Please use this identifier to cite or link to this item: https://hdl.handle.net/11499/7083
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dc.contributor.authorAlçiçek, Mehmet Cihat-
dc.contributor.authorten Veen, J.H.-
dc.date.accessioned2019-08-16T12:15:21Z
dc.date.available2019-08-16T12:15:21Z
dc.date.issued2008-
dc.identifier.issn0037-0738-
dc.identifier.urihttps://hdl.handle.net/11499/7083-
dc.identifier.urihttps://doi.org/10.1016/j.sedgeo.2008.05.003-
dc.description.abstractAlluvial fan to shallow-marine sedimentation in the Aci{dotless}payam piggy-back basin took place in the hinterland zone of the SE-facing Lycian nappe stack and constrains the age and style of late-stage advance of these nappes. Syn-orogenic sedimentation commenced in Burdigalian time and is marked by coarse-grained alluvial fan deposits that directly overlie Mesozoic ophiolitic rocks. Palaeocurrent data obtained from these coarse-clastic units suggest a south-southeastward drainage. The succession fines upwards and passes into fluvial deposits that become increasingly enriched in carbonate clasts derived from tectonically deeper-seated nappes, suggesting progressive unroofening of the nappe pile. Upwards, the succession is transitional to a Late Burdigalian-Early Langhian marginal marine succession, consisting of off-shore fines with coal seams that overly both the coarse-clastic sediments and basement rocks. Clastic sedimentation ceased at the end of Early Langhian based on reef carbonates that cap the succession. Shallow-marine deposits and overlying reef carbonates confirm a marine transgression that has been reported from elsewhere in the Tauride Belt. Detailed sedimentology of the Aci{dotless}payam basin fill succession, its age and overall tectonic setting imply that during Burdigalian time the succession was deposited in a piggy-back basin, located in the hinterland zone of actively moving thrust sheets. We propose a model in which thick-skinned thrusting invoked inversion of early extensional faults in the autochthon and may explain the generation of large open folds with thick sedimentary sequences in their core. The formation of these large folds may have importantly influenced the frontal accretion such that active shortening moved into the hanging wall resulting in episodic nappe advanced of structurally higher nappes in a mode similar to thin-skin thrusting. The tectonosedimentary evolution of the Aci{dotless}payam piggy-back is strongly dependent on its position relative to the hinge of the large open fold. The absence of any compressional signatures in the basin fill succession indicates that these thrust translations ceased shortly after Aquitanian time. By Serravallian, the succession was interrupted and the region was uplifted to its present elevation, probably by gravitationally isostatic (orogenic) rebound of the nappe stack. After these episodes, tectonic extension predominated and the succession became dissected by nappe-front parallel normal faults that bound the present Çameli Basin. © 2008 Elsevier B.V. All rights reserved.en_US
dc.language.isoenen_US
dc.relation.ispartofSedimentary Geologyen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectNappe emplacementen_US
dc.subjectPiggy-back basinen_US
dc.subjectSyntectonic sedimentationen_US
dc.subjectTauride orogenen_US
dc.subjectalluvial fanen_US
dc.subjectBurdigalianen_US
dc.subjectemplacementen_US
dc.subjectfluvial depositen_US
dc.subjectMesozoicen_US
dc.subjectMioceneen_US
dc.subjectnappeen_US
dc.subjectnormal faulten_US
dc.subjectophioliteen_US
dc.subjectpaleocurrenten_US
dc.subjectpiggyback basinen_US
dc.subjectsedimentation rateen_US
dc.subjectsyntectonic sedimenten_US
dc.subjecttectonic settingen_US
dc.subjectEurasiaen_US
dc.subjectTurkeyen_US
dc.subjectLyciaen_US
dc.titleThe late Early Miocene Aci{dotless}payam piggy-back basin: Refining the last stages of Lycian nappe emplacement in SW Turkeyen_US
dc.typeArticleen_US
dc.identifier.volume208en_US
dc.identifier.issue3-4en_US
dc.identifier.startpage101
dc.identifier.startpage101en_US
dc.identifier.endpage113en_US
dc.authorid0000-0001-7689-7625-
dc.identifier.doi10.1016/j.sedgeo.2008.05.003-
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.identifier.scopus2-s2.0-48349108428en_US
dc.identifier.wosWOS:000259078800004en_US
dc.identifier.scopusqualityQ1-
dc.ownerPamukkale University-
item.languageiso639-1en-
item.openairetypeArticle-
item.grantfulltextnone-
item.cerifentitytypePublications-
item.fulltextNo Fulltext-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
crisitem.author.dept10.08. Geological Engineering-
Appears in Collections:Mühendislik Fakültesi Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collection
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