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Do Active Transverse Faults Exist on the Southern Coast of Corinth Rift?
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SYSNO ASEP 0440249 Document Type C - Proceedings Paper (int. conf.) R&D Document Type Conference Paper Title Do Active Transverse Faults Exist on the Southern Coast of Corinth Rift? Author(s) Mrlina, Jan (GFU-E) ORCID, RID Source Title Proceedings of the 20th European Meeting of Environmental and Engineering Geophysics - Near Surface Geoscience. - Houten : EAGE, 2014 - ISBN 978-94-6282-027-2 Pages tu pa2 06/1-tu pa2 06/5 Number of pages 5 s. Publication form Medium - C Action Near Surface Geoscience 2014 - 20th European Meeting of Environmental and Engineering Geophysics Event date 14.09.2014-18.09.2014 VEvent location Athens Country GR - Greece Event type EUR Language eng - English Country NL - Netherlands Keywords active faults ; Gulf of Corinth ; gravity survey Subject RIV DC - Siesmology, Volcanology, Earth Structure Institutional support GFU-E - RVO:67985530 EID SCOPUS 84908388274 Annotation One 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. Workplace Geophysical Institute Contact Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Year of Publishing 2015
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