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 …

A combined analysis of the geodetic strain-rate field and the strain-rate field deduced from
the seismicity allows us to define the style of deformation and to distinguish seismic from …

The central area of the Ionian Islands is dominated by the existence of a major tectonic
structure called the Cephalonia Transform Fault (CTF). Its main part (Cephalonia segment) …

This study provides a multi-disciplinary overview of the seismology and geodetic data with
tectonics analysis in order to provide an evaluation of stress trajectories, and probabilistic …

A detailed study of the active crustal deformation in the Aegean sea and surrounding area is
presented. The estimation of the deformation velocities is not performed in broad seismic …

We use the combined GPS velocity field of the eastern Mediterranean for the period 1988 to
1996 to determine crustal deformation strain rates in a region comprising the Hellenic arc …

Fault plane solutions for 127 earthquakes, of magnitude M 2 55 and shallow focal depth (h-
60 km), which occurred in the Aegean Sea and surrounding area (34 N-43 N, 18 E-30" E) …

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 30 October 2020 Samos earthquake (Mw 7.0) ruptured an east–west striking,
north dipping normal fault located offshore the northern coast of Samos Island, previously …

We used the focal mechanisms of crustal earthquakes (depth< 40 km) in the period 1909–
2012 and the available GPS velocities, derived from the data collected between 1999 to …