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Generalized Inversion Method has been used to estimate the spatial variation of site effects,using the digital data of SH-waves recorded by 63 stations in the Capital Circle Region of China from 2001 to 2006.We gained the site effects of all stations participating in the calculation.We found that the site effect of rock was stabile and about 1.0 from 1.0Hz to 10.0Hz,while the site effect of deposit was high in low frequencies,about 3 ～ 7 from 1.0Hz to 8.0Hz,and the site effect was protuberant at about 5.0Hz,then fell as the frequency increased.The result shows the shape and intensity of station site effects are mainly influenced by the lithology below the station,and possibly also by the local geological structure.
Generalized Inversion Method has been used to estimate the spatial variation of site effects, using the digital data of SH-waves recorded by 63 stations in the Capital Circle Region of China from 2001 to 2006.We gained the site effects of all stations participating in the calculation. We found that the site effect of rock was stabile and about 1.0 from 1.0Hz to 10.0Hz, while the site effect of deposit was high in low frequencies, about 3 ~ 7 from 1.0Hz to 8.0Hz, and the site effect was protuberant at about 5.0Hz, then fell as the frequency increased. The result shows the shape and intensity of station site effects are primarily influenced by the lithology below the station, and possibly also by the local geological structure.