Rupture process of the 2014 Cephalonia, Greece, earthquake doublet (Mw6) as inferred from regional and local seismic data

Kód výsledku v 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>

Nalezeny alternativní kódy

RIV/61989100:27350/15:86095115 RIV/00025615:_____/15:#0002177

Výsledek na webu

<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>

Jazyk výsledku

angličtina

Název v původním jazyce

Rupture process of the 2014 Cephalonia, Greece, earthquake doublet (Mw6) as inferred from regional and local seismic data

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

Rupture process of the 2014 Cephalonia, Greece, earthquake doublet (Mw6) as inferred from regional and local seismic data

Popis výsledku anglicky

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.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DC - Seismologie, vulkanologie a struktura Země

OECD FORD obor

—

Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Tectonophysics

ISSN

0040-1951

e-ISSN

—

Svazek periodika

656

Číslo periodika v rámci svazku

August

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

11

Strana od-do

131-141

Kód UT WoS článku

000362139400009

EID výsledku v databázi Scopus

2-s2.0-84938987249