Recent measurements of surface vertical displacements of the European Alps show a
correlation between vertical velocities and topographic features, with widespread uplift at …

Abstract The European Alps are the site where classic geologic concepts such as nappe
theory, continental subduction and slab breakoff have been first proposed. However, the …

Abstract The Dora‐Maira massif is an archetypal nappe stack of subducted and exhumed
upper crust. Slices of continental crust experienced metamorphism at upper blueschist to …

SUMMARY A full understanding of the dynamics of mountain ranges such as the Alps
requires the integration of available geological and geophysical knowledge into a …

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 …

After the onset of plate collision in the Alps, at 32–34 Ma, the deep structure of the orogen is
inferred to have changed dramatically: European plate break-offs in various places of the …

Mediterranean tectonics since the Lower Cretaceous has been characterized by a
multiphase subduction and collision history with temporally and spatially variable, small …

A new method for modeling the thermal structure of the lithosphere, termed thermal isostasy,
is presented and used to calculate the lithosphere thickness and to predict geothermal heat …

Taking benefit of the AlpArray temporary network and permanent networks in W‐Europe, we
construct a 3‐D onshore‐offshore velocity model of the crust and upper mantle using …

SWinvert is a workflow developed at The University of Texas at Austin for the inversion of
surface wave dispersion data. SWinvert encourages analysts to investigate inversion …