Fig. 3From: Seismic reflection imaging of deep crustal structures using local earthquakes in the Kanto region, JapanSeismic reflection profile obtained by passive seismic reflection imaging with local earthquakes. a Final RTM section using 200 high-quality events and b final section overlaid with the P-wave velocity (Matsubara et al. 2019) used for RTM-based imaging. The red and blue arrows denote the eastward- and westward-dipping reflectors, respectively. The yellow arrows denote reflections with en-échelon pattern reflectorsBack to article page