View source: R/bssa_2014_nga.R
bssa_2014_nga | R Documentation |
This function calculates the ground motion median values and standard deviations
bssa_2014_nga(
M,
T = 1000,
Rjb,
Fault_Type,
region,
z1 = 999,
Vs30,
return.type = 1,
CA_subreg_path = FALSE,
site_lon = NULL,
site_lat = NULL,
clst_lon = NULL,
clst_lat = NULL
)
M |
Moment magnitude, a numeric value |
T |
Period (sec); Use Period = -1 for PGV computation. Use 1000 (by default) for output the array of Sa with original NGA West2 periods |
Rjb |
Joyner-Boore distance (km); closest distance (km) to surface projection of rupture plane |
Fault_Type |
The indicator of fault type: 0 for unspecified fault; 1 for strike-slip fault; 2 for normal fault; 3 for reverse fault |
region |
Region indicator: 0 for global (incl. Taiwan); 1 for California; 2 for Japan; 3 for China or Turkey; 4 for Italy |
z1 |
Basin depth (km): depth from the groundsurface to the 1km/s shear-wave horizon. 999 if unknown. |
Vs30 |
Shear wave velocity averaged over top 30 m (in m/s) |
return.type |
The indicator specifies which type of data return: 1 for the med (in g)/sigma/phi/tau/period; 2 for F_E/F_P/F_P_GS(geomteric spreading)/F_P_AA(anelastic attenuation)/F_S; 3 for r/Ln_Flin/Ln_Fnlin/f2/F_dz1/PGAr |
CA_subreg_path |
The flag indicating if a CA subregional anelastic attenuation model (Buckreis et al., 2023) is applied. Buckreis, Stewart, Brandenberg, and Wang (2023) "Subregional Anelastic Attenuation Model for California". |
site_lon |
The longitude of site (in WGS84 degree). Required if CA_subreg_path is TRUE. |
site_lat |
The latitude of site (in WGS84 degree). Required if CA_subreg_path is TRUE. |
clst_lon |
Longitude (in WGS84 degrees) of closest point on the surface projection of the rupture surface to the site. Required if CA_subreg_path is TRUE. |
clst_lat |
Latitude (in WGS84 degrees) of closest point on the surface projection of the rupture surface to the site. Required if CA_subreg_path is TRUE. |
See return.type for the returned results
Boore, D. M., Stewart, J. P., Seyhan, E., and Atkinson, G. M. (2014). NGA-West2 Equations for Predicting PGA, PGV, and 5 Shallow Crustal Earthquakes. Earthquake Spectra, 30(3), 1057-1085.
bssa_2014_nga(M = 5, T = 1000, Rjb = 85, Fault_Type = 1, region = 1, z1 = 999, Vs30 = 350)
bssa_2014_nga(M = 5, T = 1000, Rjb = 85, Fault_Type = 1, region = 1, z1 = 999, Vs30 = 350, CA_subreg_path = TRUE, site_lon = -118.8713, site_lat = 35.80407, clst_lon = -116.9274, clst_lat = 33.6204)
Add the following code to your website.
For more information on customizing the embed code, read Embedding Snippets.