Fig. 7From: 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 depthsExtracted seismic profiles obtained by (a) pre-STM and (b) post-STM. (c) The difference in heat flow between (a) and (b). (d) The difference between BSR depth and seafloor depth in profiles obtained by pre-STM (black) and post-STM (red). Note the different vertical scales of (c) and (d). Yellow arrowheads in (a) and (b) represent the location of BSRs. The main factors for the uncertainty can be caused by the difference of the BSR depthsBack to article page