Microearthquakes recorded by a downhole, three-component seismic netwo
rk deployed around the Coso, California, geothermal reservoir since 19
92 display distinctive shear-wave splitting and clear polarization dir
ections. From the polarizations we estimated three predominant subsurf
ace fracture directions, and from the time delays of the split waves w
e determined tomographically the 3-D fracture density distribution in
the reservoir.