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The dismantling of the Apulian carbonate platform during the late Campanian – early Maastrichtian in Albania

dc.rights.licenseopenen_US
dc.contributor.authorLE GOFF, J.
dc.contributor.authorREIJMER, J. J. G.
dc.contributor.authorCEREPI, A.
dc.contributor.authorLOISY, C.
dc.contributor.authorSWENNEN, R.
dc.contributor.authorHEBA, G.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCAVAILHES, Thibault
dc.contributor.authorDE GRAAF, S.
dc.date.accessioned2024-06-06T08:01:41Z
dc.date.available2024-06-06T08:01:41Z
dc.date.issued2019-04-01
dc.identifier.issn0195-6671en_US
dc.identifier.urioai:crossref.org:10.1016/j.cretres.2018.11.013
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/200296
dc.description.abstractEnThe Apulian carbonate margin is widely preserved across the Adriatic domain and has been extensively studied in the south of Italy. In Albania, Oligocene–Pliocene fold-and-thrust tectonics led to widespread exposure of the Apulian Platform and associated Ionian Basin carbonates. However, the portion linking the platform to the basin is missing, preventing a direct reconstruction of the platform margin. Syn-sedimentary folding and faulting are recognized in the uppermost part of both the platform and basinal/slope series. Mass transport deposits (MTDs) occur within the platform succession incorporated into well-bedded intertidal (stromatolites) to shallow-subtidal (rudist packstones) sedimentary sequences. They display significant lateral variability which is accompanied by both rigid and soft deformation structures. Spectacular slumps made up of sediment density flow deposits are recognized in the adjacent Ionian Basin. The lateral extent of basal shear surfaces, syn-sedimentary faults and folds evidenced in the Ionian Basin points toward multiple regional tectonic triggering events affecting the Apulian Platform margin at that time. Bio- and chrono-stratigraphic analyses suggest that the triggers occurred during the late Campanian – early Maastrichtian. Beyond the obvious interest from a stratigraphic point of view, the study of these events recording the dismantling of the Apulian carbonate platform allows for a better understanding of the triggering mechanisms and the sedimentary characteristics of MTDs and slumps at a basinal scale.
dc.language.isoENen_US
dc.sourcecrossref
dc.subject.enCarbonates
dc.subject.enApulia
dc.subject.enMass transport deposits
dc.subject.enUpper Cretaceous
dc.subject.enAlbania
dc.title.enThe dismantling of the Apulian carbonate platform during the late Campanian – early Maastrichtian in Albania
dc.title.alternativeCretac. res.en_US
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.cretres.2018.11.013en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalCretaceous Researchen_US
bordeaux.page83-106en_US
bordeaux.volume96en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamSEDIMen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04603001
hal.version1
hal.date.transferred2024-06-06T08:01:43Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
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