000193667 001__ 193667
000193667 003__ CZ-ZdVUG
000193667 005__ 20190114114334.0
000193667 041__ $$aeng
000193667 040__ $$aABC039$$bcze
000193667 1001_ $$aKostelecký, Jan
000193667 24510 $$aRupture process of the 2014 Cephalonia, Greece, earthquake doublet (Mw6) as inferred from regional and local seismic data
000193667 300__ $$a11 stran
000193667 5203_ $$aWe study the 26 January and 3 February, 2014 (~Mw6) events in Cephalonia, combining weak and strong motion wave forms from regional and local stations. The hypocenter of the January 26 event is located at the southern most tip of the Paliki Peninsula, ata depth of ~15 km. The centroid moment tensor (CMT) solution indicates rupture along a N20°E dextral strike-slip fault, dipping to the east. The hypocenter of the February 3 event is 10 km NNE of the first, at shallower depth (~5 km). The CMT solution of this event is highly uncertain. The kinematic slip model for the January 26 event indicates that the rupture was mainly confined to shallow depths, and it propagand upwards and towards NE. The major slip patches, when projected to the surface, cover the western part of the Paliki Peninsula and include the areaswhere surface ruptureswere observed. Our preferred slip model for the event of February 3 is based on a published two-segment fault model.
000193667 655_4 $$ačlánek v odborném periodiku
000193667 7001_ $$aGallovič, František
000193667 7001_ $$aJanský, J.
000193667 7001_ $$aKiratzi, Anna
000193667 7001_ $$aPlicka, Vladimír
000193667 7001_ $$aSerpetsidaki, A.
000193667 7001_ $$aSokos, Effimios
000193667 7001_ $$aTselentis, G.-A.
000193667 7001_ $$aZahradník, Jiří
000193667 7730_ $$92015$$dSpolková republika Německo, 2015.$$g656. (2015), s.131-141.$$tTectonophysics$$x0040-1951
000193667 85642 $$ahttps://www.rvvi.cz/riv?s=rozsirene-vyhledavani&ss=detail&n=0&h=RIV%2F00025615%3A_____%2F15%3A%230002177%21RIV16-MSM-00025615
000193667 910__ $$aABC039
000193667 980__ $$aclanky_vugtk
000193667 985__ $$akosteleckyjan
000193667 985__ $$ariv
000193667 985__ $$autvar24