Search results for " contourites"

showing 2 items of 2 documents

Seismic stratigraphy of upper Quaternary shallow-water contourite drifts in the Gulf of Taranto (Ionian Sea, southern Italy)

2018

Abstract The occurrence of articulated seafloor morphology over continental shelf-upper slope environments, may result in a significant change in the patterns and intensity of basin-scale thermohaline circulation during eustatic sea-level fluctuations. These changes may cause, in turn, erosion, deposition and/or transport of sediments at the seafloor, to form shallow-water contourite drifts. Here we investigate this process in the NW sector of the Gulf of Taranto (Ionian Sea) during and following the Last Glacial Maximum (LGM), by integrating multibeam bathymetric data, ultra-high resolution seismic-reflection data and gravity core data. Sea level fall caused subaerial exposure of the summi…

Axial and lateral channel-patch drifts; Channel-related drifts; Gulf of Taranto; Ionian Sea; Last Glacial Maximum; Shallow-water contourites; Younger DryasYounger Dryas010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleGulf of TarantoAxial and lateral channel-patch driftsYounger Drya010502 geochemistry & geophysicsOceanography01 natural sciencesChannel-related driftsPaleontologyGeochemistry and PetrologyShallow-water contouriteShallow-water contouritesYounger DryasSea level0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryLast Glacial MaximumContinental shelfAxial and lateral channel-patch driftGeologyContouriteLast Glacial MaximumIonian SeaSeafloor spreadingThermohaline circulationChannel-related driftQuaternaryGeology
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Eustatic and oceanographic control on sedimentary evolution of middle-late Quaternary shelf margin-to-upper slope deposits on the Egadi Islands offsh…

2016

During the past decades a number of sequence stratigraphy studies illustrated how, during Quaternary, interaction between sea level changes and sediment supply controlled the depositional evolution along continental margins, giving a cyclic signature to the sedimentary infilling. However, as both deposition and erosion are processes ultimately controlled by balance between environmental energy and sedimentary influx, also the oceanographic regime takes part in controlling the sedimentary growth along the continental margin. This is exactly what occurs on physiographic settings as islands offshore areas, where bottom currents can be very energetic. In the western Sicily offshore, southwards …

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicasea level change contourites submarine valley Egadi islands Quaternary
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