Number | GMPE | Description | Distance | Mw Range |
Periods (T) s | R*Range | Year | Site Parameter* |
Grouping† | Comments‡ |
---|---|---|---|---|---|---|---|---|---|---|
1 | AB95 | Atkinson and Boore, 1995 | Closest distance from the recording site to the ruptured area | 3.5–8.0 | 0.03–5, +PGA, PGV | 10–100 | 1995 | Vs30 a parameter | Double corner frequency | |
2 | AB06 | Atkinson and Boore, 2006 | Closest distance from the recording site to the ruptured area | 3.5–8.0 | 0.03–5, +PGA, PGV | 1–1000 | 2006 | Vs30 a parameter | Current USGS NSHMP (2008) | 140 bar stress drop |
3 | AB06+ | Atkinson and Boore, 2006 | Closest distance from the recording site to the ruptured area | 3.5–8.0 | 0.03–5, +PGA, PGV | 1–1000 | 2006 | Vs30 a parameter | Current USGS NSHMP (2008) | 200 bar stress drop Atkinson and Boore (2006), a CEUS relation |
4 | AB06p | Atkinson and Boore, 2011 | Closest distance from the recording site to the ruptured area | 3.5–8.0 | 0.03–5, +PGA, PGV | 1–1000 | 2006 | Vs30 a parameter | Proposed USGS NSHMP (2014) | No 200 bar, only magnitude-dependent stress drop |
5 | A08 | Atkinson, 2008 | Joyner-Boore distance | 4.3–7.6 | 0.03–5, +PGA, PGV | 0–200 | 2008 | Vs30 a parameter | Current USGS NSHMP (2008) | Modified from getBooreNGA07m.f |
6 | A08p | Atkinson and Boore, 2011 | Joyner-Boore distance | 5.0–8.0 | 0.03–5, +PGA, PGV | 0–200 | 2009 | Vs30 a parameter | Modified from getAtk08ENA.f | |
7 | C03 | Campbell et al., 2003 | Closest distance from the recording site to the ruptured area | 5.0–8.2 | 0.01–4 | 0–1000 | 2003 | Vs30 = 2800 m/s | Current USGS NSHMP (2008) | Hybrid empirical model |
8 | F96 | Frankel et al., 1996 | Closest distance from the recording site to the ruptured area | 4.4–8.2 | 0.2, 0.3, 1.0, + PGA | 10–1000 | 1996 | Vs30 = 760 m/s | Current USGS NSHMP (2008)/Proposed USGS NSHMP (2014) | Single corner frequency |
9 | S01 | Somerville et al., 2001 | Joyner-Boore distance | 6.0–7.5 | 0–4 | ≤500 | 2001 | Vs30 = 2830 m/s | Current USGS NSHMP (2008)/Proposed USGS NSHMP (2014) | Finite source model |
10 | SC02 | Silva et al., 2002 | Joyner-Boore distance | 4.5–8.5 | 0.01–10, +PGA, PGV | 1–400 | 2002 | Hard Rock | Proposed USGS NSHMP (2014) | Single corner frequency |
11 | SD02 | Silva et al., 2002 | Joyner-Boore distance | 4.5–8.5 | 0.01–10, +PGA, PGV | 1–400 | 2002 | Hard Rock | Double corner frequency, saturated σ | |
12 | SV02 | Silva et al., 2002 | Joyner-Boore distance | 4.5–8.5 | 0.01–10, +PGA, PGV | 1–400 | 2002 | Hard Rock | Single corner frequency variable Δσ | |
13 | T02 | Toro et al., 1997 | Joyner-Boore distance | 5.0–8.0 | 0.03–2, +PGA | 1–1000 | 1997 | Vs30 = 1830 m/s | Current USGS NSHMP (2008)/Proposed USGS NSHMP (2014) | Single corner frequency |
14 | TP05 | Tavakoli and Pezeshk 2005 | Closest distance from the recording site to the ruptured area | 5.0–8.2 | 0.00–4 | 0–1000 | 2005 | Class A, Vs30>=2000 m/s | Current USGS NSHMP (2008)/Proposed USGS NSHMP (2014) | Hybrid empirical model |
15 | PZT11 | Modified Pezeshk, Tavakoli, and Zandieh, 2011 | Closest distance from the recording site to the ruptured area | 5.0–8.2 | 0.00–4 | 0–1000 | 2012 | Class A, Vs30>=2000 m/s | Proposed USGS NSHMP (2014) | Hybrid empirical model |
16 | EPRI1 | EPRI, 2004 | Joyner-Boore distance | 5.0–8.5 | 0.25–100 | 1–1000 | 2004 | EPRI (2004) cluster 1 model | Spectral single corner | |
17 | EPRI2 | EPRI, 2004 | Joyner-Boore distance | 5.0–8.5 | 0.25–100 | 1–1000 | 2004 | EPRI (2004) cluster 2 model | Spectral double corner | |
18 | EPRI3 | EPRI, 2004 | Closest distance from the recording site to the ruptured area | 5.0–8.5 | 0.25–100 | 1–1000 | 2004 | EPRI (2004) cluster 3 model | Hybrid empirical model | |
19 | EPRI4 | EPRI, 2004 | Joyner-Boore distance | 6.0–7.5 | 0.25–100 | ≤500 | 2004 | EPRI (2004) cluster 4 model | Finite source model |
* VS30 is the average shear wave velocity for the top 30 m of soil
† USGS NSHMP, U.S. Geological Survey National Seismic Hazard Mapping Project.
‡ CEUS, central and eastern United States; getBooreNGA07m.f and getAtk08ENA.f are Fortran subroutines that were modified from the codes obtained from Petersen et al. (2008).
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