West Flank Coso FORGE: Seismic Reflection
Abstract
PDFs of seismic reflection profiles 101,110, 111 local to the West Flank FORGE site. 45 line kilometers of seismic reflection data are processed data collected in 2001 through the use of vibroseis trucks. The initial analysis and interpretation of these data was performed by Unruh et al. (2001). Optim processed these data by inverting the P-wave first arrivals to create a 2-D velocity structure. Kirchhoff images were then created for each line using velocity tomograms (Unruh et al., 2001).
- Authors:
- Publication Date:
- Other Number(s):
- 810
- DOE Contract Number:
- EE0007156
- Product Type:
- Dataset
- Research Org.:
- DOE Geothermal Data Repository; Sandia National Laboratories (SNL), Albuquerque, NM, and Livermore, CA (United States)
- Sponsoring Org.:
- USDOE Office of Energy Efficiency and Renewable Energy (EERE), Geothermal Technologies Program (EE-2C)
- Subject:
- 15 Geothermal Energy
- Keywords:
- geothermal; EGS; FORGE; West Flank; Seismic Reflection; survey map; wave; prestack kirchoff migration; seismic profiles; Coso; seismic; geophysics; California
- OSTI Identifier:
- 1287568
- DOI:
- 10.15121/1287568
Citation Formats
Blankenship, Doug. West Flank Coso FORGE: Seismic Reflection. United States: N. p., 2016.
Web. doi:10.15121/1287568.
Blankenship, Doug. West Flank Coso FORGE: Seismic Reflection. United States. doi:10.15121/1287568.
Blankenship, Doug. 2016.
"West Flank Coso FORGE: Seismic Reflection". United States. doi:10.15121/1287568. https://www.osti.gov/servlets/purl/1287568. Pub date:Mon May 16 00:00:00 EDT 2016
@article{osti_1287568,
title = {West Flank Coso FORGE: Seismic Reflection},
author = {Blankenship, Doug},
abstractNote = {PDFs of seismic reflection profiles 101,110, 111 local to the West Flank FORGE site. 45 line kilometers of seismic reflection data are processed data collected in 2001 through the use of vibroseis trucks. The initial analysis and interpretation of these data was performed by Unruh et al. (2001). Optim processed these data by inverting the P-wave first arrivals to create a 2-D velocity structure. Kirchhoff images were then created for each line using velocity tomograms (Unruh et al., 2001).},
doi = {10.15121/1287568},
journal = {},
number = ,
volume = ,
place = {United States},
year = {2016},
month = {5}
}
Save to My Library
You must Sign In or Create an Account in order to save documents to your library.