We perform the finite‐extent fault inversion of the three main events of the 2016 Central Italy
seismic sequence using near‐source strong motion records. We demonstrate that both …

Page 1 Special Paper 469 Page 2 Page 3 Geology and Tectonic Evolution of the Central-Southern
Apennines, Italy by Livio Vezzani Dipartimento di Scienze della Terra Università di Torino …

Mesoscale deformation in fold-thrust belts and foreland areas occurs during the interaction
of evolving stress regimes and mechanical stratigraphy, leading to a progressive …

Fractures can play an important role in the fluid storage–migration properties of fault
damage zones. In this present contribution, we document the role exerted by fractures on …

We studied the mechanisms and intensity of deformation across a large, active, basin-
bounding normal fault zone in Mesozoic platform carbonates. Based on the modes …

We documented the porosity, permeability, pore geometry, pore type, textural anisotropy,
and capillary pressure of carbonate rock samples collected along basin‐bounding normal …

The Tyrrhenian margin of central Italy has undergone Plio‐Quaternary extension,
developing NW‐SE normal faults and NE‐SW faults. The NE‐SW faults decrease in …

The multideformed axial zone of the Apennines provides a great opportunity to explore the
influence of pre-existing cross-structures (inherited from pre-Quaternary tectonic phases) on …

On 6 April 2009, a Mw= 6.3 earthquake occurred in the central Apennines (Italy) damaging
the city of L'Aquila and the surrounding country. We relocate the October 2008 to 6 April …

Terra Nova, 22, 43–51, 2010 Abstract An earthquake of Mw= 6.3 struck L'Aquila town
(central Italy) on 6 April 2009 rupturing an∼ 18‐km‐long SW‐dipping normal fault. The …