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Newberry EGS Seismic Velocity Model

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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.

Citation Formats

TY - DATA AB - 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. AU - Templeton, Dennise DB - Open Energy Data Initiative (OEDI) DP - Open EI | National Renewable Energy Laboratory DO - 10.15121/1148781 KW - geothermal KW - EGS KW - velocity KW - reservoir KW - seismic velocity KW - cross-correlation KW - model KW - geophysics KW - Newberry LA - English DA - 2013/10/01 PY - 2013 PB - Lawrence Livermore National Laboratory T1 - Newberry EGS Seismic Velocity Model UR - https://doi.org/10.15121/1148781 ER -
Export Citation to RIS
Templeton, Dennise. Newberry EGS Seismic Velocity Model. Lawrence Livermore National Laboratory, 1 October, 2013, GDR. https://doi.org/10.15121/1148781.
Templeton, D. (2013). Newberry EGS Seismic Velocity Model. [Data set]. GDR. Lawrence Livermore National Laboratory. https://doi.org/10.15121/1148781
Templeton, Dennise. Newberry EGS Seismic Velocity Model. Lawrence Livermore National Laboratory, October, 1, 2013. Distributed by GDR. https://doi.org/10.15121/1148781
@misc{OEDI_Dataset_6620, title = {Newberry EGS Seismic Velocity Model}, author = {Templeton, Dennise}, abstractNote = {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. }, url = {https://gdr.openei.org/submissions/282}, year = {2013}, howpublished = {GDR, Lawrence Livermore National Laboratory, https://doi.org/10.15121/1148781}, note = {Accessed: 2025-04-30}, doi = {10.15121/1148781} }
https://dx.doi.org/10.15121/1148781

Details

Data from Oct 1, 2013

Last updated Nov 14, 2019

Submitted Feb 5, 2014

Organization

Lawrence Livermore National Laboratory

Contact

Dennise Templeton

templeton4@llnl.gov

925.422.2021

Authors

Dennise Templeton

Lawrence Livermore National Laboratory

Research Areas

DOE Project Details

Project Lead Lauren Boyd

Project Number FY13 AOP 25728

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