<?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%">Athanassios Ganas</style></author><author><style face="normal" font="default" size="100%">Elias, Panagiotis</style></author><author><style face="normal" font="default" size="100%">Vasilis Kapetanidis</style></author><author><style face="normal" font="default" size="100%">Sotirios Valkaniotis</style></author><author><style face="normal" font="default" size="100%">Briole, Pierre</style></author><author><style face="normal" font="default" size="100%">Ioannis Kassaras</style></author><author><style face="normal" font="default" size="100%">Argyrakis, Panagiotis</style></author><author><style face="normal" font="default" size="100%">Barberopoulou, Aggeliki</style></author><author><style face="normal" font="default" size="100%">Moshou, Alexandra</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The July 20, 2017 M6.6 Kos Earthquake: Seismic and Geodetic Evidence for an Active North-Dipping Normal Fault at the Western End of the Gulf of Gökova (SE Aegean Sea)</style></title><secondary-title><style face="normal" font="default" size="100%">Pure and Applied Geophysics</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">Oct</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://doi.org/10.1007/s00024-019-02154-y</style></url></web-urls></urls><number><style face="normal" font="default" size="100%">10</style></number><volume><style face="normal" font="default" size="100%">176</style></volume><pages><style face="normal" font="default" size="100%">4177–4211</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">On July 20, 2017 22:31 UTC, a strong Mwþinspace}=þinspace}6.6 earthquake occurred at shallow depth between Kos Island (Greece) and Bodrum (Turkey). We derive a co-seismic fault model from joint inversion of geodetic data (GNSS and InSAR) assuming that the earthquake can be modelled by the slip of a rectangular fault buried in an elastic and homogeneous half-space. The GNSS observations constrain well most of the model parameters but do not permit to discriminate between south- and north-dipping planes. However, the interferograms, produced from C-band ESA Sentinel 1 data, give a clear preference to the north-dipping plane. We also map surface motion away from the satellite along the Turkish coast (from Bodrum towards the east) which reached about 17&amp;nbsp;cm onshore islet Karaada. The best-fit model is obtained with a 37° north-dipping, N283°E striking normal fault, in agreement with the published moment tensor solutions. The resolved slip vector is dominantly normal with a slight component of left-lateral motion (15°). The surface projection of the seismic fault outcrops in the Gökova ridge area, a well-developed bathymetric feature inside the western Gulf of Gökova. Our geodetic model fits the pattern of the shallow, north-dipping aftershocks obtained from rigorous relocation of all available recordings in the region (about 1120 events; relocated mainshock is at 36.955°N, 27.448°E; depth at 9.2&amp;nbsp;kmþinspace}±þinspace}0.5&amp;nbsp;km). The relocated aftershocks also indicate clustering at both ends of the rupture and seismicity triggering mainly towards the east and the north, within 2 weeks following the mainshock. We also analysed regional GPS data (interseismic velocities) and obtained an extension rate of 3.2&amp;nbsp;mm/yr across the Gökova rift, along a direction N165°E.</style></abstract></record></records></xml>