Brady 1D seismic velocity model ambient noise prelim
Preliminary 1D seismic velocity model derived from ambient noise correlation. 28 Green's functions filtered between 4-10 Hz for Vp, Vs, and Qs were calculated. 1D model estimated for each path. The final model is a median of the individual models. Resolution is best for the top 1 km. Poorly constrained with increasing depth.
- Research Organization:
- USDOE Geothermal Data Repository (United States); Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
- Sponsoring Organization:
- USDOE Office of Energy Efficiency and Renewable Energy (EERE), Renewable Power Office. Geothermal Technologies Office
- Contributing Organization:
- Lawrence Livermore National Laboratory
- DOE Contract Number:
- EE0005510
- OSTI ID:
- 1148801
- Report Number(s):
- 262
- Availability:
- GDRHelp@EE.Doe.Gov
- Country of Publication:
- United States
- Language:
- English
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