Magnetobiochronology of lower Pliocene marine sediments from the lower Guadalquivir Basin; insights into the tectonic evolution of the Strait of Gibraltar area

The Gibraltar Arc is a complex tectonic region, and several competing models have been proposed to explain its evolution. We studied the sedimentary fill of the Guadalquivir Basin to identify tectonic processes that were occurring when the reopening of the Strait of Gibraltar led to the reestablishm...

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Veröffentlicht in:	Geological Society of America bulletin 2018-11, Vol.130 (11-12), p.1791-1808
Hauptverfasser:	Pérez-Asensio, José N, Larrasoaña, Juan C, Samankassou, Elias, Sierro, Francisco J, Garcia-Castellanos, Daniel, Jiménez-Moreno, Gonzalo, Salazar, Ángel, Salvany, Josep Maria, Ledesma, Santiago, Mata, M. Pilar, Civis, Jorge, Mediavilla, Carlos
Format:	Artikel
Sprache:	eng
Schlagworte:	Basins biostratigraphy Boreholes Cenozoic Chronology cores depositional environment Enginyeria civil Europe Evolution Foraminifera Frameworks Geologia Geology Gibraltar, Estret de Gibraltar, Strait of Guadalquivir Basin Iberian Peninsula lithostratigraphy lower Pliocene magnetostratigraphy marine environment Marine sediments Messinian microfossils Neogene Outflow Passive margins Plate tectonics Pliocene Progradation Sea level Sediment Sedimentary facies Sedimentary geology sedimentary rocks Sedimentation Sedimentation rates Sediments Southern Europe southwestern Spain Spain Strait of Gibraltar Straits Stratigraphy Structural geology Subsidence tectonics terrestrial environment Tertiary Uplift Àrees temàtiques de la UPC
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