Electronic Supplement to
Assessment of Ground-Motion Models for Use in the British Columbia North Coast Region, Canada

by Trevor I. Allen and Camille Brillon

Table S1. Summary of the Candidate Ground-Motion Prediction Equations (GMPEs) for Active Crustal Regions, Indicating Their Distance Metrics and Conditions of Use

Ground-Motion Model Magnitude Range Distance Range (km) Period Range Site Condition Reference Style of Faulting Flags Ground-Motion Metric Region
Boore et al. (1997) 5.2 ≤ MW ≤ 7.7 0 ≤ RJB ≤ 100 PGA, SA(0.1–2.0 s) VS30 SS, RS RC Western United States
Zhao et al. (2006) 5.0 ≤ MW ≤ 7.3* 0 ≤ Rrup ≤ 300 PGA, SA(0.05–5.0 s) NEHRP RS GM Japan
Campbell and Bozorgnia (2008) 4.0 ≤ MW ≤ 7.9 0 ≤ Rrup ≤ 200 PGA, PGV, PGD, SA(0.01–10 s) VS30 RS, NS GMRotI50 Western United States, global
Chiou and Youngs (2008) 4.0 ≤ MW ≤ 8.5 0 ≤ Rrup ≤ 200 PGA, PGV, SA(0.01–10 s) VS30 RS, NS GMRotI50 Western United States, global
Bindi et al. (2011) 4.0 ≤ MW ≤ 6.9 0 ≤ RJB ≤ 200 PGA, PGV, SA(0.04–2.0 s) EC8 SS, RS, NS, U GM Italy
Atkinson and Boore (2011) 4.0 ≤ MW ≤ 8.0 0 ≤ RJB ≤ 200 PGA, PGV, SA(0.01–10 s) VS30 SS, RS, NS, U GMRotI50§ Western United States, global
Atkinson and Adams (2013) 4.5 ≤ MW ≤ 9.0 0 ≤ RJB ≤ 600# PGA, PGV, SA(0.05–10 s) VS30 (760 m/s) - GMRotI50 Western North America
Akkar et al. (2014) 4.0 ≤ MW ≤ 7.9 0 ≤ Repi; Rhyp; RJB ≤ 200 PGA, PGV, SA(0.01–4.0 s) VS30 RS, NS GM Europe, Middle East
Boore et al. (2014) 3.0 ≤ MW ≤ 8.5 0 ≤ RJB ≤ 400 PGA, PGV, SA(0.01–10 s) VS30 SS, RS, NS, U RotD50 Global
Chiou and Youngs (2014) 3.5 ≤ MW ≤ 8.5** 0 ≤ Rrup ≤ 300 PGA, PGV, SA(0.01–10 s) VS30 RS, NS RotD50†† Global

Table is based on information summarized in Allen and Wald (2009) and Douglas et al. (2013) and on original sources. Abbreviations: MW, moment magnitude; Repi, epicentral distance; Rhyp, hypocentral distance; Rrup, distance to rupture; RJB, Joyner-Boore distance; PGA, peak ground acceleration; PGV, peak ground velocity; PGD, peak ground displacement; SA, spectral acceleration; VS30, time-averaged shear-wave velocity in the upper 30 m of the crust; NEHRP, National Earthquake Hazard Reduction Program site class (Building Seismic Safety Council, 2004); EC8, Eurocode 8 (European Committee for Standardization, 2003); RS, reverse-slip; SS, strike-slip; NS, normal-slip; U, unknown slip; RC, random component; GM, geometric mean of the horizontal components; GMRotI50, 50th percentile orientation-independent geometric mean using period-independent rotation angle (Boore et al., 2006); RotD50, 50th percentile of orientation-independent, non-geometric-mean ground motions (Boore, 2010).

* Inferred from Figure 1 in Zhao et al. (2006).

MW 8.5 for strike-slip events and MW 8.0 for reverse-slip events.

‡ Updated from Boore and Atkinson (2008).

§ Small-magnitude scaling is based on the geometric mean of the horizontal components (GM).

‖ From tables available at Western University’s Engineering Seismology Toolbox (see Data and Resources).

# Approximated from tables available at Western University’s Engineering Seismology Toolbox (see Data and Resources).

** MW 8.5 for strike-slip events and MW 8.0 for reverse- and normal-slip events.

†† Not explicitly stated. Assumed based on Ancheta et al. (2014).

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