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In addition, the actual bedrock depth might be deeper than the present velocity structure model.
The effect of bedrock depth and soil parameters on strong ground motion distribution has been observed.
The spatial variation of bedrock depth is also shown in lower right part of (a).
The spatial variation of the bedrock depth is also shown in the lower right panel.
Figure 4 Relationship between bedrock depth and predominant period of long-period horizontal ground motion.
This study shows that GPR and MASW can provide complementary results in estimating bedrock depth.
Figure 4 shows the estimated PDF of predominant period as a function of the bedrock depth.
Their spatial patterns resembled the bedrock depth variation in the Osaka basin (Fig. 1).
To estimate the bedrock depth conclusively, MASW testing was performed at the same site.
The developed charts consider wall dimensions, granular soil properties, bedrock depth, and seismic input motion characteristics.
The 2-D ER method is capable in mapping karst features and bedrock depth.
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