Search results for "Flysch"

showing 3 items of 13 documents

Geological Map of the Rocca Busambra-Corleone region (western Sicily, Italy): explanatory notes

2011

The geology of the Rocca Busambra-Corleone region, in centralwestern Sicily, is relevant to the understanding of the central sector of the Maghrebian-Sicilian fold-and-thrust belt. In the investigated area Mesozoic shallow- and deep-water carbo - nate deposits pertaining respectively to the Trapanese and the Sica - nian successions, and a thick Oligo-Miocene numidian flysch body, crop out. Minor outcrops of Cretaceous-Palaeogene Sicilide complex and syn-orogenic deposits of the Late Serravallian-Early Messinian Castellana Sicula and Terravecchia formations are also present. A structural analysis reveals complex tectonic relationships between the Trapanese carbonate platform tectonic unit (t…

geographygeography.geographical_feature_categoryFlyschSettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformOutcropAnticlineGeologyFault (geology)chemistry.chemical_compoundPaleontologyTectonicschemistryWestern Sicily geological survey and mapping Mesozoic shallow- and deep-water carbonate successionstectono-stratigraphic setting Meso-Cenozoic deformational history.General Earth and Planetary SciencesCarbonateMesozoicGeologyItalian Journal of Geosciences
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Deep controls on foreland basin system evolution along the Sicilian fold and thrust belt

2015

Abstract Neogene-Quaternary wedge-top-basins arose during the Sicilian fold and thrust belt (FTB) build-up. The infilling sedimentary successions are: i) middle-upper Miocene silicoclastics succession, accommodated on top of the accreted Sicilide and Numidian flysch nappes; ii) upper Miocene-lower Pliocene deepening-upwards sediments unconformably overlying the inner Meso-Cenozoic deep-water, Imerese and Sicanian thrust units; iii) Upper Pliocene-Quaternary coastal-open shelf deposits unconformably covering (in the outer sector of the FTB) a tectonic stack (Gela thrust system). These successions are characterized by a basal unconformity on the deformed substrate believed to be the depositio…

geographygeography.geographical_feature_categoryFlyschSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleGeologyUnconformityThrust tectonicsNappePaleontologyTectonicsRestorationWedge-top basinFold and thrust beltSedimentary rockSyn-sedimentary tectonicSicilyForeland basinGeologyBulletin de la Société Géologique de France
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Effects of the 6th September 2002 earthquake: damage amplification in the south-eastern sector of Palermo explained by GIS technology

2009

During the 6th September 2002 earthquake the highest damage level in Palermo was observed in the SE sector.
 This is a recent urbanization area where reinforced concrete structures predominate. A detailed analysis of soil
 properties in Palermo was carried out by City-GIS to investigate a possible role of nearsurface geology on earthquake
 effects. City-GIS is a tool dedicated to natural hazard evaluation in urban areas. The availability of high
 density of well log data (stratigraphic and geotechnical) allowed a realistic modeling of surface geology and
 physical-mechanical properties that control the seismic response. In wide zones of the above mentioned sector
 of…

geographyseismic responseFlyschgeography.geographical_feature_categoryOutcropBedrocklcsh:QC801-809Terrainlcsh:QC851-999GISPalermoCalcarenitelcsh:Geophysics. Cosmic physicsGeophysicsNatural hazardCohesion (geology)site effectslcsh:Meteorology. ClimatologyAlluviumGeomorphologySeismologyGeologyAnnals of Geophysics
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