[HTML][HTML] Orogenic architecture of the Mediterranean region and kinematic reconstruction of its tectonic evolution since the Triassic

DJJ Van Hinsbergen, TH Torsvik, SM Schmid… - Gondwana …, 2020 - Elsevier
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 …

[HTML][HTML] Geodynamics, geophysical and geochemical observations, and the role of CO2 degassing in the Apennines

F Di Luccio, M Palano, G Chiodini, L Cucci… - Earth-Science …, 2022 - Elsevier
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 …

The anatomy of the 2009 L'Aquila normal fault system (central Italy) imaged by high resolution foreshock and aftershock locations

L Chiaraluce, L Valoroso, D Piccinini… - Journal of …, 2011 - Wiley Online Library
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 …

Classifying curved orogens based on timing relationships between structural development and vertical-axis rotations

AB Weil, AJ Sussman - Orogenic curvature: integrating …, 2004 - books.google.com
Geologists have long recognized the importance and sought the meaning of curved
orogenic belts. Over the last few decades, several classification schemes have been …

Evidence for surface rupture associated with the Mw 6.3 L'Aquila earthquake sequence of April 2009 (central Italy)

EMERGEO Working Group - Terra Nova, 2010 - Wiley Online Library
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 …

[HTML][HTML] Detrital zircon ages of Oligocene to Miocene sandstone suites of the Southern Apennines foreland basin system, Italy

A Fornelli, F Micheletti, S Gallicchio, F Tursi… - Journal of …, 2022 - Elsevier
U–Pb spot ages on detrital zircons from turbidite quartzarenites, quartz-feldspathic and
volcaniclastic sandstones of the Tufiti di Tusa (TTF), Numidian Flysch (NF), Bifurto (BF) …

Structure of a normal seismogenic fault zone in carbonates: the Vado di Corno Fault, Campo Imperatore, Central Apennines (Italy)

M Demurtas, M Fondriest, F Balsamo… - Journal of Structural …, 2016 - Elsevier
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 …

A review on the driving mechanism of the Tyrrhenian–Apennines system: Implications for the present seismotectonic setting in the Central-Northern Apennines

E Mantovani, D Babbucci, C Tamburelli, M Viti - Tectonophysics, 2009 - Elsevier
The formation of the Tyrrhenian–Apennines system has been characterized by a complex
distribution of major tectonic events, such as opening of basins, migration and distortion of …

Seismic interpretation of the Laga basin; constraints on the structural setting and kinematics of the Central Apennines

S Bigi, P Casero, G Ciotoli - Journal of the Geological Society, 2011 - lyellcollection.org
The Messinian Laga basin is the largest foreland basin within the Central Apennines fold
and thrust belt (Italy). This area, actively investigated in the 1980s and 1990s for …

The Gran Sasso fault system: Paleoseismological constraints on the catastrophic 1349 earthquake in Central Italy

P Galli, A Galderisi, P Messina, E Peronace - Tectonophysics, 2022 - Elsevier
We investigated the late Upper Pleistocene activity of the eight main faults that comprise the
active, dip-slip Gran Sasso fault system (GSFS) in the Gran Sasso d'Italia Massif (central …