Show simple item record structures of the Catalan Prelitoral range: evolution and relation with the marginal deposits of the Ebro basin

dc.contributor.authorLópez Blanco, M.
dc.description.abstractDuring paleogene times the deformation area associated to the Vallés fault system developed a series of compressive structures. In itially there was theem placement of a succession of thrusts and folds affecting mainly the mesozoic cover, whose erosion led to the deposition of mesozoic cover derived monogenic breccias and conglomerates. Subsequently the emergence of an out of sequence thrust, involving mainly paleozoic basement rocks was recorded in the basin by a paleozoic derived monogenic breccia level. Later on, basement and cover derived poligenic conglomerates and breccias were deposited as a response to the erosion of a more heterogeneous source area. The movement of a second thrust plate involving basement and cover rocks folded and thrusted the mesozoic cover and the tertiary deposits of the Ebro basin margines_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherAlpine thrustinges_ES
dc.subject.otherAlluvial fanes_ES
dc.subject.otherSource areaes_ES
dc.titleEstructuras contractivas de la Cordillera Prelitoral Catalana entre la sierra de Les Pedritxes y el río Ripofll: evolución y relación con los depósitos del márgen de la cuenca del Ebroes_ES structures of the Catalan Prelitoral range: evolution and relation with the marginal deposits of the Ebro basineng

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Atribución-NoComercial-SinDerivadas 3.0 España
Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

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