,大别山造山带是中生代碰撞造山作用的产物,合肥盆地是这一造山带隆起时开始形成的,经历了凹陷→断陷→构造反转3个阶段,造山带的“去根”过程与地慢上涌控制着大别山的隆起和合肥盆地的发育. A comprehensive study on the geology, geophysics and geochemistry of the Dabie orogenic belt and the Hefei basin shows that the Dabie orogen was the product of the Mesozoic collision orogeny. The Hefei Basin began to form during the uplift of this orogenic belt and experienced the depression → fault depression → Tectonic inversion of three stages, orogenic belt “to the root” process and the slow upwelling control of the uplift of the Dabie Mountains and the development of the Hefei Basin.