Three-dimensional P and S waves velocity structures of the Coso geothermal area, California, from microseismic travel time data
From Open Energy Information
Journal Article: Three-dimensional P and S waves velocity structures of the Coso geothermal area, California, from microseismic travel time data
AbstractHigh precision P and S wave travel times for 2104 microearthquakes with focus <6 km are used in a non-linear inversion to derive high-resolution three-dimensional compressional and shear velocity structures at the Coso Geothermal Area in eastern California. Block size for the inversion is 0.2 km horizontally and 0.5 km vertically and inversions are investigated in the upper 5 km of the geothermal area. Spatial resolution, calculated by synthetic modeling of a cross model at critical locations, is estimated to be 0.35 km for V (sub p ) and 0.5 km for V (sub s ) . Model uncertainties are estimated by a jackknife approach and simulation of random and associated picking errors. Low-velocity zones for both P and S waves are identified at geothermal production depths (1-3 km). A large, low V (sub p ) (-6%) zone is found at depth 2-2.5 km 2 km southwest of Sugarloaf Mountain where high attenuation has been previously reported. However, a general high- V (sub p ) zone is seen under Coso Hot Springs with a slightly low V (sub s ) zone, which is characteristic of fluid saturation. The overall distributions of V (sub p ) and V (sub s ) perturbations do not correlate. An isolated high- V (sub s ) (+9%) feature, about 2 km in diameter, is unambiguously seen 2 km due west of Sugarloaf extending from surface to depth. This feature is surrounded by a circular, low- V (sub s ) belt of approximately 1 km width. The surrounding belt is probably the cracked, high-porosity reservoir/conduit of geothermal fluid flow. In the 2 km southwest Sugarloaf region, we found low V (sub p ) and high V (sub s ) at geothermal production depths from 1 to 2.5 km. Combined with attenuation results, this may represent a hot, fluid-depleted center of magmatic activity.
- Wu, H.; Lees and J.M.
- Published Journal
- Journal of Geophysical Research, 6/1/1999
- Not Provided
Check for DOI availability: http://crossref.org
Wu, H.; Lees, J.M. . 6/1/1999. Three-dimensional P and S waves velocity structures of the Coso geothermal area, California, from microseismic travel time data. Journal of Geophysical Research. (!) .