Partición de la deformación cenozoica intraplaca en el Sistema Central

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dc.contributor.authorVicente, Gerardo de
dc.date.accessioned2014-05-13T09:38:47Z
dc.date.available2014-05-13T09:38:47Z
dc.date.issued2009
dc.description.abstractA new model for Cenozoic strain partitioning is proposed here for the Central System at the Messejana (Plasencia) fault zone. It explains the simultaneous movement of parallel NE-SW trending thrust and strikeslip faults within a global N-S compression. This process could account for local bends in the shmax trajectories, from NW-SE trending close to the Ponsul-Gata and Gredos thrusts to NE-SW trending along the Messejana left-lateral strike-slip fault. This structural pattern may change current thinking with regard to the paleostress evolution of the Iberia foreland during the Cenozoicen_US
dc.identifier.urihttp://hdl.handle.net/10272/8108
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherStrain partitioningen_US
dc.subject.otherPaleostressen_US
dc.subject.otherIberia forelanden_US
dc.titlePartición de la deformación cenozoica intraplaca en el Sistema Centralen_US
dc.titleCenozoic intraplate strain partitioning in the Central Systemeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 46, (2009)