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Published in 2022 at "Earthquake Spectra"
DOI: 10.1177/87552930221088609
Abstract: Ergodic site amplification models for active tectonic regions are conditioned on the time-averaged shear wave velocity in the upper 30 m (VS30) and the depth to a shear wave velocity isosurface (zx). The depth components of…
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Keywords:
site response;
depth;
amplification;
geomorphic provinces ... See more keywords