Understanding the behavior of fluids in seismically active faults and their chemical-physical
(dis) equilibrium with the host rock is important to understand the role of fluids upon …

We investigate the processes driving spatial-temporal patterns of Cenozoic exhumation in
the Mediterranean and the Middle East by compiling> 7300 published low-temperature …

The central Apennines are a fold-thrust belt currently affected by post-orogenic extensional
seismicity. To constrain the influence that the inherited thrust-related structures exert on the …

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 …

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

The evolution of the Apennine wedge has seen the time‐space migration of the forebulge,
foredeep, thrust wedge, and back‐arc extension phases in the wake of the Eastward …

Evidence from landscape evolution may provide critical constraints for past geodynamic
processes, but has been limited by the large uncertainties of topographic reconstructions …

Drainage network systems are responsive elements to recent active tectonics from among
all the topographic features. In geodynamically active areas, fluvial landscapes can record …

The evolution of topography in forearc regions results from the complex interplay of crustal
and mantle processes. The Southern Apennines represent a well‐studied forearc region that …

This paper discusses the response of topography and river networks to non-uniform
lithology and tectonic forcing in the Umbria-Marche sector of the Apennines fold and thrust …