The January 2010 Efpalio earthquake sequence in the western Corinth Gulf (Greece)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F12%3A10123788" target="_blank" >RIV/00216208:11320/12:10123788 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/68407700:21110/12:00225607

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.tecto.2012.01.005" target="_blank" >http://dx.doi.org/10.1016/j.tecto.2012.01.005</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.tecto.2012.01.005" target="_blank" >10.1016/j.tecto.2012.01.005</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The January 2010 Efpalio earthquake sequence in the western Corinth Gulf (Greece)

Popis výsledku v původním jazyce

The January 2010 Efpalio earthquake sequence provides some key elements to enhance our view on the western Corinth Gulf tectonics. The sequence lasted almost six months, and included two Mw > 5 strong events, both exhibiting normal faulting along similarto E-W trending planes. This paper attempts to construct a unified seismotectonic model of the sequence jointly interpreting earthquake locations, moment-tensors and slip inversions in terms of the possible activated fault planes. Previous studies haveconnected the prevailing microseismic activity to a major low-angle, north-dipping structure under the Corinth Gulf and the Efpalio sequence favors such a general trend. Moreover, it clearly shows the significance of the shallow activity, so far less recognized, and possibly connected to the relatively steep faults outcropping on the northern coast. The first 18 January 2010 Mw>5 event had almost no on-fault aftershocks and most likely it occurred on a 550 south-dipping nodal plane. The

Název v anglickém jazyce

The January 2010 Efpalio earthquake sequence in the western Corinth Gulf (Greece)

Popis výsledku anglicky

The January 2010 Efpalio earthquake sequence provides some key elements to enhance our view on the western Corinth Gulf tectonics. The sequence lasted almost six months, and included two Mw > 5 strong events, both exhibiting normal faulting along similarto E-W trending planes. This paper attempts to construct a unified seismotectonic model of the sequence jointly interpreting earthquake locations, moment-tensors and slip inversions in terms of the possible activated fault planes. Previous studies haveconnected the prevailing microseismic activity to a major low-angle, north-dipping structure under the Corinth Gulf and the Efpalio sequence favors such a general trend. Moreover, it clearly shows the significance of the shallow activity, so far less recognized, and possibly connected to the relatively steep faults outcropping on the northern coast. The first 18 January 2010 Mw>5 event had almost no on-fault aftershocks and most likely it occurred on a 550 south-dipping nodal plane. The

Druh

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

CEP obor

DC - Seismologie, vulkanologie a struktura Země

OECD FORD obor

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Projekt

<a href="/cs/project/GAP210%2F11%2F0854" target="_blank" >GAP210/11/0854: Prohloubení fyzikálního pohledu na zemětřesení ve Středomoří</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2012

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

530

Číslo periodika v rámci svazku

MARCH

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

11

Strana od-do

299-309

Kód UT WoS článku

000302838900019

EID výsledku v databázi Scopus

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