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Abstract
We present a framework to evaluate the inclusion of candidate basin depth models in the U.S. Geological Survey National Seismic Hazard Model. We compute intensity measures (peak and spectral amplitudes) from uniformly processed earthquake ground motions in and around the basin of interest and compare these to ground-motion model (GMM) estimates over a range of oscillator periods. The GMMs use depth to specific shear-wave velocity isosurfaces (Zx) as a proxy for basin depth. We quantify whether the GMM estimates using Zx from the candidate basin depth model outperform the default estimates based on VS30 (the time-averaged shear wave velocity in the upper 30 m). We partition GMM residuals into event and site terms and compare site terms for stations within the basin to non-basin sites. We apply this framework to the greater Reno, Nevada, region, which has shallow basin depths (less than 450 m) and empirical amplifications of up to a factor of 2.2 at 1.0 s. There are no strong trends in site terms with basin depth, and the use of Zx values from the new candidate basin model shows marginal improvement of GMM total residuals compared to the default VS30-based model (the condition of no relative basin amplification).
Study Area
Publication type | Conference Paper |
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Publication Subtype | Conference Paper |
Title | Implementation of basin models and sediment depth terms in the 2023 update of the U.S. National Seismic Hazard Model: Example from Reno, Nevada |
Year Published | 2022 |
Language | English |
Publisher | Earthquake Engineering Research Institute |
Contributing office(s) | Geologic Hazards Science Center |
Description | 5 p. |
Larger Work Type | Book |
Larger Work Subtype | Conference publication |
Larger Work Title | Proceedings from the 12th national conference on earthquake engineering |
Conference Title | 12th National Conference on Earthquake Engineering |
Conference Location | Salt Lake City, UT |
Conference Date | Jun 27 - Jul 1, 2022 |
Country | United States |
State | Nevada |
City | Reno |
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