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 …

The present kinematics in the eastern Mediterranean and Middle East is now well
constrained by GPS measurements and dominated by a circular counterclockwise motion …

The Aegean region is a concentrate of the main geodynamic processes that shaped the
Mediterranean region: oceanic and continental subduction, mountain building, high …

Field observations collected during the Sino‐French Himalaya‐Tibet cooperation project
(1980–1982) show that right‐lateral faulting between southern and northern Tibet, roughly …

We present geological and morphological observations at different scales to constrain rates
of faulting and the distribution of deformation in the seismically active Aegean region. We …

This article presents equations for the estimation of horizontal strong ground motions caused
by shallow crustal earthquakes with magnitudes M w≥ 5 and distance to the surface …

This paper presents the overall procedure followed in order to assemble the most recent pan-
European strong-motion databank: Reference Database for Seismic Ground-Motion in …

We use a new satellite laser ranging/Global Positioning System (SLR/GPS) solution at
seven sites in Anatolia and Aegea to obtain a better definition of the extrusion motion of the …

Displacement contour diagrams constructed using seismic reflection data and coal-mine
plans are analysed to establish the factors determining the dimensions, shapes and …

Summary In the Hellenic Trench south of Crete convergence between the southern Aegean
Sea and Africa occurs at a rate of at least 60 mm yr− 1. Previously published first motion fault …