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- W2902394556 abstract "espanolEl perfil sismico ESCI-N3.3, que discurre con una direccion normal a las estructuras variscicas, refleja la prolongacion del sector central del NW del Macizo Iberico bajo la plataforma continental. Se describen las principales caracteristicas geologicas del perfil sismico y se proponen interpretaciones tectonicas utilizando informacion geologica asi como datos sismicos de gran angulo registrados en tierra. Los resultados mas significativos incluyen la identificacion de dos cuencas sedimentarias meso-cenozoicas, la aparicion de reflectores inclinados en la corteza media, relacionados con los pliegues y cabalgamientos de la zona Asturoccidental-Leonesa y la posible existencia de un despegue basal de escala cortical para esta zona. La reflectividad es, en general, alta en los niveles corticales inferiores. Por ultimo, algunas reflexiones inclinadas que aparecen en el perfil por debajo de la corteza inferior reflectiva podrian estar relacionados con zonas de subduccion alpinas. EnglishThe seismic profile ESCI-N3.3, sub-perpendicular to the strike of the Variscan structures, has imaged the offshore continuation of the central section of the NW lberian Massif. This study describes its main geological features and propases tectonic interpretations based on geological information and constrained by available refraction/wide-angle reflection data. The main results include the identification of two Mesozoic-Cenozoic sedimentary basins, the occurrence of mid-crustal dipping events related to the fold and thrust tectonics of the Westasturian-Leonese Zone and the possible existence of a crustal-scale basal detachment for this zone. The reflectivity is generally high at lower crustal levels. In addition, dipping events appearing below the reflective lower crust might bear upon Alpine subduction zones." @default.
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- W2902394556 date "1995-01-01" @default.
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- W2902394556 title "Results from the ESCI-N3.3 marine deep seismic profile along the Cantabrian continental margin" @default.
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