Difference between revisions of "Hadley-Kanamori"
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| − | + | Hadley Kanamori 1D model is used for various purposes in SCEC research, and by seismic networks in California. | |
| − | |||
| + | == SCSN Hadley-Kanamori 1D Model == | ||
| + | [[Image:HadleyKanamori-1D.png|256px|thumb|right| Table 5 from Hutton et al 2010]] | ||
| − | + | The layers and Vp values in the SCSN HK model are given below. SCSN uses a Vp/Vs ratio of 1.73 | |
<pre> | <pre> | ||
| + | Top of Layer (km) P-Velocity (km/sec) | ||
| + | 0.0 5.5 | ||
| + | 5.5 6.3 | ||
| + | 16.0 6.7 | ||
| + | 32.0 7.8 | ||
| + | </pre> | ||
| + | |||
| + | A paper that cites the model and defines the layers. | ||
| + | #Hutton, K., Woessner, J., Hauksson, E. (2010) Earthquake Monitoring in Southern California for Seventy-Seven Years (1932-2008) BSSA, Vol. 100, No. 2, pp423-446, April 2010 | ||
| + | |||
| + | == SCEC Hadley-Kanamori 1D Model Definition == | ||
| + | SCEC uses a modified version of the HK model as a background model in their 3D velocity models. This means that if you query some of the Calfornia CVM's outside their defined coverage region, the CVM will return values from the HK model. In general, CVM tools will use linear interpolate between layers, so material properties returned vary gradually between model layers. | ||
| + | |||
| + | The following plot shows the SCEC HK 1D model: | ||
| + | [[File:1d_cvms4_hk.png|256px|thumb|right| Plot of Vp, Vs, and rho in SCEC HK 1D Model]] | ||
| + | |||
| + | <pre> | ||
| + | # 1D Velocity Model configuration | ||
# | # | ||
# Vp is interpolated between layer n to n+1. | # Vp is interpolated between layer n to n+1. | ||
| Line 11: | Line 30: | ||
# | # | ||
version=Hadley-Kanamori 1D (CVM-S) | version=Hadley-Kanamori 1D (CVM-S) | ||
| − | |||
# Depth of model in layers | # Depth of model in layers | ||
num_z=9 | num_z=9 | ||
| − | |||
# Depth to start of layer (km) | # Depth to start of layer (km) | ||
depth_vals=1.0, 5.0, 6.0, 10.0, 15.5, 16.5, 22.0, 31.0, 33.0 | depth_vals=1.0, 5.0, 6.0, 10.0, 15.5, 16.5, 22.0, 31.0, 33.0 | ||
| − | |||
# Vp at start of layer (km/s) | # Vp at start of layer (km/s) | ||
vp_vals=5.0, 5.5, 6.3, 6.3, 6.4, 6.7, 6.75, 6.8, 7.8 | vp_vals=5.0, 5.5, 6.3, 6.3, 6.4, 6.7, 6.75, 6.8, 7.8 | ||
</pre> | </pre> | ||
| − | == | + | == Related Entries == |
| − | + | *[[BBP 1D LA Basin Model]] | |
| + | *[[UCVM]] | ||
| + | *[[CME_Project]] | ||
Latest revision as of 21:41, 22 January 2017
Hadley Kanamori 1D model is used for various purposes in SCEC research, and by seismic networks in California.
SCSN Hadley-Kanamori 1D Model
The layers and Vp values in the SCSN HK model are given below. SCSN uses a Vp/Vs ratio of 1.73
Top of Layer (km) P-Velocity (km/sec) 0.0 5.5 5.5 6.3 16.0 6.7 32.0 7.8
A paper that cites the model and defines the layers.
- Hutton, K., Woessner, J., Hauksson, E. (2010) Earthquake Monitoring in Southern California for Seventy-Seven Years (1932-2008) BSSA, Vol. 100, No. 2, pp423-446, April 2010
SCEC Hadley-Kanamori 1D Model Definition
SCEC uses a modified version of the HK model as a background model in their 3D velocity models. This means that if you query some of the Calfornia CVM's outside their defined coverage region, the CVM will return values from the HK model. In general, CVM tools will use linear interpolate between layers, so material properties returned vary gradually between model layers.
The following plot shows the SCEC HK 1D model:
# 1D Velocity Model configuration # # Vp is interpolated between layer n to n+1. # Rho is derived from vp (./src/ucvm/ucvm_model_1d.c) # Vs is derived from Vp and Rho (./src/ucvm/ucvm_model_1d.c) # version=Hadley-Kanamori 1D (CVM-S) # Depth of model in layers num_z=9 # Depth to start of layer (km) depth_vals=1.0, 5.0, 6.0, 10.0, 15.5, 16.5, 22.0, 31.0, 33.0 # Vp at start of layer (km/s) vp_vals=5.0, 5.5, 6.3, 6.3, 6.4, 6.7, 6.75, 6.8, 7.8
