Descenso eustático messiniense en una cuenca atlántica. El cañón submarino del Río Guadalquivir. (SO de España)

Martínez del Olmo, W.Riaza Molina, C.Torrescusa Villaverde, S.2020-05-282020-05-281996http://hdl.handle.net/10272/18111Numerous seismic lines allow {he identification of a deep and long erosive canyon incised during the Messinian on shelfal and basinal deposits of Upper Tortonian and Messinian s.s. age. Reconstructions of the pre-erosional sedimentary architecture and other regional data support the interpretation of the erosion being of submarine origin and probably related with a Guadalquivir paleo-riverspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Messinian unconformityEustatic changesSystem TractsIncised valley fillDescenso eustático messiniense en una cuenca atlántica. El cañón submarino del Río Guadalquivir. (SO de España)The messinian submarine canyon of the Guadalquivir river (Atlantic coast southwestern Spain)journal articleopen access