Postseismic deformation following the Mw 7.2, 23October 2011 Van earthquake (Turkey): Evidence for a seismic fault reactivation

Ugur Dogan, Deniz Demir, Ziyadin Cakir, Semih Ergintav, Haluk Ozener, Ahmet Akoglu, Suleyman S Nalbant, Robert Reilinger

    Research output: Contribution to journalArticle

    16 Citations (Scopus)
    9 Downloads (Pure)

    Abstract

    Geodetic measurements following the 23 October 2011, Mw = 7.2 Van (eastern Turkey)earthquake reveal that a fault splay on the footwall block of the coseismic thrust fault was reactivated and slipped aseismically for more than 1.5 years following the earthquake. Although long-lasting aseismic slip on coseismic ruptures has been documented following many large earthquakes, long-lasting, triggered slip on neighboring faults that did not rupture during the earthquake has not been reported previously. Elastic dislocation and Coulomb stress modeling indicate that the postseismic deformation can be adequately explained by shallow slip on both the coseismic and splay fault and is likely driven mostly by coseismic stress changes. Thus, the slip deficit on the shallow section of the coseismic fault indicated by interferometric synthetic aperture radar-based models has been partially filled by aseismic slip, suggesting a lower likelihood for a large earthquake on the shallow section of the Van fault than suggested by previous studies.
    Original languageEnglish
    Pages (from-to)2334-2341
    JournalGeophysical Research Letters
    Volume41
    DOIs
    Publication statusPublished - 7 Apr 2014

    Keywords

    • 2011 Van earthquake
    • afterslip
    • coseismic stress change

    Fingerprint Dive into the research topics of 'Postseismic deformation following the Mw 7.2, 23October 2011 Van earthquake (Turkey): Evidence for a seismic fault reactivation'. Together they form a unique fingerprint.

  • Cite this