Rupture process of the 2014 Cephalonia, Greece, earthquake doublet (Mw6) as inferred from regional and local seismic data
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F15%3A10314777" target="_blank" >RIV/00216208:11320/15:10314777 - isvavai.cz</a>
Alternative codes found
RIV/61989100:27350/15:86095115 RIV/00025615:_____/15:#0002177
Result on the web
<a href="http://dx.doi.org/10.1016/j.tecto.2015.06.013" target="_blank" >http://dx.doi.org/10.1016/j.tecto.2015.06.013</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.tecto.2015.06.013" target="_blank" >10.1016/j.tecto.2015.06.013</a>
Alternative languages
Result language
angličtina
Original language name
Rupture process of the 2014 Cephalonia, Greece, earthquake doublet (Mw6) as inferred from regional and local seismic data
Original language description
We study the 26 January and 3 February, 2014 (similar to Mw6) events in Cephalonia, combining weak and strong motion waveforms from regional and local stations. The hypocenter of the January 26 event is located at the southern-most tip of the Paliki Peninsula, at a depth of similar to 15 km. The centroidmoment tensor (CMT) solution indicates rupture along a N20 degrees 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 (similar to 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 propagated upwards and towards NE. The major slip patches, when projected to the surface, cover the western part of the Paliki Peninsula and include the areas where surface ruptures were observed. Our preferred slip model for the event of February 3 is based on a published two-segment fault model.
Czech name
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Czech description
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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
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Result continuities
Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2015
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
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Volume of the periodical
656
Issue of the periodical within the volume
August
Country of publishing house
NL - THE KINGDOM OF THE NETHERLANDS
Number of pages
11
Pages from-to
131-141
UT code for WoS article
000362139400009
EID of the result in the Scopus database
2-s2.0-84938987249