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Characterization of geothermal reservoir crack patterns using shear-wave splitting

Journal Article · · Geophysics
DOI:https://doi.org/10.1190/1.1444159· OSTI ID:483823
;  [1]
  1. Univ. of North Carolina, Chapel Hill, NC (United States)
Microearthquakes recorded by a downhole, three-component seismic network deployed around the Coso, California, geothermal reservoir since 1992 display distinctive shear-wave splitting and clear polarization directions. From the polarizations the authors estimated three predominant subsurface fracture directions, and from the time delays of the split waves they determined tomographically the 3-D fracture density distribution in the reservoir.
Sponsoring Organization:
Department of the Navy, Washington, DC (United States); Idaho National Engineering Lab., Idaho Falls, ID (United States); USDOE, Washington, DC (United States)
OSTI ID:
483823
Journal Information:
Geophysics, Journal Name: Geophysics Journal Issue: 2 Vol. 62; ISSN GPYSA7; ISSN 0016-8033
Country of Publication:
United States
Language:
English

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