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The January 2010 Efpalio earthquake sequence in the western Corinth Gulf (Greece)

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F12%3A10123788" target="_blank" >RIV/00216208:11320/12:10123788 - isvavai.cz</a>

  • Alternative codes found

    RIV/68407700:21110/12:00225607

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.tecto.2012.01.005" target="_blank" >http://dx.doi.org/10.1016/j.tecto.2012.01.005</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.tecto.2012.01.005" target="_blank" >10.1016/j.tecto.2012.01.005</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    The January 2010 Efpalio earthquake sequence in the western Corinth Gulf (Greece)

  • Original language description

    The January 2010 Efpalio earthquake sequence provides some key elements to enhance our view on the western Corinth Gulf tectonics. The sequence lasted almost six months, and included two Mw > 5 strong events, both exhibiting normal faulting along similarto E-W trending planes. This paper attempts to construct a unified seismotectonic model of the sequence jointly interpreting earthquake locations, moment-tensors and slip inversions in terms of the possible activated fault planes. Previous studies haveconnected the prevailing microseismic activity to a major low-angle, north-dipping structure under the Corinth Gulf and the Efpalio sequence favors such a general trend. Moreover, it clearly shows the significance of the shallow activity, so far less recognized, and possibly connected to the relatively steep faults outcropping on the northern coast. The first 18 January 2010 Mw>5 event had almost no on-fault aftershocks and most likely it occurred on a 550 south-dipping nodal plane. The

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DC - Seismology, volcanology and Earth structure

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GAP210%2F11%2F0854" target="_blank" >GAP210/11/0854: Improving physical insight into the Mediterranean earthquakes</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)

Others

  • Publication year

    2012

  • 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

  • Volume of the periodical

    530

  • Issue of the periodical within the volume

    MARCH

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    11

  • Pages from-to

    299-309

  • UT code for WoS article

    000302838900019

  • EID of the result in the Scopus database