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We conducted a seismic reflection survey along the coast line of the eastern part of the Kanto Plain, central Japan. Four reflectors were clearly recognized in the reflection profile: Reflector A is nearly flat (about 0.1-0.25 s in 2-way time); Reflector B is gently tilted to the south at about 0.25-0.5 s; Reflector C is waved around the 0.5-1.0 s at the northern and southern parts of the profile; Reflector D is hugely waved deeper than 1.5 s. With respect to borehole data adjacent to the seismic line, the strata between Reflectors C and D can be correlated with the early middle Miocene half-graben deposits distributed along the Tanagura Tectonic Line. It suggests that the southern trace of the Tanagura Tectonic Line should be concealed at just east of the present seismic line.

jishin. dai1shuu/jishin/jishin. dai2shuu

Seismic Reflection Survey Using Vibroseis at Taiyo Village, Ibaraki Prefecture, Central Honshu, Japan, and Its Implication of the Southern Trace of the Tanagura Tectonic Line