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 …

I combine recently published GPS results to derive a geodetic horizontal velocity field
consistent at the scale of the Mediterranean and the surrounding Alpine belts. The velocity …

The GPS‐derived velocity field (1988–2005) for the zone of interaction of the Arabian,
African (Nubian, Somalian), and Eurasian plates indicates counterclockwise rotation of a …

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

This paper reviews the main tectonic features of the Eastern Mediterranean region
combining the recent information obtained from GPS measurements, seismicity and …

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 …

Metamorphic core complexes of the Aegean region have revealed midcrustal, shallow‐
dip** extensional shear zones. These shear zones display constant kinematic indicators …

Reviewed by David R. Lentz Department of Geology, University of New Brunswick,
Fredericton, NB and regional experts. Although there is an obvious emphasis on the …

In this paper, we discuss the possibility that the North Anatolian fault (NAF) results from the
deep deformation of the slab beneath the Bitlis–Hellenic subduction zone. We described the …

Using the peri-Mediterranean blueschist belts as a case study we discuss the mechanisms
of syn-orogenic exhumation of high-pressure (HP) and ultra-highpressure (UHP) rocks. The …