SEGJ Technical Conference


Estimation of deep ground S-wave velocity structure using the horizontal array earthquake records (No.2)


Abstract
An array measurement of earthquakes are conducted in the Wakasa bay area, for estimation deep groud S-wave velocity structure.Newly PS logging from surface to about 300m depth and microtremor array are carried out this time to improve the accuracy.And we estimate the deep ground S-wave velocity structure from surface to about 5km depth with these records.