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Title: Newberry EGS Seismic Velocity Model

We use ambient noise correlation (ANC) to create a detailed image of the subsurface seismic velocity at the Newberry EGS site down to 5 km. We collected continuous data for the 22 stations in the Newberry network, together with 12 additional stations from the nearby CC, UO and UW networks. The data were instrument corrected, whitened and converted to single bit traces before cross correlation according to the methodology in Benson (2007). There are 231 unique paths connecting the 22 stations of the Newberry network. The additional networks extended that to 402 unique paths crossing beneath the Newberry site.
Publication Date:
OSTI Identifier:
Report Number(s):
DOE Contract Number:
FY13 AOP 25728
Resource Type:
Data Type:
Specialized Mix
Research Org:
DOE Geothermal Data Repository; Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
Sponsoring Org:
USDOE Office of Energy Efficiency and Renewable Energy (EERE), Geothermal Technologies Office (EE-4G)
Contributing Orgs:
Lawrence Livermore National Laboratory
Country of Publication:
United States
15 Geothermal Energy geothermal; EGS; velocity; reservoir; seismic velocity