<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Donnellan, A.</style></author><author><style face="normal" font="default" size="100%">Parker, JW</style></author><author><style face="normal" font="default" size="100%">Peltzer, G</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Combined GPS and InSAR models of postseismic deformation from the Northridge earthquake</style></title><secondary-title><style face="normal" font="default" size="100%">PURE AND APPLIED GEOPHYSICS</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">afterslip</style></keyword><keyword><style  face="normal" font="default" size="100%">earthquake</style></keyword><keyword><style  face="normal" font="default" size="100%">GPS</style></keyword><keyword><style  face="normal" font="default" size="100%">InSAR</style></keyword><keyword><style  face="normal" font="default" size="100%">Northridge</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2002</style></year><pub-dates><date><style  face="normal" font="default" size="100%">SEP</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">10</style></number><publisher><style face="normal" font="default" size="100%">BIRKHAUSER VERLAG AG</style></publisher><pub-location><style face="normal" font="default" size="100%">VIADUKSTRASSE 40-44, PO BOX 133, CH-4010 BASEL, SWITZERLAND</style></pub-location><volume><style face="normal" font="default" size="100%">159</style></volume><pages><style face="normal" font="default" size="100%">2261-2270</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Models of combined Global Positioning System (GPS) and Interferometric Synthetic Aperture Radar (InSAR) data collected in the region of the Northridge earthquake indicate that significant afterslip on the main fault occurred following the earthquake. Additional shallow deformation occurred to the west of the main rupture plane. Both data sets are consistent with logarithmic time-dependent behavior following the earthquake indicative of afterslip rather than postseismic relaxation. Aftershocks account for only about 10% of the postseismic motion. The two data sets are complimentary in determining the postseismic processes. Fault afterslip and shallow deformation dominate the deformation field in the two years following the earthquake. Lower crustal deformation may play an important role later in the earthquake cycle.</style></abstract><work-type><style face="normal" font="default" size="100%">Article</style></work-type></record></records></xml>