2015
DOI: 10.5194/se-6-173-2015
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High-precision relocation of seismic sequences above a dipping Moho: the case of the January–February 2014 seismic sequence on Cephalonia island (Greece)

Abstract: Abstract. Detailed velocity structure and Moho mapping is of crucial importance for a high precision relocation of seismicity occurring out of, or marginal to, the geometry of seismological networks. Usually the seismographic networks do not cover the boundaries of converging plates such as the Hellenic arc. The crustal thinning from the plate boundary towards the back-arc area creates significant errors in accurately locating the earthquake, especially when distant seismic phases are included in the analysis.… Show more

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Cited by 39 publications
(27 citation statements)
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“…This choice is based on the fact that this epicenter: a) is supported by the first-motion polarities at near station DMLN (Z+, N+, E+), which imply that the epicenter lies south-west of the station and b) is in agreement with the provisions imposed by the collocation of hypocenter and fault plane position . Our preferred solution is in disagreement with the relocations proposed by other authors (Karakostas et al, 2014;Karastathis et al, 2015), which are closer to our epicenter obtained from the local data.…”
Section: The 26 January 2014 Eventcontrasting
confidence: 63%
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“…This choice is based on the fact that this epicenter: a) is supported by the first-motion polarities at near station DMLN (Z+, N+, E+), which imply that the epicenter lies south-west of the station and b) is in agreement with the provisions imposed by the collocation of hypocenter and fault plane position . Our preferred solution is in disagreement with the relocations proposed by other authors (Karakostas et al, 2014;Karastathis et al, 2015), which are closer to our epicenter obtained from the local data.…”
Section: The 26 January 2014 Eventcontrasting
confidence: 63%
“…This test also showed that the epicenter defined by the use of the local stations (Fig. 2a), close to that of Karastathis et al (2015), is much less favored. This stems from the fact that even a large increase in the depth still leaves the hypocenter distance from the fault too large (~5 km) and, moreover, such a hypocenter would project closer to the conjugate WNW-ESE trending nodal plane.…”
Section: The 26 January 2014 Eventmentioning
confidence: 85%
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