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.

Data and Resources

Field Value
DOI 10.15121/1148781
accessLevel public
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datagov_dedupe_retained 20250120143002
identifier https://data.openei.org/submissions/6620
issued 2013-10-01T06:00:00Z
landingPage https://gdr.openei.org/submissions/282
license https://creativecommons.org/licenses/by/4.0/
modified 2019-11-14T22:45:16Z
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programCode {019:006}
projectLead Lauren Boyd
projectNumber FY13 AOP 25728
publisher Lawrence Livermore National Laboratory
resource-type Dataset
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Groups
  • AmeriGEOSS
  • National Provider
  • North America
Tags
  • AmeriGEO
  • AmeriGEOSS
  • CKAN
  • GEO
  • GEOSS
  • National
  • North America
  • United States
  • cross-correlation
  • egs
  • geophysics
  • geothermal
  • model
  • newberry
  • reservoir
  • seismic-velocity
  • velocity
isopen True
license_id cc-by
license_title Creative Commons Attribution
license_url http://www.opendefinition.org/licenses/cc-by
maintainer Dennise Templeton
maintainer_email templeton4@llnl.gov
metadata_created 2025-09-24T22:30:11.102338
metadata_modified 2025-09-24T22:30:11.102346
notes 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.
num_resources 1
num_tags 17
title Newberry EGS Seismic Velocity Model