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

We present a new global model of plate motions and strain rates in plate boundary zones
constrained by horizontal geodetic velocities. This Global Strain Rate Model (GSRM v. 2.1) …

This study presents relative sea level (RSL) curves for seven coastal areas in Akarnania and
the northwestern Peloponnese (NW Greece) since the mid-Holocene. RSL fluctuations are …

In this paper we present a global model (GSRM-1) of both horizontal velocities on the Earth's
surface and horizontal strain rates for almost all deforming plate boundary zones. A model …

We present a new geodetic velocity solution for Italy and the surrounding areas, obtained
from an analysis of continuous and survey-mode Global Positioning System observations …

We calculate and analyse the coordinate time-series of 282 permanent GPS stations located
in Greece and 47 in surrounding countries. The studied period is 2000–2020. The average …

Site velocities from six separate Global Positioning System (GPS) networks comprising 374
stations have been referred to a single common Eurasia‐fixed reference frame to map the …

We use the GPS velocity field (1988–1998) for eastern Mediterranean and Asia Minor to
determine the crustal deformation strain rate field in an area bounded by 35° N and 43° N …

Crustal deformation and seismicity in Europe are still poorly understood. Seismic activity is
classically ascribed to crustal strain rates generated by edge‐driven tectonic forces …

The Hellenic plate boundary region, located in the collision zone between the
Nubian/Arabian and Eurasian lithospheric plates, is one of the seismo-tectonically most …