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Neogene and Quaternary rollback evolution of the Tyrrhenian Sea, the Apennines, and the Sicilian Maghrebides

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dc.contributor.authorRosenbaum, Gideon
dc.contributor.authorLister, Gordon
dc.date.accessioned2015-12-08T22:43:14Z
dc.date.issued2004
dc.date.updated2023-07-02T08:16:22Z
dc.description.abstractReconstruction of the evolution of the Tyrrhenian Sea shows that the major stage of rifting associated with the opening of this basin began at ∼ 10 Ma. It involved two episodes of back arc extension, which were induced by the rollback of a west dipping
dc.identifier.issn0278-7407
dc.identifier.urihttp://hdl.handle.net/1885/37185
dc.publisherAmerican Geophysical Union
dc.sourceTectonics
dc.subjectKeywords: backarc basin; basin evolution; Cenozoic; slab; subduction; tectonic evolution; tectonics; Mediterranean Sea; Tyrrhenian Sea Apennines; Reconstruction; Sicilian Maghrebides; Subduction rollback; Tyrrhenian Sea
dc.titleNeogene and Quaternary rollback evolution of the Tyrrhenian Sea, the Apennines, and the Sicilian Maghrebides
dc.typeJournal article
local.bibliographicCitation.startpageTC1013
local.contributor.affiliationRosenbaum, Gideon, Monash University
local.contributor.affiliationLister, Gordon, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidLister, Gordon, u4065900
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040313 - Tectonics
local.identifier.absfor040312 - Structural Geology
local.identifier.ariespublicationu9503261xPUB145
local.identifier.citationvolume23
local.identifier.doi10.1029/2003TC001518
local.identifier.scopusID2-s2.0-4344675967
local.identifier.thomsonID000189048500002
local.type.statusPublished Version

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