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 …

Integration of new field structural and geophysical data with existing information from the
Apennines chain in Italy and its adjacent Adriatic foreland indicates that the styles of positive …

Mélanges represent a significant component of collisional and accretionary orogenic belts
and occur widely around the world. Since its first introduction and use, the term has evolved …

Defining the structural style of fold–thrust belts and understanding the controlling factors are
necessary steps towards prediction of their long-term and short-term dynamics, including …

The Meso-Cenozoic stratigraphical successions that crop out in central Italy are part of the
sedimentary wedge developed on the southern Neotethyan passive margin. On the previous …

The geological structure of continental lithosphere shows complex variety that is inherited
into orogenic belts and influences the localization and amplification of contractional …

We present an interpretation of the eastern half portion of the CROP 11 line, a deep
reflection seismic profile 265 km long that cuts across the central Apennines from the …

This paper furnishes a brief, but exhaustive, description of the tectonics and stratigraphy of
the Campania region (southern Italy). The attached geological map (Main Map) at 1 …

On 6 April (01: 32 UTC) 2009 a MW 6.1 normal faulting earthquake struck the axial area of
the Abruzzo region in central Italy. We study the geometry of fault segments using high …

We describe how thin‐skinned/thick‐skinned deformation in the Zagros Folded Belt
interacted in time and space. Homogeneous fold wavelengths (15.8±5.3 km), tectono …