Intellectual Merit
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The intellectual merit of this TAG lies in coordinating the development, verification and validation of a robust family of computational tools that advance the capabilities of SCEC ground motion simulation platforms to capture nonlinear effects that manifest in the shallow crust. By shallow crust, we refer to the upper 300--600 m of local and regional basins, where the crustal structure is predominantly composed of sedimentary soil deposits with typical shear wave velocities less than 1 km/s. On the temporal scale, our activities focus on localized transient phenomena occurring during, or as a consequence of, strong earthquake ground motions. On the spatial scale, we study how these effects affect far- and near-field ground motions, excluding the off-fault damaged rock zones. |
Broader Impacts
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Within SCEC5, this TAG is complementary to research activities carried out in earthquake geology (focused on much deeper structures), fault and rupture mechanics (where nonlinearities are related to rupture dynamics), stress evolution and geodynamic modeling (focused on much longer time scales), and in developing the Community Rheology Model (focused on larger and deeper geologic scales). The TAG facilitates research initiatives at the intersection of seismology, ground motion, and computational science; supports the CXM initiative contributing to the characterization of small scale heterogeneities, sedimentary velocity structures, and shallow geomaterial rheology; and promotes the activities of the Earthquake Engineering Implementation Interface Focus Group by coordinating the development of products intended for the engineering community, such as site modules of the Broadband Platform (BBP) and semi-empirical site factors. |