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The illustration of the depth variation of long-period Love wave amplitude in Figure 5b might be suggestive of the weak physical effect of the bedrock on the excitation of long-period Love waves.
Although there is a large scatter of data, this observation implies that the physical effect of the bedrock on long-period ground motions is sufficiently strong to be observable in the shallow part of the basin, but it becomes very weak where the depth of the bedrock exceeds about 2 km. Figure 3 Comparison between the predominant period of long-period horizontal ground motion and bedrock depth.
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We compare linear and equivalent-linear site response predictions for a soil layer of varying thickness over bedrock, and assess the effects of varying the bedrock shear-wave velocity (VSb) and quality factor (Q).
Finally, we investigate the effect of a bedrock geometry on a steady-state position of the grounding line.
The effect of bedrock depth and soil parameters on strong ground motion distribution has been observed.
This study generated new insight into the effect of bedrock grain sizes on pedogenesis under identical topographic and climatic environment.
We present a numerical simulation of cosmogenic nuclide production and distribution in landslide-dominated catchments to address the effect of bedrock landsliding on erosion rates.
We also assess the effect of bedrock depth on soil amplification for a generic soil profile in artificial fill, using both linear and equivalent-linear site response models.
Based on drill core logging, the bedrock of Olkiluoto consists mainly of gneiss (9% of the bedrock volume), migmatitic gneiss (64% of the bedrock volume), TGG (tonalite-granodiorite-granite) gneiss (8%), and pegmatitic granite (19%) [ 19].
His thoughts form a useful map of the bedrock.
The depth of the bedrock is at about twenty meters.
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