Negative structural inversion: An overview
The same sense movement on any given fault plane occurs much more frequently
compared to the cases when the sense reverses. Therefore, positive or negative structural …
compared to the cases when the sense reverses. Therefore, positive or negative structural …
Structural architecture of the central Apennines: Interpretation of the CROP 11 seismic profile from the Adriatic coast to the orographic divide
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 …
reflection seismic profile 265 km long that cuts across the central Apennines from the …
The anatomy of the 2009 L'Aquila normal fault system (central Italy) imaged by high resolution foreshock and aftershock locations
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 …
the Abruzzo region in central Italy. We study the geometry of fault segments using high …
Tectono-stratigraphic evolution of the offshore Apulian Swell, a continental sliver between two converging orogens (Northern Ionian Sea, Central Mediterranean)
Abstract The Calabrian Arc subduction complex, in the northern Ionian Sea, is facing directly
the westward subducting Apulian Swell, a sliver of continental crust covered by about 8 km …
the westward subducting Apulian Swell, a sliver of continental crust covered by about 8 km …
The impact of structural complexity, fault segmentation, and reactivation on seismotectonics: Constraints from the upper crust of the 2016–2017 Central Italy seismic …
Young and tectonically active chains like the Central Apennines (Italy) are featured by high
structural complexity as a result of the overprint of subsequent deformational stages, making …
structural complexity as a result of the overprint of subsequent deformational stages, making …
Slab retreat and active shortening along the central-northern Apennines
The Quaternary geodynamic evolution and the tectonic processes active along the Central
and Northern Apennines thrust fronts and in the adjacent Padane-Adriatic foredeep domains …
and Northern Apennines thrust fronts and in the adjacent Padane-Adriatic foredeep domains …
Large earthquakes driven by fluid overpressure: The Apennines normal faulting system case
Fluid overpressure is a primary mechanism behind fault interaction and earthquakes
triggering. The Apennines section within the young Alpine mobile belt is a key locus to …
triggering. The Apennines section within the young Alpine mobile belt is a key locus to …
Thrust front segmentation induced by differential slab retreat in the Apennines (Italy)
D Scrocca - Terra Nova, 2006 - Wiley Online Library
New seismic reflection data reveal that the south‐eastward prolongation of the Apennine
thrust front in the central Adriatic Sea is most likely located in a more external position with …
thrust front in the central Adriatic Sea is most likely located in a more external position with …
Structure of a normal seismogenic fault zone in carbonates: the Vado di Corno Fault, Campo Imperatore, Central Apennines (Italy)
Abstract The Vado di Corno Fault Zone (VCFZ) is an active extensional fault cutting through
carbonates in the Italian Central Apennines. The fault zone was exhumed from∼ 2 km depth …
carbonates in the Italian Central Apennines. The fault zone was exhumed from∼ 2 km depth …
Positive inversion tectonics in foreland fold-and-thrust belts: A reappraisal of the Umbria–Marche Northern Apennines (Central Italy) by integrating geological and …
V Scisciani, S Agostini, F Calamita, P Pace, A Cilli… - Tectonophysics, 2014 - Elsevier
Unraveling the tectonic style in the outer zones of fold-and-thrust belts is generally puzzling
because the basement–cover relationships are often hidden in the subsurface as in the …
because the basement–cover relationships are often hidden in the subsurface as in the …