Search results for "Sedimentary dynamics"

showing 4 items of 4 documents

Sedimentary dynamics and extensional structuring related to early Cretaceous rifting of Neocomian and Barremian deposits of the interior basin of Gab…

2008

18 pages; International audience; Recent field and subsurface data about the early Neocomian N'dombo series and the Neocomian to mid-Barremian Schistes series of the interior basin of Gabon further our understanding of the initial stages of early Cretaceous N40–60E extensional rifting. The syn-rift series comprise fluvial–lacustrine claystones–sandstones, rare conglomerates, and carbonates. The syn-rift fill begins with braided-stream feldspathic sandstones. These are overlain first by fluvial–lacustrine deposits and then by predominantly lacustrine–palustrine claystones, which are potential petroleum source rocks. The claystones are eroded in part and are capped by the pre-Aptian angular u…

Tectono-sedimentary010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesPalaeoenvironment010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesUnconformitySedimentary depositional environmentPaleontologySedimentary dynamicsLower CretaceousGabon0105 earth and related environmental sciencesEarth-Surface Processes[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsRiftGeologySubsidence[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/TectonicsCretaceous[ SDE.MCG ] Environmental Sciences/Global ChangesSource rock[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesSedimentary rockSyn-riftGeology
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Efectos de una crecida en un cauce antropizado. La riada del Palancia de octubre de 2000

2011

[EN] In October of 2000, the Palància River underwent a major flood, which substantially modified the morphology of the river channel. These changes took place on a river bed previously modified by public works aimed at cleaning and simplifying the river section. The flood partially restored the braided morphology, reconstructing bars and channels. Moreover, river incision processes increased, particularly downstream the Palància bridges. This process reveals a sedimentary deficit caused by reservoirs; land use changes and gravel mining. The aim of this work is to describe these processes of change and to analyze the morphosedimentary consequences, through the interpretation of aerial photo…

UNESCO::HISTORIAGeografíaDinámica sedimentariaGeociencias. Medio ambienteFluvial morphologyGISSIGEphemeral riversBraided riversRíos braidedSedimentary dynamicsMorfología fluvialGrupo B:HISTORIA [UNESCO]Cauces efímeros
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SEDIMENTARY DYNAMICS OF THE MARETTIMO CONTINENTAL SHELF AND MARETTIMO CHANNEL (EGADI ISLANDS – WESTERN MEDITERRANEAN): ANALYSIS OF DEPOSITIONAL AND E…

2011

Sedimentary dynamics of the Marettimo continental shelf and Marettimo Channel (Egadi Island – Western Mediterranean), have been unveiled based on the erosive and depositional features observed at the seafloor. Different morphologic features were recognized through side scan sonar, multibeam and high-resolution seismics, acquired in the framework of national Research Projects (CARG, GebecSud, MaGIC) carried out by the Department of Earth and Marine Science (former Department of Geology and Geodesy) of the University of Palermo. Sediment samples have been also collected and analyzed. The Egadi Islands are part of the NW Sicilian offshore, and belong to the mountain chain that connects the Sic…

Sedimentary dynamics Marine geomorphology Marine bedforms Egadi Islands
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Approche d'un territoire de montagne : occupations humaines et contexte pédo-sédimentaire des versants du col du Petit-Saint-Bernard, de la Préhistoi…

2014

As part of a multi-year programme, survey campaigns have been carried out on both slopes of the Petit-Saint-Bernard pass (2188 m, western Alps), at an altitude of between 750 and 3000 m. The method employed abandons ground-based surveying in favour of multiple manual surveys carried out on selected topographic contexts down to the base of the Holocene fill. The results obtained document the longterm development of the pedo-sedimentary dynamic and the occupation of the different altitude stages. The significance of the archaeological data collected is discussed in relation to the state of knowledge in a comparison area including the neighbouring valleys of the western Alps, to existing settl…

funerary practicesBronze Agepédogenèsepratiques funérairesIron Age[SDE.MCG]Environmental Sciences/Global Changesdynamique du peuplement alpin[SHS.GEO] Humanities and Social Sciences/GeographyNéolithiquesédentarisationâge du FerAlpine settlement dynamicssites perchéshabitatspedo-sedimentary dynamicsNeolithicalpagesdynamique pédo-sédimentaireAlpes occidentales[SDE.IE]Environmental Sciences/Environmental Engineering[SHS.GEO]Humanities and Social Sciences/Geographyhabitationpedogenesis[SDE.ES]Environmental Sciences/Environmental and Societyalpine pasturespastoralismewestern Alpscirculations transalpines[SDE.BE] Environmental Sciences/Biodiversity and Ecologytrans-Alpine circulation[SDE.MCG] Environmental Sciences/Global Changesâge du Bronzesedentism[SDE.ES] Environmental Sciences/Environmental and Society[SDE.IE] Environmental Sciences/Environmental Engineering[SDE.BE]Environmental Sciences/Biodiversity and Ecologypastoralism
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