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New structural and seismological evidence and interpretation of a lithospheric-scale shear zone at the southern edge of the Ionian subduction system (central-eastern Sicily, Italy). / Barreca, G.; Scarfì, L.; Cannavò, F. и др.

в: Tectonics, Том 35, № 6, 01.06.2016, стр. 1489-1505.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Barreca, G, Scarfì, L, Cannavò, F, Koulakov, I & Monaco, C 2016, 'New structural and seismological evidence and interpretation of a lithospheric-scale shear zone at the southern edge of the Ionian subduction system (central-eastern Sicily, Italy)', Tectonics, Том. 35, № 6, стр. 1489-1505. https://doi.org/10.1002/2015TC004057

APA

Barreca, G., Scarfì, L., Cannavò, F., Koulakov, I., & Monaco, C. (2016). New structural and seismological evidence and interpretation of a lithospheric-scale shear zone at the southern edge of the Ionian subduction system (central-eastern Sicily, Italy). Tectonics, 35(6), 1489-1505. https://doi.org/10.1002/2015TC004057

Vancouver

Barreca G, Scarfì L, Cannavò F, Koulakov I, Monaco C. New structural and seismological evidence and interpretation of a lithospheric-scale shear zone at the southern edge of the Ionian subduction system (central-eastern Sicily, Italy). Tectonics. 2016 июнь 1;35(6):1489-1505. doi: 10.1002/2015TC004057

Author

Barreca, G. ; Scarfì, L. ; Cannavò, F. и др. / New structural and seismological evidence and interpretation of a lithospheric-scale shear zone at the southern edge of the Ionian subduction system (central-eastern Sicily, Italy). в: Tectonics. 2016 ; Том 35, № 6. стр. 1489-1505.

BibTeX

@article{72b50e28fbe64b7586f7f33ed7f05bc2,
title = "New structural and seismological evidence and interpretation of a lithospheric-scale shear zone at the southern edge of the Ionian subduction system (central-eastern Sicily, Italy)",
abstract = "Geological, gravimetric, and seismological data from the central-eastern Sicily (Italy) provide evidences of a NW-SE oriented shear zone at the southern edge of the Ionian subduction system. This structure consists of a near 100 km long lithospheric-scale structural and seismic boundary. In the near-surface, it shows Plio-Pleistocene vertical-axis structural rotations, kilometer-scale topographic imprint, progressive wrenching, and large down-faulting. All these features, together with its location south-west of the subduction system, allow us to interpret the shear zone as the upper plate expression of an abandoned Subduction Transform Edge Propagator fault, working before slab detachment, currently reactivated by elastic rebound or mantle upwelling mechanism triggered by slab detachment, to form an incipient transform belt separating compartments characterized by different motion in the modern context of Africa-Europe convergence.",
keywords = "abandoned STEP fault, central Mediterranean, elastic rebound, Sicilian/Calabrian subduction system, wrench zone",
author = "G. Barreca and L. Scarf{\`i} and F. Cannav{\`o} and I. Koulakov and C. Monaco",
year = "2016",
month = jun,
day = "1",
doi = "10.1002/2015TC004057",
language = "English",
volume = "35",
pages = "1489--1505",
journal = "Tectonics",
issn = "0278-7407",
publisher = "Wiley-Blackwell",
number = "6",

}

RIS

TY - JOUR

T1 - New structural and seismological evidence and interpretation of a lithospheric-scale shear zone at the southern edge of the Ionian subduction system (central-eastern Sicily, Italy)

AU - Barreca, G.

AU - Scarfì, L.

AU - Cannavò, F.

AU - Koulakov, I.

AU - Monaco, C.

PY - 2016/6/1

Y1 - 2016/6/1

N2 - Geological, gravimetric, and seismological data from the central-eastern Sicily (Italy) provide evidences of a NW-SE oriented shear zone at the southern edge of the Ionian subduction system. This structure consists of a near 100 km long lithospheric-scale structural and seismic boundary. In the near-surface, it shows Plio-Pleistocene vertical-axis structural rotations, kilometer-scale topographic imprint, progressive wrenching, and large down-faulting. All these features, together with its location south-west of the subduction system, allow us to interpret the shear zone as the upper plate expression of an abandoned Subduction Transform Edge Propagator fault, working before slab detachment, currently reactivated by elastic rebound or mantle upwelling mechanism triggered by slab detachment, to form an incipient transform belt separating compartments characterized by different motion in the modern context of Africa-Europe convergence.

AB - Geological, gravimetric, and seismological data from the central-eastern Sicily (Italy) provide evidences of a NW-SE oriented shear zone at the southern edge of the Ionian subduction system. This structure consists of a near 100 km long lithospheric-scale structural and seismic boundary. In the near-surface, it shows Plio-Pleistocene vertical-axis structural rotations, kilometer-scale topographic imprint, progressive wrenching, and large down-faulting. All these features, together with its location south-west of the subduction system, allow us to interpret the shear zone as the upper plate expression of an abandoned Subduction Transform Edge Propagator fault, working before slab detachment, currently reactivated by elastic rebound or mantle upwelling mechanism triggered by slab detachment, to form an incipient transform belt separating compartments characterized by different motion in the modern context of Africa-Europe convergence.

KW - abandoned STEP fault

KW - central Mediterranean

KW - elastic rebound

KW - Sicilian/Calabrian subduction system

KW - wrench zone

UR - http://www.scopus.com/inward/record.url?scp=84977669275&partnerID=8YFLogxK

U2 - 10.1002/2015TC004057

DO - 10.1002/2015TC004057

M3 - Article

AN - SCOPUS:84977669275

VL - 35

SP - 1489

EP - 1505

JO - Tectonics

JF - Tectonics

SN - 0278-7407

IS - 6

ER -

ID: 25707441