We review the geodynamic evolution of the Aegean–Anatolia region and discuss strain
localisation there over geological times. From Late Eocene to Present, crustal deformation in …

Shoreline and shelf‐edge trajectories describe the migration through time of sedimentary
systems, using geomorphological breaks‐in‐slope that are associated with key changes in …

Abstract The Corinth Rift, central Greece, enables analysis of early rift development as it is
young (< 5 Ma) and highly active and its full history is recorded at high resolution by …

The style of extension and strain distribution during the early stages of intra‐continental
rifting is important for understanding rift‐margin development and can provide constraints for …

Abstract The Corinth rift (Greece) is one of the world's most active rifts. The early Plio‐
Pleistocene rift is preserved in the northern Peloponnese peninsula, south of the active …

Gilbert‐type deltas are sensitive recorders of short‐term base‐level changes, but the delta‐
front record of a base‐level rise tends to be erased by fluvial erosion during a subsequent …

Abstract The Kerinitis Delta in the Corinth Rift, Greece, is a footwall derived, coarse‐grained,
Gilbert‐type fan delta deposited in the hangingwall of a linked normal fault system. This …

The present-day tectonic setting of the Western Mediterranean region, from the Pyrénées to
the Betics and from the Alps to the Atlas, results from a complex 3-D geodynamic evolution …

A multichannel seismic and bathymetry survey of the central and eastern Gulf of Corinth
(GoC), Greece, reveals the offshore fault geometry, seismic stratigraphy and basin evolution …

The coexistence of shortening and extensional tectonic regimes is a common feature in
orogenic belts. The westernmost end of the Western Mediterranean is an area undergoing …