Publikationsdatum:
2021-05-12
Beschreibung:
The 2016–2017 Amatrice-Norcia seismic sequence was triggered by the reactivation of a complex NNW-SSE
trending, WSW-dipping normal fault system cross-cutting the Umbria-Marche fold and thrust belt near M. Vettore.
This fault system produced clear and impressive co-seismic ruptures on normal faults in the hangingwall of
the M. Sibillini thrust, whereas ruptures in the footwall were observed, but less clear. As a result, a strong
controversy exists in the literature about the geometry of the seismogenic faults, their relationships with preexisting
thrusts, and the location of normal-faulting rupture tips. In this work, we present a 3D geological
model of the M. Vettore area located between the Castelluccio basin and the outcrop of the M. Sibillini thrust,
where the most evident co-seismic ruptures have been observed. The model shows the relationship between the
ruptured normal faults and the M. Sibillini thrust, and was constructed using a grid of 14 geological crosssections
parallel and orthogonal to the main structural elements (i.e. normal faults and thrusts) down to a
depth of 3 km. The model was built using reference structural surfaces, such as the top of the Early Cretaceous
Maiolica Fm., the M. Sibillini thrust and the main seismogenic normal faults belonging to the M. Vettore fault
system. The 3D model has allowed us to calculate the vertical cumulative throw distribution for the M. Vettore
normal faults. The cumulative geological throw of ca. 1300 m across the normal faults in the proximity of the M.
Sibillini thrust indicates that the seismogenic fault system continues into the footwall of the thrust, displacing it
in the sub-surface. The results of this study provide important constraints on the cross-cutting relationships
between active normal and pre-existing compressional structures in seismically active areas, contributing to a
better definition of the faults segmentation, and the related seismic hazard.
Beschreibung:
Published
Beschreibung:
103938
Beschreibung:
2T. Deformazione crostale attiva
Beschreibung:
JCR Journal
Schlagwort(e):
2016-2017 Central Italy earthquake
;
Apennines
;
Cross-cutting relationships
;
Inherited structures
;
3D structural model
Repository-Name:
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
Materialart:
article
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