Hinterland-Verging Thrusting in the Northern Sicily Continental Margin: Evidences for a Late Collisional Stage of the Sicilian Fold and Thrust Belt?

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Abstract

The Sicilian Fold and Thrust Belt developed during Neogene-Quaternary times characterized by main African-wards tectonic transport direction. Recent investigations highlighted extensive hinterland-verging tectonic structures active during late Pliocene-Pleistocene time suggesting a late collisional stage of the Sicilian Fold and Thrust Belt that could be a precursor of a change in the subduction polarity in the central belt of Mediterranean.
Lingua originaleEnglish
Pagine251-253
Numero di pagine3
Stato di pubblicazionePublished - 2018

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fold and thrust belt
continental margin
tectonic structure
Neogene
Pliocene
subduction
Pleistocene
tectonics

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title = "Hinterland-Verging Thrusting in the Northern Sicily Continental Margin: Evidences for a Late Collisional Stage of the Sicilian Fold and Thrust Belt?",
abstract = "The Sicilian Fold and Thrust Belt developed during Neogene-Quaternary times characterized by main African-wards tectonic transport direction. Recent investigations highlighted extensive hinterland-verging tectonic structures active during late Pliocene-Pleistocene time suggesting a late collisional stage of the Sicilian Fold and Thrust Belt that could be a precursor of a change in the subduction polarity in the central belt of Mediterranean.",
author = "{Gasparo Morticelli}, Maurizio and Mauro Agate and Attilio Sulli and Elisabetta Zizzo",
year = "2018",
language = "English",
pages = "251--253",

}

TY - CONF

T1 - Hinterland-Verging Thrusting in the Northern Sicily Continental Margin: Evidences for a Late Collisional Stage of the Sicilian Fold and Thrust Belt?

AU - Gasparo Morticelli, Maurizio

AU - Agate, Mauro

AU - Sulli, Attilio

AU - Zizzo, Elisabetta

PY - 2018

Y1 - 2018

N2 - The Sicilian Fold and Thrust Belt developed during Neogene-Quaternary times characterized by main African-wards tectonic transport direction. Recent investigations highlighted extensive hinterland-verging tectonic structures active during late Pliocene-Pleistocene time suggesting a late collisional stage of the Sicilian Fold and Thrust Belt that could be a precursor of a change in the subduction polarity in the central belt of Mediterranean.

AB - The Sicilian Fold and Thrust Belt developed during Neogene-Quaternary times characterized by main African-wards tectonic transport direction. Recent investigations highlighted extensive hinterland-verging tectonic structures active during late Pliocene-Pleistocene time suggesting a late collisional stage of the Sicilian Fold and Thrust Belt that could be a precursor of a change in the subduction polarity in the central belt of Mediterranean.

UR - http://hdl.handle.net/10447/359228

UR - https://doi.org/10.1007/978-3-030-01455-1

M3 - Other

SP - 251

EP - 253

ER -