Architecture and seismotectonics of a regional low‐angle normal fault zone in central Italy
Information from surface geology, subsurface geology (boreholes, seismic reflection, and
refraction profiles), and seismicity are used to depict the geometry and the possible …
refraction profiles), and seismicity are used to depict the geometry and the possible …
Tectonic evolution of a low‐angle extensional fault system from restored cross‐sections in the Northern Apennines (Italy)
F Mirabella, F Brozzetti, A Lupattelli, MR Barchi - Tectonics, 2011 - Wiley Online Library
Broad geological and geophysical documentation is available on regional extensional
systems driven by low‐angle normal faults. However, little information exists about the three …
systems driven by low‐angle normal faults. However, little information exists about the three …
Anatomy of late orogenic extension: the Northern Apennines case
JVA Keller, G Minelli, G Pialli - Tectonophysics, 1994 - Elsevier
Late orogenic extensional structures overprint the compressional structures of the Northern
Apennines fold and thrust belt. The Tyrrhenian Sea is the result of major continental …
Apennines fold and thrust belt. The Tyrrhenian Sea is the result of major continental …
Site amplifications observed in the Gubbio Basin, Central Italy: hints for lateral propagation effects
In this study we investigate the site amplification effects observed in the Gubbio plain, central
Italy. The recordings of 140 local earthquakes (1.2≤ Ml≤ 4.7) observed by two linear arrays …
Italy. The recordings of 140 local earthquakes (1.2≤ Ml≤ 4.7) observed by two linear arrays …
The Gubbio normal fault (Central Italy): geometry, displacement distribution and tectonic evolution
Normal faults within orogenic belts can be pre-, syn-or post-orogenic features. We studied
the Gubbio normal fault (central Italy), which is an example of a pre-orogenic fault …
the Gubbio normal fault (central Italy), which is an example of a pre-orogenic fault …
Sentinel-1 interferometry and UAV aerial survey for map** coseismic ruptures: Mts. sibillini vs. Mt. etna volcano
The survey and structural analysis of surface coseismic ruptures are essential tools for
characterizing seismogenic structures. In this work, a procedure to survey coseismic …
characterizing seismogenic structures. In this work, a procedure to survey coseismic …
Normal faulting vs regional subsidence and sedimentation rate
C Doglioni, N Dagostino, G Mariotti - Marine and Petroleum Geology, 1998 - Elsevier
Normal faults occur in a variety of geodynamic environments, both in areas of subsidence
and uplift. Normal faults may have slip rates faster or slower than regional subsidence or …
and uplift. Normal faults may have slip rates faster or slower than regional subsidence or …
Interseismic creep of carbonate-hosted seismogenic normal faults: Insights from central Italy
Understanding fault behavior in carbonates is critical because they represent loci of
earthquake nucleation. Models of fault-slip mode generally assume:(1) seismic sliding and …
earthquake nucleation. Models of fault-slip mode generally assume:(1) seismic sliding and …
The Gubbio fault: can different methods give pictures of the same object?
Different investigation techniques (field geology and structural analysis, geomorphology,
seismic reflection profiles and seismological data) have been used to develop images of the …
seismic reflection profiles and seismological data) have been used to develop images of the …
Controls of radiogenic heat and moho geometry on the thermal setting of the marche region (Central Italy): an analytical 3D geothermal model
Using published cross-sections and a series of geological constraints, a 3D geological
model of an important area of the Adriatic sector of peninsular Italy—ie, the Marche region …
model of an important area of the Adriatic sector of peninsular Italy—ie, the Marche region …