Re-checking Spatial Auto Correlation method based on the theory of seismic interferometry

The applicability of the seismic interferometry was examined for the purpose of establishing a method for investigating the two-dimensional S wave velocity structure. Microtremor records were obtained for 14 hours and 22 hours at two sites with different vibration levels, respectively. The main findings obtained are as follows.1. S-wave velocity structures at depths of 20 m or more can be explored, which is difficult to do with existing surface wave surveys.2. Phase velocity can be detected in about one hour of measurement by arranging a large number of receiving points in a straight line.

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Review of Seismic Interferometry

Shiraishi¹,

Matsuoka²,

Kawanaka³

2008

J. Geogr.

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Re-checking Spatial Auto Correlation method based on the theory of seismic interferometry

Cited by 4 publications

References 13 publications

Three-dimensional microtremor array measurement with irregular receiver geometries in town and residential area

Three-dimensional microtremor array measurement with irregular receiver geometries in town and residential area

Applicability of Seismic Interferometry to Microtremor Records for Two Dimensional S-Wave Velocity Structure Survey

Review of Seismic Interferometry

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