Chapter
Feb 22, 2024

Capturing the Path Dependency of Site Response in Basin and Non-Basin Southern California Locations

Publication: Geo-Congress 2024

ABSTRACT

The manifestation of ground shaking in sedimentary basins during an earthquake event depends on the energy released by the seismic source, the distance between the source and the basin in question, and the geologic characteristics of the basin. The combination of these components leads to amplification of ground shaking in basins relative to non-basin regions. Within sedimentary basins, spatial variability of ground shaking from location to location occurs due to the complexities associated with the interactions of seismic waves with the 3-dimensional characteristics of the subsurface and the variation of geologic material. This includes refraction which alters the propagation direction of seismic waves, diffraction which spreads and scatters the waves, reflection which can concentrate seismic energy, and their combinations which can generate propagating surface waves. The intensity of these basin-related site effects is drastically impacted by the path between the source and the site within basin (attenuation and basin boundary interactions). Both site effects and path effects are intertwined, and as such, the determination of site response in these geomorphic provinces requires proper understanding of their interactions in order to separate both effects. Using an expanded southern California ground motion dataset that comprises a subset of NGA-West2 plus recent event recordings, this study uses iterative mixed effects modelling scheme to propose a site-dependent path model for southern California. The site-dependent model attempts to partition path-site effects, and the regional model aims to release the ergodic assumption. It is expected that incorporating site dependence based on basin and non-basin features will show reduction in uncertainty in comparison to current in practice ergodic GMMs.

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