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dc.contributor.authorAlvaro López, M.
dc.date.accessioned2020-07-03T16:00:22Z
dc.date.available2020-07-03T16:00:22Z
dc.date.issued1987
dc.identifier.urihttp://hdl.handle.net/10272/18426
dc.description.abstractThe subsidence trajectories are built with two localities data from the Iberian Chain. Both curves show two rifting-tectonic subsidence cycles. The first one (Triassic-Jurassic) belongs to the development of the Celtiberian Aulacogen, in relationship with the BeticBalearic passive margin (Western Tethys). The second cycle occurred in Cretaceous times, and it was conditioned by the Iberian Plate anti-clockwise drifting and Bay of Biscay openning. The stretching rates were Iow to moderate: 1.12 and 7.26.es_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherTectonic subsidencees_ES
dc.subject.otherExtensional tectonicses_ES
dc.subject.otherIntraplate basines_ES
dc.subject.otherIberian chaines_ES
dc.titleLa subsidencia tectónica en la Cordillera Ibérica durante el Mesozoicoes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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Atribución-NoComercial-SinDerivadas 3.0 España
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