... of the surrounding Aegean region. The stratigraphy (relative position, 3D geometry, dating) of these deposits is still subject to controversies. The syn-rift evolution of the central part of the southern coast of the Corinth rift is revisited, based on new sedimentological and paleontological data. While ostracods...

...Figure 1. Index map of the eastern Gulf of Corinth region, central Greece. P—Perachora Peninsula; C—Corinth; Is—Isthmus of Corinth. ...

...Alan Wood; Douglas Paton; Richard Collier; Viki O’Connor Abstract A major challenge when exploring for hydrocarbons in frontier areas is a lack of data coverage. Data may be restricted to regional-scale 2D seismic lines, from which assumptions of the 3D geometric configuration are drawn...

...R. E. LI. COLLIER; C. J. DART Abstract Normal faulting, regional uplift and glacio-eustacy have controlled patterns of sedimentation on a variety of scales during the active rift history of the Corinth Basin. Extensive sections through 800 m of early rift deposits are exposed in the north...

... in the Corinth-Saronikos region during 1861 to 1975. 02 11 1984 Copyright © 1985, by the Seismological Society of America References Bollinger G. A. (1977) . Reinterpretation of the intensity data for the 1886 Charleston, South...

... traces, indicates how interpretation of the elongation or ellipticity of the isoseismal lines in terms of the orientation of the causative fault may lead to misleading interpretation. Similarity of this composite isoseismal map with the published map for the 1861 earthquake in the Gulf of Corinth region...

... of fault slip. The envisaged mechanism for this regional component of uplift and the Quaternary rifting of the Gulf of Corinth is Aegea being pushed over the hinge of the steeply dipping section of the subducted African plate (Fig. 1 c) onto the shallow-dipping section below the Peloponnese. Isostatic...

... interglacial; a much larger reduction was obtained for scenario 3. We infer from this that catchments in the Corinth Rift must have a response time of ∼10 4 yrs for this signal to be observed in the basin. Our finding that sediment routing systems at a regional scale are sensitive to climate change...

... structure of the Achaia earthquake. The first Efpalio event ruptured a mapped normal fault that trends east‐northeast–west‐southwest, dipping 55°–60° to the south. We estimate ∼2‐fold seismicity rate changes in the western Corinth gulf region for the interseismic period (June 2008–January 2010), and we find...

... and strain localization across the boundary; the Corinth rift. We are able to constrain the spatial and time framework of rift-climax deepening as follows. Local and regional paleocurrents ( Fig. 2 ) ( Rohais et al., 2007 ) indicate that R-DF turbidites were derived from the west, via the Killini...

...) , Duverger et al. (2018) , and references therein. The Corinth rift (central Greece) is a Quaternary graben characterized by ∼east–west normal faulting. The western Gulf of Corinth (WGoC) is its most active region (Fig.  1 ), with an extension rate reaching 15    mm · yr − 1 across...