2005
DOI: 10.1016/j.jog.2005.07.005
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Palaeoseismic data and their implication for active deformation in Greece

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Cited by 39 publications
(32 citation statements)
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“…Due to this the sea barriers that protect the deltaic plain were destroyed and catastrophic floods have occurred several times. (Chatzipetros et al, 2005;Gounaris et al, 2007;Martinod et al, 1997;Stiros, 2001;Stiros and Drakos, 2000). …”
Section: Sindos-kalochorimentioning
confidence: 99%
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“…Due to this the sea barriers that protect the deltaic plain were destroyed and catastrophic floods have occurred several times. (Chatzipetros et al, 2005;Gounaris et al, 2007;Martinod et al, 1997;Stiros, 2001;Stiros and Drakos, 2000). …”
Section: Sindos-kalochorimentioning
confidence: 99%
“…This horizontal extension was interpreted either as a long-term post-seismic relaxation processes within the graben or as a continuous aseismic slip motion. Based on paleoseismological trenching in different sites within the basin Chatzipetros et al (2005) evidence aseismic creeping with a maximum slip-rate of 2.5 mm.yr and a minimum of 0.7 mm.yr. According these authors aseismic creeping plays a very important role in this area.…”
Section: Mygdonian Grabenmentioning
confidence: 99%
“…Moreover, there is not any evidence that the Helike fault was activated at that time [8]. This suggests that the earthquake responsible for the devastation of Helike was caused by the activation of another of the numerous faults in the Corinth Gulf.…”
Section: Discussionmentioning
confidence: 95%
“…According to Heracleides, Helike was built on the delta plain formed by the above mentioned rivers at a distance of 2 km from the shoreline, near the foothills of the mountains to the south (Figure 2). The delta plain, on which Helike was built, developed on a tilted fault block bounded to the north and south by the Aigion and Helike active faults, respectively [8] (Figures 1 and 2).…”
Section: Geographical-geological Settingmentioning
confidence: 99%
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