“…The hazard deaggregation is used to guide the selection of ground motion records, which are subsequently scaled to represent the target design spectrum. The selection and scaling of ground motions is a broad and currently debated topic, however, based on the recommendations of ASCE 7-05 (2006), those of Bommer and Acevedo (2004) and similarly done in Haselton's Group I (2009), it was decided that the selected ground motion records should conform to the following criteria: - Strong motions records should be compatible with the tectonic regime anticipated at the site and of similar anticipated source mechanisms (i.e., strike-slip, reverse, or normal).
- Magnitude-distance ( M , R ) pairs of the selected records should be compatible with results of the deaggregation analysis from the probabilistic seismic hazard for the site of interest. With regard to magnitude selection, records were sought with magnitudes within 0.2 units of the target magnitude, as the dependency on seismological characteristics and its site-specific record selection is not as critical when undertaking nonlinear analysis (Iervolino and Cornell, 2005),
- The selected ground motion records should be compatible with the soil characteristics of the site of interest (namely site class C, with a shear wave velocity in the upper 30 m ranging from 360 m/s to 760 m/s).
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