..., and was probably open to the east. During the second phase, the Gulf of Corinth assumed its present configuration. Sediments related to this second phase were Gilbert-type deltas and deep-sea deposits. During this phase the basin was connected to the Ionian Sea through the Gulf of Patra. This implies...

...D. Sorel Abstract Earthquake seismology requires an active, shallow, low-angle (∼20°) north-dipping normal fault beneath the western Corinth-Patras rift. However, extensional faults that crop out south of the gulf, in northern Peloponnesus, are steeper (40°–50°), and this difference of dip has...

... in the western Gulf of Corinth (Greece) between December 2020 and February 2021. This area is the main focus of the Corinth Rift Laboratory (CRL) network, and has been closely monitored with local seismological and geodetic networks for 20 yr. The 2020–2021 seismic crisis evolved in three stages: It started...

...D. J. W. Piper; A. G. Panagos; G. G. Pe Abstract A flysch succession more than 2 km thick is exposed between the Gulf of Patras and the Lake Trikhonis depression. A monocline repeats the stratigraphic sequence, such that sediments can be correlated for at least 10 km across the depositional strike...

... and tectonism in Eocene marine sediments of the Ainsa basin, Spanish Pyrenees. PhD Thesis, University of Wales, Cardiff. Ferentinos G. Brooks M. Doutsos T. Quaternary tectonics in the Gulf of Patras, Western Greece Journal of Structural Geology 1985 7 713 717 Fleury J. J...

... results, and finally to depict this evolution with a morphodynamic suitable model. In the study area ( fig. 1 ), a master fault known as Northern Peloponnese Major Fault extends from the mainland 3 km away from the coast in correspondence to the Gulf of Patras Fault. To the east, the fault extends...

...Paola Albini; Andrea Rovida; Oona Scotti; Hélène Lyon‐Caen Abstract The area of the western Gulf of Corinth around the city of Aigio (Achaea, northwest Peloponnese, Greece) represents an international pilot site for continuous monitoring and multidisciplinary research on earthquake processes...

... of light shocks (M = 3), with epicenter near the apex of the Gulf of Patras, jolted the Northwest coasts of Peloponnese. These shocks were accompanied by a strong agitation and turbidity of the sea which lasted several days. On 7th February, a strong seismic seawave developed and flooded the coasts...

... , 108 , 2248 – 2264 . Chronis G. Piper D. Anagnostou G. , 1991 , Late Quaternary evolution of the Gulf of Patras, Greece: Tectonism, deltaic sedimentation and sea level change : Marine Geology 0025-3227 , 97 , 191 – 199 . Davies D. L. Bouldin W. , 1979...

...Figure 1. (a) Map showing the tectonic setting in western Greece. Major faults and plate boundaries have been adopted from Papazachos and Papazachou (1997) . KFT , Kefalonia Transformation fault; Kef, Kefalonia Island; Lef, Lefkada Island; Zak, Zakynthos Island; GP , Gulf of Patras; Py, city...

...) belongs to a small network jointly operated by Charles University and Patras University in the western Corinth Gulf since 1997 ( Zahradnik and Tselentis, 1999 ). The main shock and selected M 4 aftershock records are shown in Figure 8 . Three parameters are needed for the EGF summation: the rise...

... at 6°–8°/My by Chousianitis et al. (2015) and 8°/My by Vernant et al. (2014) . This Patras–Achaïa area is limited to the northeast by a zone of left-lateral shear between the Gulf of Amavrakikos and the eastern tip of the Gulf of Corinth. The rate of motion along this zone of shear is estimated...

... of these sediments has been also proposed by correlating them with the basal syn-rift series outcropping in the gulf of Patras (west) and with the sediments in Corinth canal region to the east (fig. 1 ). There, the oldest syn-rift fill has been dated at Middle to Late Pliocene using the faunal and floral assemblages...