Search results for "Sediment"

showing 10 items of 1648 documents

Seismically-induced soft-sediment deformation structures in Upper Triassic deepwater carbonates (Central Sicily)

2016

We describe soft-sediment deformation structures into the Upper Triassic cherty limestone outcropping in the Pizzo Lupo section (Central Sicily, Italy), pertaining to the deep-water palaeodomain of the Southern Tethyan margin. In the study section, mainly consisting of thin-bedded mudstone/marl alternations with bedded chert intercalations, some lithofacies have been separated on the basis of the abundance of the calcium carbonate/clay content and the overall textural features. The deformational structures, displaying different deformational styles as folded and faulted beds, disturbed layers, clastic dikes, and slumps occur mainly in the deformed horizons that involve marl-dominated lithof…

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicasoft-sediment deformation structures synsedimentary tectonics Upper Triassic deep-water carbonates
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Stratigraphy in the study area

2011

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicastratigraphy central Sicilywell log stratigraphy
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STOP 2-Mesozoic and Cenozoic carbonates of the Imerese basin along the Rocca di Sclafani Bagni outcrop

2011

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicastratigraphy deep water succession petrography
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Subduction-related structures and geodinamic evolution of SE Sicily-Calabria offshore

2008

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicasubduction zones oceanic structures
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Development, human impact and habitat distribution in submarine canyons of the Central and Western Mediterranean

2015

We present in this paper different studies on canyon systems, adopting distinct approaches, temporal and spatial scales. Most of our study areas coincide with the NW Sicilian canyons, which present striking differences in their morphologies in response to the Plio-Quaternary tectonic evolution of the northern Sicilian margin. In the present-day, active sedimentary processes inferred from bedform analyses along some of the studied canyons could drive to enhanced biological activities along them. This is also confirmed by an on-going study of the impact of trawling fishery on the morphology and sedimentary environments of the Sicilian margin, where intense deep-sea bottom trawling activities …

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicasubmarine canyon human impact habitat distribution Mediterranean Sea
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The tectono-sedimentary evolution of the syntectonic basins growing on the Sicilian fold and thrust belt

2013

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicasyntectonic basin tectono-sedimentary evolution Sicilian fold and thrust belt
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Computation of run-up heights for landslide-generated tsunami. An attempt of hazard assessment in the North Sicily continental margin

2014

The North Sicily continental margin is a very active region located in a transitional area between the Sicilian- Maghrebian Chain to the south and the southern Tyrrhenian Sea to the north. Strong seismicity, active tectonics and volcanism, fluid escape, high sediment supply and widespread mass movements exposed this region to marine geohazards, with a potential for tsunami generation (e.g. Messina 1908, Stromboli 2004 events). In recent years, high resolution swath mapping and high resolution to high penetration seismic reflection profiles have been collected during several oceanographic cruises, in the frame of the MaGIC and CARG projects. Morphobatymetric and geoseismic analysis evidenced…

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicatsunami run-up submarine landslideSettore GEO/03 - Geologia Strutturale
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A scenario-based assessment of the tsunami hazard in palermo, northern sicily, and the southern tyrrhenian sea

2020

Palermo is a populous city situated on the northern coast of Sicily, bordered by the Tyrrhenian Sea. This central part of the Mediterranean Sea features dramatic bathymetry, numerous subaqueous landslides and is also the epicentre to many subaqueous earthquakes. As such, the region is an area prone to tsunamis. This investigation uses the Cornell Multi-Grid Coupled Tsunami (COMCOT) tsunami modelling package to simulate five near-field landslides, and five near-field earthquakes regarded as worst-case credible scenarios for Palermo. The seismic simulations produced waves on a very small scale, the largest being c. 5 cm at its maximum height, and none of the earthquake-generated tsunami waves…

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicatsunami submarine landslideearthquakeSettore GEO/03 - Geologia StrutturaleSettore GEO/04 - Geografia Fisica E Geomorfologiamultibeamtsunami; Sicily; multibeamtsunamiSicilygeo-hazard
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Sequence stratigraphy of a mesozoic carbonate platform-to-basin system in Western sicily

2009

Abstract Sequence stratigraphic studies of the Triassic through Paleogene carbonate successions of platform, slope and basin in western Sicily (Palermo and Termini Imerese Mountains) have identified a sedimentary cyclicity mostly caused by relative oscillations of sea level. The stratigraphic successions of the Imerese and Panormide palaeogeographic domains of the southern Tethyan continental margin were studied with physical-stratigraphy and facies analysis to reconstruct the sedimentary evolution of this platform-to-basin system. The Imerese Basin is characterized by a carbonate and siliceous-calcareous succession, 1200–1400m thick, Late Triassic to Eocene in age. The strata display a typ…

Shelf-to-basin system sedimentologyQE1-996.5tectono-eustatic cyclesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformTransgressive/regressive cyclesGeologyEnvironmental Science (miscellaneous)Paleontologychemistry.chemical_compoundchemistryContinental marginFaciesTectono-eustatic cycleGeneral Earth and Planetary SciencesCarbonateSedimentary rockSequence stratigraphyProgradationMesozoic western SicilyPaleogeneGeology
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An exceptional rocky shore preserved during Oligocene (Late Rupelian) transgression in the Upper Rhine Graben (Mainz Basin, Germany)

2012

The Early Oligocene (Late Rupelian) Alzey Formation (Mainz Basin, Upper Rhine Graben, Germany) records the development of a rocky coast depositional system during transgression. The formation unconformably overlies Permian bedrock across a composite transgressive ravinement surface. Exposure of the surface shows a succession of subplanar bedrock terraces, separated by near-vertical risers. Terraces show a broad staircase geometry and display wave-erosional features (notches, sea stacks, furrows). Detailed sedimentological and palaeoecological investigations reveal prograding beachface and shoreface depositional units that overlie terraces and are adjacent to risers. Terraces are interpreted…

Shore010506 paleontologygeographyTectonic subsidencegeography.geographical_feature_categoryBedrockGeology010502 geochemistry & geophysics01 natural sciencesWave-cut platformSedimentary depositional environmentGrabenPaleontologyTerrace (geology)14. Life underwaterGeology0105 earth and related environmental sciencesMarine transgressionGeological Journal
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