The complete (3-D) surface displacement field in the epicentral area of the 1999 M(w)7.1 Hector Mine earthquake, California, from space geodetic observations
Y. Fialko et al., The complete (3-D) surface displacement field in the epicentral area of the 1999 M(w)7.1 Hector Mine earthquake, California, from space geodetic observations, GEOPHYS R L, 28(16), 2001, pp. 3063-3066
We use Interferometric Synthetic Aperture Radar (InSAR) data to derive cont
inuous maps for three orthogonal components of the co-seismic surface displ
acement field due to the 1999 M-w 7.1 Hector Mine earthquake in southern Ca
lifornia. Vertical and horizontal displacements are both predominantly anti
symmetric with respect to the fault plane, consistent with predictions of l
inear elastic models of deformation for a strike-slip fault. Some deviation
s from symmetry apparent in the surface displacement data may result from c
omplexity in the fault geometry.