Search results for " wedge-top"

showing 5 items of 5 documents

“Inner” and “outer” wedge-top sequences in the Late Miocene Sicilian Foreland Basin System; inferences from the Upper Tortonian – Lower Messinian Ter…

2010

Late Miocene Sedimentology Terravecchia Formation Wedge-top depozoneSettore GEO/02 - Geologia Stratigrafica E Sedimentologica
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Burial and thermal evolution of the Sicilian fold-and-thrust belt: preliminary results from the Scillato wedge top basin (central-northern Sicily, It…

2016

Wedge top basins are key elements for unravelling the tectonic evolution of fold-and-thrust belts. In detail, their thermal signature and sedimentary fill records modes and time of exhumation of their edges. The Scillato basin is a wedge-top basin located in the central-northern sector of the Sicilian fold-and-thrust belt (western sector of the Madonie Mts). Upper Serravallian-upper Tortonian succession composed by up to 1,200 m thick delta-river to open marine siliciclastic sediments, fills the basin. This succession lies on a deformed substrate made up of thrust sheets composed of Numidian Flysch, Sicilidi and Imerese units stacked with a SW tectonic transport. The basin fill records a po…

Scillato basin thermal history Ro% XRD on clay minerals wedge-topSettore GEO/02 - Geologia Stratigrafica E Sedimentologica
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The Camporeale wedge-top basin (NW Sicily; Italy) in the frame of the Late Miocene Sicilian Foreland Basin System; inferences from the Upper Tortonia…

2010

Terravecchia Formation Late Miocene sedimentology wedge-top basin foreland basin systemSettore GEO/02 - Geologia Stratigrafica E Sedimentologica
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Middle Miocene–Early Pliocene wedge-top basins of NW Sicily (Italy): constraints for the tectonic evolution of a ‘non-conventional’ thrust belt, affe…

2014

The study of geological evolution of a multiphase orogenic belt is complex, expecially when the tectonic events are superimposed in a coaxial fashion. The Sicilian fold-and-thrust belt represents an interest- ing case study, as a non-coaxial superimposition of structures is recognizable, owing to large synkinematic clockwise rotations during each of two subsequent compressional events. These rotations involved also the syntectonic basins that developed in the wedge-top depozone. This study aims to constrain the tectono-depo- sitional evolution of the NW Sicily fold-and-thrust belt and the associated wedge-top depozone between the middle Miocene and the early Pliocene. Integrated analyses of…

business.product_categoryGeological evolutionThrust beltSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia Strutturalefold and thrust beltsWedge top basinGeologyThrustStructural basinWedge (mechanical device)language.human_languageTranspressionPaleontologyTectonicslanguagewedge-top basinsClockwisebusinessfold and thrust belts; wedge-top basins; sicilySicilianSicilySeismologyGeology
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Inner vs. outer wedge-top depozone “sequences” in the Late Miocene (late Tortonian–early Messinian) Sicilian Foreland Basin System; new data from the…

2012

Abstract The wedge-top depozone belongs to the innermost portion of a Foreland Basin System (FBS) ( DeCelles and Giles, 1996 ) and includes all sediments, typically coarse-grained proximal facies, that bury the active frontal part of a fold and thrust belt. The Terravecchia Formation ( Flores, 1959 , Schmidt Di Friedberg, 1962 , Schmidt Di Friedberg, 1964 , Catalano, 1979 ) is a composite lithostratigraphic unit widespread in Sicily (southern Italy) which has been recently considered ( Gugliotta, 2010 ) as a part of the stratigraphic record of the Late Miocene (late Tortonian to early Messinian) Sicilian wedge-top depozone and represent the main object of this paper. Two end-member wedge-to…

geographygeography.geographical_feature_categoryLate MioceneSedimentary basinUnconformitylanguage.human_languageSedimentary depositional environmentPaleontologyForeland Basin System Wedge-top depozone Late Miocene Terravecchia Formation SicilyGeophysicsFold and thrust beltFacieslanguageForeland basinSicilianGeologyEarth-Surface ProcessesJournal of Geodynamics
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