moe333
Geotechnical
- Jul 31, 2003
- 416
Hi All,
I'm trying to perform a Site Specific Ground Motion Hazard Analysis in West Virginia. I have done these previously in California where there are many discrete faults but that isn't the case in West Virginia.
Is this analysis typically performed in this part of the country to attempt to reduce the seismic design category as is the case in California?
My problem is: what fault would I use for the deterministic part of the analysis? The discrete faults are 100's of km's away where attenuation relationships are not considered valid. The only one valid for the Eastern US I have access to is Toro (97). Is this a commonly used relationship in this part of the country? Most of the probabilistic seismicity based on the 2008 USGS deaggregation is from gridded sources. Is it customary to use the gridded source with the R and M as shown in the 2008 USGS deaggregation as a discrete fault in the deterministic analysis?
The other smaller problem is that I'm using the 2008 USGS Deaggregation for the probaibilistic part of the analysis. It will only provide values for Vs-30 of Site Class A and B/C, whereas I need it for Site Class C. I'm assuming I can just apply Fa and Fv coefficients to get to a Site Class C?
Thanks, any suggestions are appreciated.
I'm trying to perform a Site Specific Ground Motion Hazard Analysis in West Virginia. I have done these previously in California where there are many discrete faults but that isn't the case in West Virginia.
Is this analysis typically performed in this part of the country to attempt to reduce the seismic design category as is the case in California?
My problem is: what fault would I use for the deterministic part of the analysis? The discrete faults are 100's of km's away where attenuation relationships are not considered valid. The only one valid for the Eastern US I have access to is Toro (97). Is this a commonly used relationship in this part of the country? Most of the probabilistic seismicity based on the 2008 USGS deaggregation is from gridded sources. Is it customary to use the gridded source with the R and M as shown in the 2008 USGS deaggregation as a discrete fault in the deterministic analysis?
The other smaller problem is that I'm using the 2008 USGS Deaggregation for the probaibilistic part of the analysis. It will only provide values for Vs-30 of Site Class A and B/C, whereas I need it for Site Class C. I'm assuming I can just apply Fa and Fv coefficients to get to a Site Class C?
Thanks, any suggestions are appreciated.