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 …

Crustal rheology controls the style of rifting and ultimately the architecture of rifted margins.
Here we review the formation of three magma-poor margin pairs, Iberia-Newfoundland, the …

Many rifts develop through multiphase extension; it can be difficult, however, to determine
how strain is distributed during reactivation because structural and stratigraphic evidence …

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 onshore central Corinth rift contains a syn‐rift succession> 3 km thick deposited in 5–15
km‐wide tilt blocks, all now inactive, uplifted and deeply incised. This part of the rift records …

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 …

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 …

Displacements on tectonic faults primarily accrue during earthquakes at rates that vary
through time. To examine the processes that underlie the temporal changes in fault …

The need to predict accurately the volume, timing and location of sediments that are
transported from an erosional source region into a basin-depocentre sink is important for …