The AlpArray programme is a multinational, European consortium to advance our
understanding of orogenesis and its relationship to mantle dynamics, plate reorganizations …

The surface of the Earth is the ever-changing expression of the dynamic processes
occurring at depth and at or above its surface. However, our ability to “read” landscapes in …

A large data set of surface wave phase velocity measurements is compiled to study the
structures of the crust and upper mantle underneath the Alpine continental collision zone …

We present the first three‐dimensional (3D) anisotropic teleseismic P‐wave tomography
model of the upper mantle covering the entire Central Mediterranean. Compared to isotropic …

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 …

An accurate survey of old and new datasets allowed us to probe the nature and role of fluids
in the seismogenic processes of the Apennines mountain range in Italy. New datasets …

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 …

The topography of orogenic belts responds to several contributions operating at short and
long temporal and spatial (ie, wavelengths) scales, from the surface to the deep mantle …

The elevation of an orogenic belt is commonly related to crustal/lithosphere thickening.
Here, we discuss the Apennines as an example to show that topography at a plate margin …

Investigating rock‐uplift variations in time and space provides insights into the processes
driving mountain‐belt evolution. The Apennine Mountains of Italy underwent substantial …