The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …

Alps and Apennines developed along opposite subductions, which inverted the tethyan
passive continental margins located along the boundaries of Europe, Africa and the Adriatic …

Carbonate clumped isotope thermometry is based on the preference of 13C and 18O to form
bonds with each other. At elevated temperatures such bond ordering is susceptible to …

Solid-state reordering of C–O bonds in the calcite lattice can alter the clumped isotope
composition of paleotemperature archives such as fossil brachiopod shells without inducing …

We integrate existing and new geologic data [REtreating TRench, Extension, and Accretion
Tectonics (RETREAT project)], particularly on the origin, growth, and activity of the mountain …

Several small pyrite±baryte±iron-oxide orebodies (Buca della Vena, Canale della Radice,
Fornovolasco, Monte Arsiccio and Pollone) are hosted in the metamorphic rocks of the …

Isotropic and anisotropic seismic structures across the Northern Apennines (Italy)
subduction zone are imaged using a new method for the analysis of teleseismic receiver …

Abstract The Alps/Apennines system, as well as many collisional orogens through the world,
shows a finite deformation produced during a long geological history which involves …

Abstract Three samples of (Tl, Sb, As)-rich pyrite from the ore deposits of the southern Apuan
Alps (Tuscany, Italy) were studied through a multi-technique approach in order to constrain …

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 …