Comparisons of the NGA ground-motion relations

• Published in: Earthquake spectra 2008-02, Vol.24 (1), p.45-66
• Main Authors: Abrahamson, Norman A, Atkinson, Gail M, Boore, David M, Bozorgnia, Yousef, Campbell, Kenneth, Chiou, Brian, Idriss, I. M, Silva, Walter, Youngs, Robert
• Format: Article
• Language: English
• Subjects: acceleration; aftershocks; attenuation; bedrock; body waves; crust; data bases; data processing; depth; earthquakes; elastic waves; faults; ground motion; hanging wall; long-period waves; magnitude; NGA Project; normal faults; numerical models; peak ground acceleration; peak ground velocity; reverse faults; rupture; S-waves; scale factor; sediments; seismic waves; Seismology; shallow-focus earthquakes; soils; spectra; spectral analysis; strike-slip faults; velocity
• ISSN: 8755-2930; 1944-8201
• DOI: 10.1193/1.2924363

The data sets, model parameterizations, and results from the five NGA models for shallow crustal earthquakes in active tectonic regions are compared. A key difference in the data sets is the inclusion or exclusion of aftershocks. A comparison of the median spectral values for strike-slip earthquakes shows that they are within a factor of 1.5 for magnitudes between 6.0 and 7.0 for distances less than 100 km. The differences increase to a factor of 2 for M5 and M8 earthquakes, for buried ruptures, and for distances greater than 100 km. For soil sites, the differences in the modeling of soil/sediment depth effects increase the range in the median long-period spectral values for M7 strike-slip earthquakes to a factor of 3. The five models have similar standard deviations for M6.5-M7.5 earthquakes for rock sites and for soil sites at distances greater than 50 km. Differences in the standard deviations of up to 0.2 natural log units for moderate magnitudes at all distances and for large magnitudes at short distances result from the treatment of the magnitude dependence and the effects of nonlinear site response on the standard deviation.