Item talk:Q243383
From geokb
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"abstract": "We use interferometric synthetic aperture radar (InSAR), body wave seismology, satellite imagery, and field observations to constrain the fault parameters of the Mw\u20097.1\u20092011\u2009Van (Eastern Turkey) reverse-slip earthquake, in the Turkish-Iranian plateau. Distributed slip models from elastic dislocation modeling of the InSAR surface displacements from ENVISAT and COSMO-SkyMed interferograms indicate up to 9\u2009m of reverse and oblique slip on a pair of en echelon NW\u200940 \u00b0\u201354 \u00b0 dipping fault planes which have surface extensions projecting to just 10\u2009km north of the city of Van. The slip remained buried and is relatively deep, with a centroid depth of 14\u2009km, and the rupture reaching only within 8\u20139\u2009km of the surface, consistent with the lack of significant ground rupture. The up-dip extension of this modeled WSW striking fault plane coincides with field observations of weak ground deformation seen on the western of the two fault segments and has a dip consistent with that seen at the surface in fault gouge exposed in Quaternary sediments. No significant coseismic slip is found in the upper 8\u2009km of the crust above the main slip patches, except for a small region on the eastern segment potentially resulting from the Mw\u20095.9 aftershock on the same day. We perform extensive resolution tests on the data to confirm the robustness of the observed slip deficit in the shallow crust. We resolve a steep gradient in displacement at the point where the planes of the two fault segments ends are inferred to abut at depth, possibly exerting some structural control on rupture extent.",
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