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 …

This paper presents a synthesis of the neotectonic studies performed in mainland Portugal
that address the “recent”(post Piacenzian,~ 3 Ma) tectonic evolution of the Portuguese …

Summary The Western Mediterranean displays a complex pattern of crustal deformation
distributed along tectonically active belts developed in the framework of slow oblique plate …

Marine gateways play a critical role in the exchange of water, heat, salt and nutrients
between oceans and seas. As a result, changes in gateway geometry can significantly alter …

A unique GPS velocity field that spans the entire Southeast Asia region is presented. It is
based on 10 years (1994–2004) of GPS data at more than 100 sites in Indonesia, Malaysia …

The missing link in the plate boundary between Eurasia and Africa in the central Atlantic is
presented and discussed. A set of almost linear and sub parallel dextral strike–slip faults, the …

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 …

The Rif Belt belongs to a much larger orogen, ie the Betic-Rif-Tell orogen, which itself is part
of the still larger Mediterranean Alpine belts (Fig. 5.1; see also Chap. 1.1, Fig. 1.2). The Rif …

We investigate crustal deformation along the Eurasia‐Nubia plate boundary in Calabria and
Sicily revealed by the GPS velocity field obtained by the combination of continuous site …