AbstractSince the discovery of high‐pressure metamorphic minerals such as coesite and diamond (Xu et al., 1992), the exhumation mode and process of the Dabie ultrahigh‐high pressure (UHP) rocks had become hot topics. For the exhumation process of UHP rocks, several explanation models had been proposed, and the subduction tunnel mode (Warren et al., 2008) seemed to be recognized by most scholars. A low rheological zone formed along the subduction, and the deep subduction material was rapidly exhumated by buoyancy or tectonic stress. In the tunnel, the exhuming rock moved at the opposite direction of the subduction. Following this model, the Dabie UHP rock exhumation structure would generally tend to NW, and show a top to SE shear sense (Fig 1a, b). However, the existing structural observations indicate that the UHP rocks tend to be S‐SE with the top to NW shear sense (Faure et al., 2003). Therefore, the more detailly analysis of the exhumation structure in the UHP rocks, especially in the exhuming shear zone is very necessary.