E Serpelloni, A Cavaliere, L Martelli, F Pintori… - Frontiers in Earth …, 2022 - frontiersin.org
In this work we present and discuss new geodetic velocity and strain-rate fields for the Euro- Mediterranean region obtained from the analysis of continuous GNSS stations. We describe …
The western Mediterranean recorded subduction rollback, slab segmentation and separation. Here we address the questions of what caused Oligocene rollback initiation, and …
F Antonioli, L Ferranti, P Stocchi, G Deiana… - Earth-Science …, 2018 - Elsevier
We report detailed morphometric observations on several MIS 5.5 and a few older (MIS 11, 21, 25) fossil tidal notches shaped along carbonate coasts at 80 sites in the central …
Abstract The Apennines-Sicilian-Maghrebian fold-and-thrust belt originated from the subduction of the Alpine Tethys and the later collision of drifted continental blocks against …
One of the most conspicuous features of a mountain belt is the main drainage divide. Divide location is influenced by a number of parameters, including tectonic uplift and horizontal …
In the western Mediterranean, following the intervening continent-continent collision, the subduction of the Tethyan ocean has progressively come to an end or almost in large …
The global sea-level rise (SLR) projections for the next few decades are the basis for developing flooding maps that depict the expected hazard scenarios. However, the spatially …
Abstract The Calabrian Arc is a narrow subduction–rollback system resulting from Africa/Eurasia plate convergence. While crustal shortening is taken up in the accretionary …
Subduction of a narrow slab of oceanic lithosphere beneath a tightly curved orogenic arc requires the presence of at least one lithospheric scale tear fault. While the Calabrian …