Fig. 6From: Possible fluid discharge associated with faults observed by a high-resolution dense-2D seismic reflection survey in Uchiura Bay off Numazu, Japana EWF observed on the raw field data of line 10. b The rms amplitude of each trace of the raw field data of line 10 is displayed. A relatively high rms amplitude can be seen along the zone of the EWF. c EWF observed on the shot records of line 10. A similar EWF can be observed as that on the raw field data. d NMO velocities estimated on line 10. Dip correction has been conducted by using Levin (1971) equationBack to article page