Summary of the ASK14 Ground Motion Relation for Active Crustal Regions
Norman A. Abrahamson,a)
M.EERI, Walter J. Silva,
M.EERI,
and Ronnie Kamai,c)
M.EERI
Empirical ground motion models for the average horizontal component from
shallow crustal earthquakes in active tectonic regions are derived using the PEER
NGA-West2 database. The model is applicable to magnitudes 3.0–8.5, distances
0–300 km, and spectral periods of 0–10 s. The model input parameters are the
same as those used by Abrahamson and Silva (2008), with the following exceptions:
the loading level for nonlinear effects is based on the spectral acceleration
at the period of interest rather than the PGA; and the distance scaling for hanging
wall (HW) effects off the ends of the rupture includes a dependence on the sourceto-
site azimuth. Regional differences in large-distance attenuation and VS30 scaling
between California, Japan, China, and Taiwan are included. The scaling for
the HW effect is improved using constraints from numerical simulations. The
standard deviation is magnitude-dependent, with smaller magnitudes leading
to larger standard deviations at short periods, but smaller standard deviations
at long periods. Directivity effects are not included through explicit parameters,
but are captured through the variability of the empirical data. [DOI: 10.1193/
070913EQS198M]
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