Search results for "Balearic promontory"

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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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Role of extension and compression in the evolution of the eastem margin of Iberia: the ESCI- València Trough seismic profile

1994

Carlos.Santisteban@uv.es The ESCI-València Trough deep seismic reflection profile crosses the eastern margin of Iberia and can be divided into three regions according to crustal structure. From NW to SE they are: a) the Ebro Basin, whit a 33 km thick continental crust wich remained almost undeformed during the Cenozoic and is very reflective in its lower part; b) the Continental Margin, made up of the Catalan-Valencian Domain and the Balearic Promontory with a thin (12 to 30 km thick) continental crust wich was deformed during the Cenozoic, extensional structures predominating the first domain and contractional structures in the second; and c) the Algerian Basin, with a 9 km thick oceanic c…

Sísmica de reflexión profunda; Estructura cortical; Surco de Valencia; Promontorio BalearSísmica de reflexión profundaDeep seismic relfection; Crustal structure; Valencia Tough; Balearic PromontoryValencia ToughBalearic PromontoryCrustal structureEstructura corticalSurco de ValenciaUNESCO::CIENCIAS DE LA TIERRA Y DEL ESPACIO::Geología:CIENCIAS DE LA TIERRA Y DEL ESPACIO::Geología [UNESCO]Promontorio BalearDeep seismic relfection
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