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Statements

Subject Item
n2:RIV%2F00216208%3A11320%2F12%3A10126823%21RIV13-GA0-11320___
rdf:type
n14:Vysledek skos:Concept
rdfs:seeAlso
http://dx.doi.org/10.1007/s11200-011-0482-7
dcterms:description
The western part of the Corinth Gulf attracts attention clue to its seismically active fault system and considerable seismic hazard. A moderate size earthquake occurred close to the town of Efpalio on January 18, 2010, followed by a sequence of smaller earthquakes. In the present paper we use this sequence to derive a local structural model for the region in the vicinity of Efpalio. The model is based on the minimization of travel-time residuals. In particular, we used arrival times from 51 selected events recorded 017 January 19 and 20 by at least 5 stations at epicentral distances less than about 25 kin. A variant of the method of conjugate gradients has been used for this purpose. In comparison with several previous models, the new model is characterized by higher velocities to a depth of about 8 km. The velocity ratio in the model is upsilon(P)/upsilon(S) = 1.83. The hypocentres of the selected earthquakes lay at depths between about 5 and 9 km, but their distribution is rather irregular. The western part of the Corinth Gulf attracts attention clue to its seismically active fault system and considerable seismic hazard. A moderate size earthquake occurred close to the town of Efpalio on January 18, 2010, followed by a sequence of smaller earthquakes. In the present paper we use this sequence to derive a local structural model for the region in the vicinity of Efpalio. The model is based on the minimization of travel-time residuals. In particular, we used arrival times from 51 selected events recorded 017 January 19 and 20 by at least 5 stations at epicentral distances less than about 25 kin. A variant of the method of conjugate gradients has been used for this purpose. In comparison with several previous models, the new model is characterized by higher velocities to a depth of about 8 km. The velocity ratio in the model is upsilon(P)/upsilon(S) = 1.83. The hypocentres of the selected earthquakes lay at depths between about 5 and 9 km, but their distribution is rather irregular.
dcterms:title
Upper crustal structure of the western Corinth Gulf, Greece, inferred from arrival times of the January 2010 earthquake sequence Upper crustal structure of the western Corinth Gulf, Greece, inferred from arrival times of the January 2010 earthquake sequence
skos:prefLabel
Upper crustal structure of the western Corinth Gulf, Greece, inferred from arrival times of the January 2010 earthquake sequence Upper crustal structure of the western Corinth Gulf, Greece, inferred from arrival times of the January 2010 earthquake sequence
skos:notation
RIV/00216208:11320/12:10126823!RIV13-GA0-11320___
n14:predkladatel
n22:orjk%3A11320
n4:aktivita
n13:P n13:Z
n4:aktivity
P(GAP210/11/0854), Z(MSM0021620860)
n4:cisloPeriodika
4
n4:dodaniDat
n10:2013
n4:domaciTvurceVysledku
n9:4517989 n9:8519153
n4:druhVysledku
n15:J
n4:duvernostUdaju
n17:S
n4:entitaPredkladatele
n16:predkladatel
n4:idSjednocenehoVysledku
176146
n4:idVysledku
RIV/00216208:11320/12:10126823
n4:jazykVysledku
n6:eng
n4:klicovaSlova
1-D model; conjugate gradients; Corinth Gulf; Greece; arrival times; crustal structure
n4:klicoveSlovo
n8:Greece n8:1-D%20model n8:conjugate%20gradients n8:Corinth%20Gulf n8:arrival%20times n8:crustal%20structure
n4:kodStatuVydavatele
CZ - Česká republika
n4:kontrolniKodProRIV
[A099CF7E76CB]
n4:nazevZdroje
Studia Geophysica et Geodaetica
n4:obor
n20:DC
n4:pocetDomacichTvurcuVysledku
2
n4:pocetTvurcuVysledku
3
n4:projekt
n18:GAP210%2F11%2F0854
n4:rokUplatneniVysledku
n10:2012
n4:svazekPeriodika
56
n4:tvurceVysledku
Novotný, Oldřich Sokos, Efthimios Plicka, Vladimír
n4:wos
000311588500007
n4:zamer
n5:MSM0021620860
s:issn
0039-3169
s:numberOfPages
12
n11:doi
10.1007/s11200-011-0482-7
n12:organizacniJednotka
11320