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Do Active Transverse Faults Exist on the Southern Coast of Corinth Rift?

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    SYSNO ASEP0440249
    Document TypeC - Proceedings Paper (int. conf.)
    R&D Document TypeConference Paper
    TitleDo Active Transverse Faults Exist on the Southern Coast of Corinth Rift?
    Author(s) Mrlina, Jan (GFU-E) ORCID, RID
    Source TitleProceedings of the 20th European Meeting of Environmental and Engineering Geophysics - Near Surface Geoscience. - Houten : EAGE, 2014 - ISBN 978-94-6282-027-2
    Pagestu pa2 06/1-tu pa2 06/5
    Number of pages5 s.
    Publication formMedium - C
    ActionNear Surface Geoscience 2014 - 20th European Meeting of Environmental and Engineering Geophysics
    Event date14.09.2014-18.09.2014
    VEvent locationAthens
    CountryGR - Greece
    Event typeEUR
    Languageeng - English
    CountryNL - Netherlands
    Keywordsactive faults ; Gulf of Corinth ; gravity survey
    Subject RIVDC - Siesmology, Volcanology, Earth Structure
    Institutional supportGFU-E - RVO:67985530
    EID SCOPUS84908388274
    AnnotationOne of the most seismoactive regions of the Corinth Rift in Greece is the area around Aigion on the southwestern coast of the Gulf of Corinth. The system of active normal faults was determined by both geological and seismological studies. However, many questions persist on total slip rates on the faults, as well as the thickness and geometry of sedimentary cover of the basement formed by Mesozoic carbonates. Moreover, not enough information was available on the structural and tectonic setting between the Helike and Aigion faults. No discussions were held on possible existence and activity of transverse faults of N-S to NNE-SSW direction.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2015
Number of the records: 1  

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