Search results for "Sediment"

showing 10 items of 1648 documents

Pattern and rate of post-20 ka vertical tectonic motion around the Capo Vaticano Promontory (W Calabria, Italy) based on offshore geomorphological in…

2014

The magnitude and rate of Late Pleistocene-Holocene vertical tectonic movements offshore of the Capo Vaticano Promontory (western Calabria, southern Italy) have been measured on the basis of the present-day depth variations of the edges of submerged depositional terraces (and associated abrasion platforms) that formed below the storm-wave base, during the sea level stillstand of the Last Glacial Maximum (LGM). These depositional features, represented by submerged prograding wedges and an associated terrace-shaped upper boundary, have been identified in high-resolution seismic reflection profiles acquired along the continental shelf and the upper slope of the promontory, and are referred to …

geographyPromontorygeography.geographical_feature_categoryPleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaContinental shelfSettore GEO/03 - Geologia StrutturaleAbrasion platformInfralittoral Prograding Wedge; Abrasion platform; Last Glacial MaximumCalabriaCapo Vaticano Calabria Infralittoral Prograding Wedge; Abrasion platform; Last Glacial Maximum Vertical movementsLast Glacial MaximumCapo Vaticano Calabria Infralittoral Prograding WedgeCapo VaticanoVertical movementsSedimentary depositional environmentTectonicsLast Glacial Maximum Vertical movementsGeomorphologyGeologyHoloceneSea levelEarth-Surface Processes
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Partitioning between “wedge-top” river- and wave-dominated successions: an example from the late Tortonian — early Messinian Terravecchia Formation (…

2011

AbstractDetailed field sedimentological and facies analyses have been performed in the Terravecchia Formation cropping out in NW Sicily, in order to differentiate and describe, for the first time, wave- and river-dominated shallow-marine (deltaic) siliciclastic successions. The latter were deposited filling syntectonic basins, developed between the late Tortonian and early Messinian time, within the wedge-top depozone of the Sicilian Foreland Basin System. It has been observed that river-dominated successions, recording the deposition of small fan-deltas are characterized by fining- to coarsening upward, transgressive-regressive sequences which were mostly deposited filling relatively narro…

geographyQE1-996.5geography.geographical_feature_categoryOutcropterravecchia formationwedge-top depozoneGeologyEnvironmental Science (miscellaneous)Sedimentary basinLate Miocenelate miocenelanguage.human_languageforeland basin systemPaleontologyFacieslanguageGeneral Earth and Planetary SciencessicilySiliciclasticriver-dominated deltasTransgressivewave-dominated deltasSicilianForeland basinGeologyOpen Geosciences
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Mediterranean Tertiary lamproites derived from multiple source components in postcollisional geodynamics

2008

Abstract In the Mediterranean area, lamproitic provinces in Spain, Italy, Serbia and Macedonia have uniform geological, geochemical and petrographic characteristics. Mediterranean lamproites are SiO2-rich lamproites, characterized by relatively low CaO, Al2O3 and Na2O, and high K2O/Al2O3 and Mg-number. They are enriched in LILE relative to HFSE and in Pb, and show depletion in Ti, Nb and Ta. Mediterranean lamproites show huge regional variation of Sr, Nd and 207Pb/204Pb isotopic values, with 87Sr/86Sr range of 0.707–0.722, eNd range from −13 to −3, and 207Pb/204Pb range of 15.62–15.79. Lamproitic rocks are derived from melts with three components involved in their origin, characterized by c…

geographyRadiogenic nuclideOlivinegeography.geographical_feature_categorybiologyTerrigenous sedimentGeochemistry550 - Earth sciencesGeodynamicsengineering.materialbiology.organism_classificationMantle (geology)Volcanic rockGeochemistry and PetrologyLithosphereengineeringGeologyLileGeochimica et Cosmochimica Acta
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Solution and recrystallisation processes and associated landforms in gypsum outcrops of Sicily

2003

Abstract Four small areas of Messinian (Upper Miocene) age gypsum, outcropping in western Sicily, are described. Messinian age evaporites are found in Sicily over a 1000-km 2 area. Here, gypsum outcrops extensively as a consequence of soil erosion induced by human impact. Geomorphological maps show how the rocky surfaces are characterized by a wide range of forms. There are large, medium, small, and microsized forms, which can be identified as belonging to different morphotypes. The morphotypes can be classified into two main categories: those that originated by solution and those that originated through recrystallisation. Four areas, illustrated by geomorphological maps, were specifically …

geographyRecrystallization (geology)geography.geographical_feature_categoryGypsumEvaporiteOutcropGeochemistryMineralogyCrustWeatheringengineering.materialKarstengineeringSedimentary rockGeologyEarth-Surface ProcessesGeomorphology
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Plio-Pleistocene geological evolution of the northern Sicily continental margin (southern Tyrrhenian Sea): new insights from high-resolution, multi-e…

2003

High-resolution seismic profiles were acquired in the north Sicily offshore region with an innovative, multi-tip sparker array which lacks ringing and has a base frequency around 600 Hz. The new data, combined with published data, suggest that intra-slope and extensional basins formed as a consequence of the late Miocene (?)–early Pliocene shortening and thrusting, and the middle (?)–late Pliocene continental rifting affecting the internal side of the Sicilian-Maghrebian chain. Early (?) Pleistocene to Holocene high-amplitude and high-frequency sea-level changes resulted in repeated sub-aerial exposure and flooding of the shelf, and the deposition of cyclically arranged hemipelagic and shel…

geographyRiftgeography.geographical_feature_categoryHigh-resolution seismic profilePleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaContinental shelfNorth Sicily offshoreSequence StratigraphyPlio-PleistoceneEnvironmental Science (miscellaneous)Late MioceneGeotechnical Engineering and Engineering GeologyOceanographyNorth Sicily offshore; High-resolution seismic profiles; Cefalù basin; Sequence StratigraphyPaleontologyContinental marginCefalù basinEarth and Planetary Sciences (miscellaneous)TransgressiveGeologyHolocene
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Integration of HVSR measures and stratigraphic constraints for seismic microzonation studies: the case of Oliveri (ME)

2014

Abstract. Because of its high seismic hazard the urban area of Oliveri has been subject of first level seismic microzonation. The town develops on a large coastal plain made of mixed fluvial/marine sediments, overlapping a complexly deformed substrate. In order to identify points on the area probably suffering relevant site effects and define a preliminary Vs subsurface model for the first level of microzonation, we performed 23 HVSR measurements. A clustering technique of continuous signals has been used to optimize the calculation of the HVSR curves. 42 reliable peaks of the H/V spectra in the frequency range 0.6–10 Hz have been identified. A second clustering technique has been applied t…

geographySeismic microzonationgeography.geographical_feature_categoryHVSRSettore GEO/02 - Geologia Stratigrafica E SedimentologicaBedrockInversion (geology)BoreholemicrotremorMicrozonationAmplitudeSeismic hazardSettore GEO/11 - Geofisica ApplicataRange (statistics)Cluster analysisSeismologyGeology
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Integrating facies and structural analyses with subsidence history in a Jurassic-Cretaceous intraplatform basin: Outcome for paleogeography of the Pa…

2016

Abstract We illustrate the tectono-sedimentary evolution of a Jurassic–Cretaceous intraplatform basin in a fold and thrust belt present setting (Cala Rossa basin). Detailed stratigraphy and facies analysis of Upper Triassic–Eocene successions outcropping in the Palermo Mts (NW Sicily), integrated with structural analysis, restoration and basin analysis, led to recognize and describe into the intraplatform basin the proximal and distal depositional areas respect to the bordered carbonate platform sectors. Carbonate platform was characterized by a rimmed reef growing with progradational trends towards the basin, as suggested by the several reworked shallow-water materials interlayered into th…

geographySouthern Tethyan margingeography.geographical_feature_category010504 meteorology & atmospheric sciencesCarbonate platformStratigraphyGeologyStructural basin010502 geochemistry & geophysics01 natural sciencesCretaceousPaleontologyTectonicsTectonics vs. sedimentationContinental marginFold and thrust beltRestorationFaciesSedimentary basin analysisBasin analysiGeologyIntraplatform basinJurassic-Cretaceous paleogeography0105 earth and related environmental sciences
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Badlands in the Tabernas Basin, Betic Chain

2014

The complex badland landscape at Tabernas results from a combination of relief amplitude generated by tectonic uplift since the Pliocene and reactivated several times during the Pleistocene, the properties of the Tortonian sedimentary rocks and a predominantly arid climate. The landscape is dominated by deep incision of the main river systems, which continues in part of the headwater tributaries, and characterized by contrasting slope morphologies and a variety of microecosystems. The Tabernas badlands exhibit a diversity of landforms resulting from the combination of multi-age soil surface components that allow a variety of processes to operate at different rates. These are dominated by ri…

geographyTectonic upliftgeography.geographical_feature_categoryPleistoceneLandformTributaryErosionSedimentary rockStructural basinSurface runoffGeomorphologyGeology
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Geochemistry of gases and waters discharged by the mud volcanoes at Paternò, Mt. Etna (Italy)

1996

Approximately 20 km south of Mt. Etna craters, at the contact between volcanic and sedimentary formations, three mud volcanoes discharge CO2-rich gases and Na–Cl brines. The compositions of gas and liquid phases indicate that they are fed by a hydrothermal system for which temperatures of 100–150 °C were estimated by means of both gas and solute geothermometry. The hydrothermal system may be associated with CO2-rich groundwaters over a large area extending from the central part of Etna to the mud volcanoes. Numerous data on the He, CH4, CO2 composition of the gases of the three manifestations, sampled over the past 5 years, indicate clearly that variations are due to separation processes of…

geographyVolcanic hazardsgeography.geographical_feature_categoryVolcanoImpact craterGeochemistry and PetrologyGeochemistrySedimentary rockVolcanismSedimentologyGeologyHydrothermal circulationMud volcano
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Deep structural setting of the North American-Caribbean plate boundary in eastern Guatemala

2009

Se presenta un modelo bidimensional de gravedad para determinar la estructura en profundidad del sistema de fallas lateral-izquierda de Motagua-Polochic, que son parte del límite de las placas América del Norte y del Caribe. Estos elementos tectónicos, sismicamente activos, atraviesan oeste-este la región de Guatemala y se sobreponen a una línea de sutura donde afloran cuerpos ophiolíticos. En las principales zonas de desplazamiento de las fallas se han desarrollado cuencas de pull-apart y regiones de restricción (push-up). El análisis estructural de algunas de estas fallas, situadas a lo largo del valle Izabal y del valle Motagua, en combinación con los datos obtenidos del satélite, ha per…

geographyeducation.field_of_studygeography.geographical_feature_categoryLineamentSettore GEO/03 - Geologia StrutturalePopulationMotagua transform systemsEastern Guatemaladeep crustal structurePolochic-Motagua transform systemsStructural basinSedimentary basinTectonicsPlate tectonicsgravity modelingGeneral EnergyGeophysicsPolochicCiencias de la TierraSuture (geology)Eastern Guatemala Polochic-Motagua transform system gravity modelling deep crustal structure.educationGeologySeismologyBouguer anomalyGeofísica Internacional
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