<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>47</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">A. Ganas</style></author><author><style face="normal" font="default" size="100%">P. Elias</style></author><author><style face="normal" font="default" size="100%">V. Kapetanidis</style></author><author><style face="normal" font="default" size="100%">S. Valkaniotis</style></author><author><style face="normal" font="default" size="100%">Briole, P.</style></author><author><style face="normal" font="default" size="100%">Kassaras, I.</style></author><author><style face="normal" font="default" size="100%">P. Argyrakis</style></author><author><style face="normal" font="default" size="100%">A. Barberopoulou</style></author><author><style face="normal" font="default" size="100%">A. Moshou</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The July 20, 2017 M6.6 Kos-Bodrum earthquake: seismic and geodetic evidence for a north-dipping, normal fault at the western end of the Gulf of Gökova</style></title><secondary-title><style face="normal" font="default" size="100%">EGU General Assembly 2018</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><pub-location><style face="normal" font="default" size="100%">Vienna, Austria</style></pub-location><volume><style face="normal" font="default" size="100%">20</style></volume><pages><style face="normal" font="default" size="100%">9262</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;On July 20, 2017 22:31 UTC, a strong Mw = 6.6 earthquake occurred at shallow depth between Kos (Greece) and Bodrum (Turkey).We derive a co-seismic fault model from joint inversion of geodetic data (GNSS and InSAR).We assume that the earthquake can be modelled by the slip on a rectangular fault buried in an elastic and homogenous half-space. The GNSS observations constrain well most of the model parameters but do not permit to discriminate between south- and north-dipping planes. The interferograms, produced from C-band ESA Sentinel 1 synthetic&lt;br&gt;aperture radar data, give a clear preference to the north-dipping plane. The orientation of the GNSS vectors and the absence of InSAR fringes onshore Kos constrain the fault’s length. We also mapped surface motion away from the&lt;br&gt;satellite along the Turkish coast (from Bodrum towards east) which reached about 20 cm onshore islet Karaada. The best-fit model was obtained with a 37 deg. north-dipping normal fault, in agreement with the published moment tensor solutions. The slip vector is dominantly normal in a ESE-WNW direction with a component of left-lateral motion (5 deg.). The surface projection of the seismic fault outcrops in the Gökova ridge area, a well-developed bathymetric feature inside the western Gulf of Gökova (SE Aegean Sea). The seismic fault plane extends 14 km along strike by&lt;br&gt;12.5 km wide. Our geodetic model is in agreement with relocated seismicity distribution (about 1160 events) from regional networks, which indicates an aftershock occurrence towards both ends of the rupture.&lt;/p&gt;</style></abstract></record></records></xml>