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The 2020 Samos Mw7 earthquake: Source model depicting complexity and rupture directivity

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F22%3A10452467" target="_blank" >RIV/00216208:11320/22:10452467 - isvavai.cz</a>

  • Result on the web

    <a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=8~K625kd2K" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=8~K625kd2K</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.tecto.2022.229591" target="_blank" >10.1016/j.tecto.2022.229591</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    The 2020 Samos Mw7 earthquake: Source model depicting complexity and rupture directivity

  • Original language description

    The October 30, 2020, Mw7 Samos earthquake ruptured a north-dipping offshore normal fault, bounding the Samos basin; it accommodated-N-S extension and can be viewed as a modern manifestation of the basin evolution. It caused 118 fatalities, generated a tsunami, and caused a co-seismic uplift of 20 to 35 cm of the NW part of Samos Island. Using broadband, strong-motion, and geodetic data, we constrain the location and source geometry of the mainshock. A multiple-point source model suggests three sequential subevents providing 20 s of source duration. Our finite-fault kinematic model confirms the prevalence of large slip amplitudes (-2.4 m) along the entire ruptured area and the up-dip and westward rupture propagation. This directivity is indepen-dently confirmed by Apparent Source Time Functions inferred from regional recordings using a herein developed new variant of the empirical Green&apos;s function method. Static GNSS displacements from inland stations yield a near-surface co-seismic slip of-1 m amplitude, contributing to any interpretation of the observed island uplift. The 2020 Samos event showed that in the spatially heterogeneous oblique transtentional regions in the back-arc Aegean region, normal faults bounding the basins are capable to rupture in M7 earthquakes, provoke tsunami generation, and constitute a constant threat to the nearby coastal areas of both Greece and Turkey.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10500 - Earth and related environmental sciences

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2022

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Tectonophysics

  • ISSN

    0040-1951

  • e-ISSN

    1879-3266

  • Volume of the periodical

    843

  • Issue of the periodical within the volume

    October

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    15

  • Pages from-to

    229591

  • UT code for WoS article

    000892625500002

  • EID of the result in the Scopus database

    2-s2.0-85140204433