Search results for " Sedimentolog"

showing 10 items of 358 documents

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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SEA-LEVEL AND CLIMATIC CHANGES DURING THELAST 41,000 YEARS IN THE OUTER SHELF OF THE SOUTHERN TYRRHENIAN SEA: EVIDENCE FROM FORAMINIFERA AND SEISMOST…

2012

Sea Level Changes QuaternarySettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/01 - Paleontologia E PaleoecologiaVariazioni del livello marino QuaternarioSettore GEO/08 - Geochimica E Vulcanologia
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Reply to comment by C. Morhange, C. Flaux, P.A. Pirazzoli, M.B. Carre on “Holocene Sea level Change in Malta”

2013

The pits of Birzebbugia are located near the present-day mean sea level, and some are partially submerged. They were dated using pottery discovered in an archaeological site close to the coast, dated to the Bronze Age (Zammit, 1928; Abela, 1999). As they have been interpreted as sites for the retting of flax, during their utilization they should have remained dry and the sea could not submerge them. This is the reason why these structures are not directly related to the sea level, as suggested by Biolchi et al. (2011), so they represent an upper limit.

Sea level changeClimatic changes -- MaltaSea level -- MaltaSettore GEO/02 - Geologia Stratigrafica E SedimentologicaMaltaSettore GEO/04 - Geografia Fisica E Geomorfologiasea level change; Malta;upliftPaleoecology -- MaltaGeographyOceanographyPalynology -- Maltaupliftsea level changeHoloceneEarth-Surface Processes
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Core description collected during Oceanographic Survey NextData2013 (12 – 19 September 2013)

2013

Sediment Core Micropaleontology Sedimentology Paleoclimatology Tephra
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Mineralogical and chemical variability of fluvial sediments: 1. Bedload sand (Ganga–Brahmaputra, Bangladesh)

2010

This study investigates the natural processes that control concentration of detrital minerals and consequently chemical elements in river sand. The novelty of our approach consists in the systematic integration of detailed textural, petrographical, mineralogical and chemical data, and in the quantitative description and modeling of relationships among mineralogical and chemical variables for each sample and each grain-size class in each sample. Bed sediment in transit in the largest sedimentary system on Earth chiefly consists of fine-grained lithofeldspatho quartzose sand including rich amphibole–epidote–garnet suites, mixed with minor very-fine grained-sand to silt subpopulations containi…

Sedimentary petrologyProvenanceHimalayaGeochemistrysedimentary geochemistry sedimentary petrology settling equivalence selective entrainment placer sands opaque minerals REE-bearing minerals Eu anomaly HimalayaSedimentFluvialEu anomalyWeatheringSiltSedimentary geochemistryGeophysicsPlacer sandSettling equivalenceSpace and Planetary ScienceGeochemistry and PetrologyOpaque mineralEarth and Planetary Sciences (miscellaneous)Sedimentary rockGEO/02 - GEOLOGIA STRATIGRAFICA E SEDIMENTOLOGICAREE-bearing mineralSelective entrainmentChemical compositionGeologyBed load
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The integration of surface and subsurface stratigraphic data with HVSR measures for studies of seismic microzonation: the case of Oliveri (ME)

2013

Because of its high seismic hazard the urban area of Oliveri has been subject of a study on seismic microzonation at first level (OPCM 3907/2010). The urban area develops on a large coastal plain made of Late Pleistocene and Holocene mixed fluvial/marine sediments, that mainly consist of silty sands and gravels. The eastern part of this plain is dominated by the alluvial deposits of the Elicona torrent. The coastal and alluvial sediments overlap a complexly deformed substrate made of Hercynian metamorphites (Aspromonte unit), the Capo d’Orlando Flysch, the Antisicilide Argille Scagliose and Pleistocene clays and calcarenites. This area is affected by high uplift rates as recently estimated …

Seismic microzonation HVSR coastal plain sediments paleo-valleySettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/11 - Geofisica Applicata
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Hatching Success of Caretta caretta on a Mediterranean Volcanic Beach: Impacts from Environmental Parameters and Substrate Composition

2022

New data on the potential impact of environmental parameters and the mineralogical nature of the substrate on the hatching success of the loggerhead sea turtle Caretta caretta on a volcanic beach on Linosa Island in the central Mediterranean Sea are reported. During 2 years of investigation (2018-19), five nests were observed. The temperature and moisture of the nests were determined along with the grain size and mineralogical nature of the substrate. The temperature values of the nests recorded at depths of 5 and 35 cm showed an average temperature incubation of 32.2°C ± 1.4°C and 32.8°C ± 1.6°C, respectively, with peaks close to 37°C. The sedimentological analysis carried out on two cores…

Settore BIO/07 - EcologiaSettore GEO/02 - Geologia Stratigrafica E SedimentologicaEcologyLoggerhead sea turtle volcanic island Mediterranean Sea sedimentological features moisture temperature biometric parameters malformations.Settore BIO/05 - ZoologiaSettore GEO/07 - Petrologia E PetrografiaEarth-Surface ProcessesWater Science and TechnologyJournal of Coastal Research
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ASPRACOAST: A model of integrated coastal zone management of the eastern part of the Gulf of Palermo (Sicily, Italy)

2009

Settore BIO/07 - EcologiaSettore M-GGR/02 - Geografia Economico-PoliticaSettore GEO/02 - Geologia Stratigrafica E SedimentologicaGulf of PalermoSettore GEO/01 - Paleontologia E PaleoecologiaSettore GEO/12 - Oceanografia E Fisica Dell'Atmosferacoastal zone managementSettore ING-IND/35 - Ingegneria Economico-GestionaleSicily
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ASPRACOAST: Modello di gestione ambientale della fascia costiera del comune di Bagheria

2008

Settore BIO/07 - EcologiaSettore M-GGR/02 - Geografia Economico-PoliticaSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSicilia Gestione fascia costiera BagheriaSettore GEO/01 - Paleontologia E PaleoecologiaSettore GEO/12 - Oceanografia E Fisica Dell'AtmosferaSettore ING-IND/35 - Ingegneria Economico-Gestionale
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The Messinian Salinity Crisis deposits in the Balearic Promontory: An undeformed analog of the MSC Sicilian basins??

2021

International audience; The Messinian Salinity Crisis (MSC) is a controversial geological event that influenced the Mediterranean Basin in the late Miocene leaving behind a widespread Salt Giant. Today, more than 90% of the Messinian evaporitic deposits are located offshore, buried below the Plio-Quaternary sediments and have thus been studied mainly by marine seismic reflection imaging. Onshore-offshore records’ comparisons and correlations should be considered a key approach to progress in our understanding of the MSC.This approach has however not been widely explored so far. Indeed, because of the erosion on the Messinian continental shelves and slopes during the MSC, only few places in …

Settore GEO/02 - Geologia Stratigrafica E Sedimentologica010504 meteorology & atmospheric sciencesOutcropStratigraphy[SDU.STU]Sciences of the Universe [physics]/Earth SciencesLate MioceneStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesSedimentary depositional environmentPaleontologyBalearic promontory Caltanissetta basin Central Mallorca depression Messinian salinity crisis Outcrops14. Life underwater0105 earth and related environmental sciencesgeographyPromontorygeography.geographical_feature_categoryContinental shelfGeologySettore GEO/01 - Paleontologia E Paleoecologialanguage.human_languageTectonicsGeophysics13. Climate actionlanguageEconomic GeologySicilianGeologyMarine and Petroleum Geology
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