[PDF][PDF] Geology of the southern Apennines
E Patacca, P Scandone - Bollettino della Società Geologica …, 2007 - researchgate.net
This paper aims to provide a concise description of the geology of the Southern Apennines
especially useful for readers having scarce familiarity with this complex region. The text is …
especially useful for readers having scarce familiarity with this complex region. The text is …
Spatial and temporal variations in growth rates along active normal fault systems: an example from The Lazio–Abruzzo Apennines, central Italy
GP Roberts, AM Michetti - Journal of Structural Geology, 2004 - Elsevier
The geometry, kinematics and rates of active extension in Lazio–Abruzzo, Italian Apennines,
have been measured in order to gain a better understanding of the spatial and temporal …
have been measured in order to gain a better understanding of the spatial and temporal …
[PDF][PDF] Geology of the central Apennines: a regional review
D Cosentino, P Cipollari, P Marsili… - Journal of the virtual …, 2010 - researchgate.net
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 …
sedimentary wedge developed on the southern Neotethyan passive margin. On the previous …
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 …
Sedimentary and tectonic evolution of Plio–Pleistocene alluvial and lacustrine deposits of Fucino Basin (central Italy)
GP Cavinato, C Carusi, M Dall'Asta, E Miccadei… - Sedimentary …, 2002 - Elsevier
The Fucino Basin was the greatest lake of the central Italy, which was completely drained at
the end of 19th century. The basin is an intramontane half-graben filled by Plio–Quaternary …
the end of 19th century. The basin is an intramontane half-graben filled by Plio–Quaternary …
Seismic reflection profiles and subsurface geology of the area interested by the 2016–2017 earthquake sequence (Central Italy)
Starting from 24 August 2016, a long seismic sequence, including nine Mw> 5.0
earthquakes, struck a wide area of the Central Italy. A large amount of geological, geodetic …
earthquakes, struck a wide area of the Central Italy. A large amount of geological, geodetic …
Architecture and evolution of an extensionally-inverted thrust (Mt. Tancia Thrust, Central Apennines): Geological, structural, geochemical, and K–Ar geochronological …
Fault inversion may lead to significant obliteration of earlier tectonic structures, thus
preventing the straightforward interpretation of the complete kinematics and deformation …
preventing the straightforward interpretation of the complete kinematics and deformation …
[PDF][PDF] Kinematic evolution of the Volsci Range: a new overview
E Centamore, P Di Manna, D Rossi - BOLLETTINO-SOCIETA …, 2007 - academia.edu
Kinematic evolution of the Volsci Range: a new overview Page 1 ABSTRACT The Volsci
Range, in the central Apennines of peninsular Italy, object of this contribution, has recently …
Range, in the central Apennines of peninsular Italy, object of this contribution, has recently …
Looking into the entanglement between karst landforms and fault activity in carbonate ridges: the Fibreno fault system (Central Italy)
The entanglement between active tectonics and karst systems is well-known in the literature.
Karst systems are sound recorders of continental deformation in terms of brittle structures …
Karst systems are sound recorders of continental deformation in terms of brittle structures …
Morphostructural elements of central–eastern Abruzzi: Contributions to the study of the role of tectonics on the morphogenesis of the Apennine chain
L D'Alessandro, E Miccadei, T Piacentini - Quaternary International, 2003 - Elsevier
The relief features of the Apennine chain have been developed in a complex
geomorphological and geological evolution from Neogene to Quaternary. In order to define …
geomorphological and geological evolution from Neogene to Quaternary. In order to define …