Fig. 2From: Identification of active faults and tectonic features through heat flow distribution in the Nankai Trough, Japan, based on high-resolution velocity-estimated bottom-simulating reflector depthsThe flowchart of seismic data processing conducted in this study. Automated velocity analysis was applied on CMP sorted gathers after preprocessing (Nakamura et al. 2022) and additional signal enhancement. Final reflection profile was obtained through depth conversion of the post-stack time migration based on the high-density velocity modelBack to article page