The Aegean Sea and its surrounding regions comprise one of the most rapidly deforming
parts of the Alpine-Himalayan mountain belt. Though the deformation of the belt as a whole …

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 …

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 …

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 …

A 66-station GPS network spanning central Greece, first observed in 1989, has been
occupied fully on three occasions: June 1989, October 1991 and May 1993. Subsets of this …

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 …

Results acquired using global positioning system (GPS) data taken over a large part of SE-
Asia, indicate that Sundaland, ie Indochina along with the western and central part of …

The spatial–height analyses of deposits belonging to isotopic substages 5e and 5c indicate
the occurrence of differential uplift in the Gibraltar Strait area. Maximum mean uplift rates do …

Recent crustal movements detected by the analysis of repeated satellite geodetic
measurements reflect the ongoing geodynamic processes in the Alpine-Mediterranean area …

Variations in fluid loads such as the oceans and the atmosphere deform the surface of the
Earth. The accuracy of station coordinates, in particular, heights, that can be estimated …