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

0440249 - GFÚ 2015 RIV NL eng C - Konferenční příspěvek (zahraniční konf.)
Mrlina, Jan
Do Active Transverse Faults Exist on the Southern Coast of Corinth Rift?
Proceedings of the 20th European Meeting of Environmental and Engineering Geophysics - Near Surface Geoscience. Houten: EAGE, 2014, Tu PA2 06/1-Tu PA2 06/5. ISBN 978-94-6282-027-2.
[Near Surface Geoscience 2014 - 20th European Meeting of Environmental and Engineering Geophysics. Athens (GR), 14.09.2014-18.09.2014]
Grant ostatní: European Commission(XE) 5FP Project NNE5-2001-00501
Institucionální podpora: RVO:67985530
Klíčová slova: active faults * Gulf of Corinth * gravity survey
Kód oboru RIV: DC - Seismologie, vulkanologie a struktura Země

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.
Trvalý link: http://hdl.handle.net/11104/0243355