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 Iberian Peninsula and the Maghreb experience moderate earthquake activity and
oblique,∼ NW–SE convergence between Africa and Eurasia at a rate of∼ 5 mm/yr. Coeval …

We present a description of the characteristics of the seismic deformation occurring in the
Alpine Mediterranean Belt, and outline its association with tectonic and geologic features …

The North Anatolian fault (NAF) extends over 1500 km in a complex tectonic setting. In this
region of the eastern Mediterranean, collision of the Arabian, African and Eurasian plates …

It is argued that the Plio-Quaternary deformation pattern in the Mediterranean region is
compatible with a SSWNNE convergence between Africa (Nubia) and Eurasia and that the …

We argue that seismotectonic activity in the Central Mediterranean area and the Aegean–
Balkan zone is driven by the NNE-ward motion of Africa and westward motion of Anatolia …

The hypothesis that trench-arc-back arc migrating systems in the Mediterranean area
developed as extrusion processes, driven by the convergence of the confining plates, ie …

The Aegean–Hellenic arc is a deformed sector of a long heterogeneous orogenic system
(Tethyan belt), constituted by an inner old metamorphic crystalline core flanked by younger …

In this study, the GNSS and gravity data were processed and compared together for
examining the continental structures of the Western Anatolia region which has very …

An attempt at quantifying post-seismic relaxation triggered by decoupling earthquakes along
the eastern thrusting border of the Adriatic plate (southern Dinarides) is carried out by finite …