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 …

We use improved focal mechanisms and centroid depth estimates of earthquakes, combined
with GPS velocities, to examine the tectonics of the Hellenic subduction zone, and in …

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

The present study aims to suggest an approach that allows the simultaneous hazard
zonation mapping of earthquake-induced secondary effects. The modeling process of the …

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 …

We processed data from~ 100 continuous GPS stations to provide new insights into the
crustal motion and deformation of central and western Greece. We used the derived velocity …

Abstract The Cenozoic East African Rift System (EARS) extends from the Red Sea to
Mozambique. Here we use seismic reflection and bathymetric data to investigate the tectonic …

From the apex of the NW Sub-basin of the South China Sea, we present new long-cable
deep-penetration seismic profiles and deepwater drillings together with corrected seismic …

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 …