2020
DOI: 10.1016/j.earscirev.2020.103257
|View full text |Cite
|
Sign up to set email alerts
|

Structural and tectono-stratigraphic review of the Sicilian orogen and new insights from analogue modeling

Abstract: The Apennines-Sicilian-Maghrebian fold-and-thrust belt originated from the subduction of the Alpine Tethys and the later collision of drifted continental blocks against the African and Apulian paleomargins. From North to South, the Sicilian Fold-and-Thrust Belt (SFTB) is divided in four main tectono-stratigraphic domains: (1) the Calabro-Peloritani terrane, drifted from the European margin, (2) the remnants of the Alpine Tethys accretionary Wedge (ATW) related to the subduction of the Tethys, (3) the folded an… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
18
0

Year Published

2020
2020
2024
2024

Publication Types

Select...
8

Relationship

1
7

Authors

Journals

citations
Cited by 29 publications
(18 citation statements)
references
References 209 publications
(387 reference statements)
0
18
0
Order By: Relevance
“…From a geological point of view, this territory is mainly made up of sedimentary successions belonging to different periods. The dominance of Flysch is mostly noted, the oldest sediments belonging to the Alpine Tethys Units [40], they are Cretaceous in age and are represented by deep-water flyschs and scaly clays. Most of the outcropping rocks are part of the so-called Flysch of Monte Soro (upper Tithonian, lower Cretaceous) and Numidian (lower Oligocene Miocene) [41].…”
Section: Study Areamentioning
confidence: 99%
“…From a geological point of view, this territory is mainly made up of sedimentary successions belonging to different periods. The dominance of Flysch is mostly noted, the oldest sediments belonging to the Alpine Tethys Units [40], they are Cretaceous in age and are represented by deep-water flyschs and scaly clays. Most of the outcropping rocks are part of the so-called Flysch of Monte Soro (upper Tithonian, lower Cretaceous) and Numidian (lower Oligocene Miocene) [41].…”
Section: Study Areamentioning
confidence: 99%
“…9.7.1; https://www.seequent.com/products-solutions/geosoft-oasis-montaj/ ). a foreland area cropping out in the Hyblean Plateau and representing the onshore portion of the relative undeformed North Africa-Pelagian basement bounded to the east by the Ionian plate; a tight Pliocene–Pleistocene NW-dipping foredeep, prolonging from SE to the Gela Basin; the orogenic wedge made up of an E-SE trending fold and thrust complex 6 , 10 , 20 – 22 made up of a European portion (Peloritani Units), a Tethyan element (Sicilide Units) and an African component (Maghrebian Sicilian Units) 2 , 3 , 9 , 20 , 23 . …”
Section: Geological Settingmentioning
confidence: 99%
“…the orogenic wedge made up of an E-SE trending fold and thrust complex 6 , 10 , 20 – 22 made up of a European portion (Peloritani Units), a Tethyan element (Sicilide Units) and an African component (Maghrebian Sicilian Units) 2 , 3 , 9 , 20 , 23 .…”
Section: Geological Settingmentioning
confidence: 99%
See 1 more Smart Citation
“…Four main tectono‐stratigraphic domains are attributed to the Sicilian orogen (Figure 1, e.g., Henriquet et al., 2020): (a) To the northeast (Peloritan and Calabrian mountain ranges), the Calabro‐Peloritani block corresponds to upper‐plate continental remnants derived from the European margin. (b) In Central and Northern Sicily, the Alpine Tethys accretionary wedge relics come from the offscraping of the neo‐Tethyan sedimentary cover during the Oligocene‐Early Miocene subduction phase.…”
Section: Introductionmentioning
confidence: 99%