Search results for "Sediment"

showing 10 items of 1648 documents

The Camporeale wedge-top basin (NW Sicily; Italy) in the frame of the Late Miocene Sicilian Foreland Basin System; inferences from the Upper Tortonia…

2010

Terravecchia Formation Late Miocene sedimentology wedge-top basin foreland basin systemSettore GEO/02 - Geologia Stratigrafica E Sedimentologica
researchProduct

Cyanophyte calcification morphotypes and depositional environments (Alenquer oncolite, upper Kimmeridgian?, Portugal)

1985

Terrigenous red siliciclastics of Upper Kimmeridgian(?) to Portlandian age around Alenguer, Portugal, comprise a narrow level of oncoid-bearing limestones. Oncoid cortices are composed of cyanophytes which appear in different calcification morphotypes according to changing physico-chemical parameters. Recent examples reveal that in most cases each calcification morphotype is related to one single species or one defined association. Hence, the characteristic calcification patterns are mostly biologically rather than abiogenetically controlled. Oncoid shapes, sizes and arrangement, on the other hand, are mainly determined by the hydraulic parameter within the depositional environment.

Terrigenous sedimentStratigraphyPaleontologyGeologymedicine.diseaseSedimentary depositional environmentPaleontologySingle speciesPaleobotanymedicineSedimentologyBiogeosciencesGeologyCalcificationOncoliteFacies
researchProduct

Review of “Marine Hard Substrates: Colonization and Evolution,” a Thematic Session at the Geological Society of America Annual Meeting, Denver, USA, …

2005

A theme session, jointly sponsored by the Paleontological Society and the Geological Society of America Sedimentary Geology division, and entitled “Marine Hard Substrates: Colonization and Evolutio...

Thematic mapHistorySedimentary GeologyPaleontologyLibrary scienceColonizationEnvironmental ethicsSession (computer science)Theme (narrative)Ichnos
researchProduct

Luminescence Dating of Fluvial Deposits in the Rock Shelter of Cueva Antón, Spain

2015

Abstract The fluvial sediments at Cueva Antón, a Middle Palaeolithic rock shelter located in the valley of the River Mula (Southeast Spain), produced abundant lithic assemblages of Mousterian affinities. Radiocarbon dates are available for the upper part of the archaeological succession, while for the middle to lower parts chronometric data have been missing. Here we present luminescence dating results for these parts of the succession. Quartz OSL on small aliquots and single grain measurements yield ages ranging from 69 ± 7 ka to 82 ± 8 ka with a weighted mean of 72 ± 4 ka for sub-complexes AS2 to AS5. Equivalent dose estimates from large aliquots were highest and inconsistent with those f…

Thermoluminescence datingLuminescence datingFluvial sedimentGeochemistryFluvialMousterianEcological successionArqueologiaFeldsparlaw.inventionlawvisual_artEarth and Planetary Sciences (miscellaneous)visual_art.visual_art_mediumMiddle PalaeolithicRadiocarbon datingSingle grain datingPost-IR IRSLCueva AntónQuartzGeomorphologyRock shelterGeologyGeochronometria
researchProduct

Middle to Upper Pleistocene morphostructural evolution of the NW-coast of Sicily: thermoluminescence dating and palaeontological-stratigraphical eval…

1997

Abstract Infralittoral and terrigenous Middle to Upper Pleistocene deposits outcropping at the NW-coast of Sicily (Gulf of Castellammare and peninsula of Capo San Vito) were investigated in order to recognise glacio-eustatically caused sea level highstands and the interference between tectonics, eustasy and local conditions of the coast. The results, originating from a stratigraphically important area, were obtained by palaeontological-stratigraphical analyses, physical age determination with the thermoluminescence method and by detailed morphostructural studies. The marine deposits, situated at 3–40 m a.s.l., mainly provide an oligotypic molluscan fauna referable to modern SGCF-, SFHN- and…

Thermoluminescence datingPleistoceneOutcropTerrigenous sedimentPaleontologyOceanographyDeep seaPaleontologyStage (stratigraphy)Glacial periodEcology Evolution Behavior and SystematicsGeologySea levelEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
researchProduct

Beaches in Valencian Coast

2018

The main factors that determined the Valencian beaches characteristics are the configuration of relief structures; fluvial sediment supply; low tidal range; the predominance of low energy waves; scarcity of big storms; longshore littoral drift; and human action. There is a significant prevalence of sandy beaches. Nevertheless, both at the northern part of the Gulf of Valencia and in the structural segment, between the Cape Sant Antoni and Alicante city, pebble and gravel beaches are predominant. Most of the Valencian beaches have experienced significant morphological changes during the last decades due to the human interventions -voluntary or involuntary- in the coastal system. The implemen…

Tidal range010504 meteorology & atmospheric sciencesStorm010502 geochemistry & geophysics01 natural sciencesValencianlanguage.human_languageCoastal erosionLongshore driftOceanographyGeographylanguageSedimentary rockPebbleFluvial sediment0105 earth and related environmental sciences
researchProduct

Impact of sedimentology and diagenesis on the petrophysical properties of a tight oolitic carbonate reservoir. The case of the Oolithe Blanche Format…

2013

18 pages; International audience; The Oolithe Blanche Formation was studied in three quarries, located at the south-eastern edge of the Paris Basin (France). Heterogeneities in reservoir properties were assessed through a sedimentological, diagenetic and petrophysical study. The relationships between depositional settings, diagenesis and petrophysical properties were analysed using detailed petrographic studies, image analysis, Nano CTscans and petrophysical measurements. The carbonate reservoir pore network is mainly controlled by intraparticle microporosity which ensures the connectivity with interparticle meso- and macroporosity. Early cementation vs. early compaction processes (mainly g…

Tight carbonate reservoir010504 meteorology & atmospheric sciencesStratigraphyGeochemistry010502 geochemistry & geophysicsOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPermeabilityDiagenesisSedimentary depositional environmentPetrographyPetrophysicschemistry.chemical_compoundParis BasinSedimentologyGeomorphology[SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesPetrophysicsGeologyCementation (geology)Fluid-flow propertiesDiagenesisPermeability (earth sciences)GeophysicschemistryOoids[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateEconomic GeologyPorosityGeology
researchProduct

Human settlement dynamics and alluvial dynamics of the Rhine River during the Holocene: Geoarchaeology of the site of Oedenburg (Haut-Rhin, France).

2007

The relationship between alluvial dynamics and control parameters such as climate are well known and understood at plurimillennial and pluriannual time-scales. But it is not really the case at multicentennial and multidecennal time-scales compatible with human society settlement time-scales. In a present and near future context, when human settlement may be affected by strong climatic variation, alluvial dynamics understanding is however a major centre of attention to the development of efficient models. To approach this scale-related question, a segment of the Upper Rhine River presenting both anastomosed and braided was investigated. This area also gives us the opportunity to study settle…

Tomographie électrique[SDU.STU.GM] Sciences of the Universe [physics]/Earth Sciences/Geomorphology[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryStratigraphy[SDE.MCG]Environmental Sciences/Global ChangesCartes anciennesMonnaies romainesInondationsMagnetic prospectingStratigraphieGéoradarProspections géomagnétiquesGround Penetrating RadarRhin supérieurArchéologieSystème d'information géographique[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentAlluvial forestsForêts alluviales[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentPedestrian prospecting[ SDU.STU.GM ] Sciences of the Universe [physics]/Earth Sciences/Geomorphology[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and PrehistoryGeographic Information SystemSédimentologieUpper RhineGeomorphologySedimentology[SDE.ES]Environmental Sciences/Environmental and Society[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentFloodsElectrical Tomography[ SDE.MCG ] Environmental Sciences/Global Changes[SDE.MCG] Environmental Sciences/Global ChangesArchaeology[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and PrehistoryProspections pédestres[SDE.ES] Environmental Sciences/Environmental and SocietyGéomorphologie[ SDE.ES ] Environmental Sciences/Environmental and SocietyAncient maps
researchProduct

Soil and organic carbon redistribution in a recently burned Mediterranean hillslope affected by water erosion processes

2022

Forest fires cause many changes in the physical, chemical and biological soil properties such as aggregation and soil organic carbon contents (SOC) as well as on soil hydrology and erosion processes. Most studies on post-fire soil erosion in Mediterranean environments have been plot-based and research at hillslope or broader scale is scarce. Understanding SOC nature, distribution and modifications, as produced by forest fires and erosion, has become crucial to model and define the role of soil erosion as source or sink of C, and to sustainably manage ecosystem services related to the soil resource. This research provides data about the loss and redistribution of soil and SOC in a Mediterran…

Total organic carbonCanopyMediterranean climateConnectivitySòls ErosióForest firesSoil ScienceSedimentSoil scienceSoil carbonCoupled hillslopesSedimentary depositional environmentSòls DegradacióSoil organic carbon sinkSoil waterIncendisDensity fractionationErosionEnvironmental science
researchProduct

Geochemical implications for changing dust supply by the Indian Monsoon system to the Arabian Sea during the last glacial cycle

2004

Element concentrations of 43 elements as well as inorganic and organic carbon content of sediment core 70KL from the western Arabian Sea were measured with high (1 cm) sample resolution. Principal components of the sediment’s chemical composition were determined with the help of statistical principle component analysis. These components are representing the major environmental factors at the site. The most important processes controlling the observed variations are the changing lithogenic influx derived from the major wind systems of the region (i.e., the Arabian northwesterly winds, the northeast winter monsoon and the southwest summer monsoon), summer monsoon associated upwelling and biog…

Total organic carbonMonsoon of South AsiaOceanographyProductivity (ecology)UpwellingSediment550 - Earth sciencesGlacial periodMonsoonChemical compositionGeology
researchProduct