摘要：We estimate Q s values (quality factor for S-wave) of the slab near the southern Kurile trench by using seismic data observed at ocean bottom seismometer (OBS) stations from selected local earthquakes. The seismic rays pass mainly through the slab and this enable us to directly estimate the slab Q s values. The spectral inversion and coda normalization method are applied to these data. The estimated Q s values from the two methods are nearly the same and increase with frequencies. However, these Q s values are not high enough to explain the abnormal distribution of ground motion that has been recognized as abnormal distribution of seismic intensities at the Japanese arc. Thus we propose a two-layer Q s structure of the slab to explain the both facts, our slab Q s values and the abnormal distribution of ground motion. The two-layer Q s structure consists of the upper layer with not so high Q s values (39 f 1.0 ) and lower layer with very high Q s values (500 f 1.0 ); the upper layer has a thickness of about 50 km. Seismic activity is restricted only within the upper layer of the two-layer Q s structure. This may mean that the two-layer Q s structure reflects the different material property between the upper and lower layer of the slab.
关键词：Two-layer Q s structure of the slab ;Spectral inversion method ;Coda normalization method ;Abnormal distribution of seismic intensities
