Dispersion of Love waves from the 2010 Efpalio earthquake in the Corinth Gulf region, Greece

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F15%3A10314792" target="_blank" >RIV/00216208:11320/15:10314792 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1007/s10950-015-9492-1" target="_blank" >http://dx.doi.org/10.1007/s10950-015-9492-1</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s10950-015-9492-1" target="_blank" >10.1007/s10950-015-9492-1</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Dispersion of Love waves from the 2010 Efpalio earthquake in the Corinth Gulf region, Greece

Popis výsledku v původním jazyce

A moderate size earthquake occurred close to the town of Efpalio in the Corinth Gulf region on January 18, 2010. In the present paper, we have used this earthquake to study the dispersion of short-period Love waves along nine paths in a broader vicinityof the Corinth Gulf. The observed group velocities require very low S-wave velocities in the uppermost 2-km depth. This structural feature differs distinctly from most previous models that were derived from arrival times of body waves in the region. Moreover, it was recognized that the observed group velocities were relatively low for western paths, and medium velocities were observed in the central part of the region, and the highest velocities in its eastern part.

Název v anglickém jazyce

Dispersion of Love waves from the 2010 Efpalio earthquake in the Corinth Gulf region, Greece

Popis výsledku anglicky

A moderate size earthquake occurred close to the town of Efpalio in the Corinth Gulf region on January 18, 2010. In the present paper, we have used this earthquake to study the dispersion of short-period Love waves along nine paths in a broader vicinityof the Corinth Gulf. The observed group velocities require very low S-wave velocities in the uppermost 2-km depth. This structural feature differs distinctly from most previous models that were derived from arrival times of body waves in the region. Moreover, it was recognized that the observed group velocities were relatively low for western paths, and medium velocities were observed in the central part of the region, and the highest velocities in its eastern part.

Druh

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

CEP obor

DC - Seismologie, vulkanologie a struktura Země

OECD FORD obor

—

Projekt

<a href="/cs/project/LM2010008" target="_blank" >LM2010008: CzechGeo/EPOS ? Distribuovaný systém observatorních a terénních měření geofyzikálních polí v České republice</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název periodika

Journal of Seismology

ISSN

1383-4649

e-ISSN

—

Svazek periodika

19

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

6

Strana od-do

801-806

Kód UT WoS článku

000355694300010

EID výsledku v databázi Scopus

2-s2.0-84930380825