Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/10479| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | Barreca, G.; Università di Catania | en |
| dc.contributor.authorall | Scarfì, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
| dc.contributor.authorall | Cannavò, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
| dc.contributor.authorall | Koulakov, I.; Institute of Petroleum Geology and Geophysics, Novosibirsk, Russia | en |
| dc.contributor.authorall | Monaco, C.; Università di Catania | en |
| dc.date.accessioned | 2017-03-22T08:10:22Z | en |
| dc.date.available | 2017-03-22T08:10:22Z | en |
| dc.date.issued | 2016 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/10479 | en |
| dc.description | - We performed an integrative analysis of geological gravimetric and seismological data - Analyzed data depicted a not well-known wrench zone in the central-eastern Sicily - Our findings enabled us to interpret this shear zone as a Plio-Pleistocene STEP fault | en |
| dc.description.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 | en |
| dc.language.iso | English | en |
| dc.publisher.name | American Geophysical Union | en |
| dc.relation.ispartof | Tectonics | en |
| dc.relation.ispartofseries | /35 (2016) | en |
| dc.subject | abandoned STEP fault | en |
| dc.subject | Sicilian/Calabrian subduction system | en |
| dc.subject | central Mediterranean | en |
| dc.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) | en |
| dc.type | article | en |
| dc.description.status | Published | en |
| dc.type.QualityControl | Peer-reviewed | en |
| dc.description.pagenumber | 1489–1505 | en |
| dc.identifier.URL | http://onlinelibrary.wiley.com/doi/10.1002/2015TC004057/abstract | en |
| dc.subject.INGV | 04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics | en |
| dc.identifier.doi | 10.1002/2015TC004057 | en |
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(1992), First- and second-order patterns of stress in the lithosphere: The World Stress Map Project, J. Geophys. Res., 97(B8), 11,703–11,728, doi:10.1029/92JB00132. | en |
| dc.description.obiettivoSpecifico | 1T. Geodinamica e interno della Terra | en |
| dc.description.journalType | JCR Journal | en |
| dc.description.fulltext | restricted | en |
| dc.relation.issn | 0278-7407 | en |
| dc.relation.eissn | 1944-9194 | en |
| dc.contributor.author | Barreca, G. | en |
| dc.contributor.author | Scarfì, L. | en |
| dc.contributor.author | Cannavò, F. | en |
| dc.contributor.author | Koulakov, I. | en |
| dc.contributor.author | Monaco, C. | en |
| dc.contributor.department | Università di Catania | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
| dc.contributor.department | Institute of Petroleum Geology and Geophysics, Novosibirsk, Russia | en |
| dc.contributor.department | Università di Catania | en |
| item.openairetype | article | - |
| item.cerifentitytype | Publications | - |
| item.languageiso639-1 | en | - |
| item.grantfulltext | restricted | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| crisitem.author.dept | Dipartimento di Scienze Biologiche, Geologiche e Ambientali - Sezione di Scienze della Terra, Università di Catania | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
| crisitem.author.dept | IPGG SB RAS, Novosibirsk, Russia | - |
| crisitem.author.dept | Dipartimento di Scienze Biologiche, Geologiche e Ambientali, Sezione di Scienze della Terra, Università di Catania | - |
| crisitem.author.orcid | 0000-0002-5995-3880 | - |
| crisitem.author.orcid | 0000-0001-7550-8579 | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| Appears in Collections: | Article published / in press | |
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