"Upper crustal structure of the western Corinth Gulf, Greece, inferred from arrival times of the January 2010 earthquake sequence"@en . "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."@en . . "Upper crustal structure of the western Corinth Gulf, Greece, inferred from arrival times of the January 2010 earthquake sequence"@en . "Upper crustal structure of the western Corinth Gulf, Greece, inferred from arrival times of the January 2010 earthquake sequence" . . "Novotn\u00FD, Old\u0159ich" . "Sokos, Efthimios" . "000311588500007" . "Upper crustal structure of the western Corinth Gulf, Greece, inferred from arrival times of the January 2010 earthquake sequence" . . . "10.1007/s11200-011-0482-7" . "11320" . "RIV/00216208:11320/12:10126823!RIV13-GA0-11320___" . . . . "Studia Geophysica et Geodaetica" . . . "176146" . "[A099CF7E76CB]" . . "RIV/00216208:11320/12:10126823" . "2"^^ . . "3"^^ . . "12"^^ . . . . . . "4" . "CZ - \u010Cesk\u00E1 republika" . "1-D model; conjugate gradients; Corinth Gulf; Greece; arrival times; crustal structure"@en . "Plicka, Vladim\u00EDr" . "http://dx.doi.org/10.1007/s11200-011-0482-7" . "P(GAP210/11/0854), Z(MSM0021620860)" . . . "56" . . . "0039-3169" .