Determinación de la deformación finita en la vertiente sur del Pirineo oriental a lo largo de la transversal del rio Ter

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dc.contributor.authorCasas, J. M.
dc.contributor.authorDurney, D.
dc.contributor.authorFerret, J.
dc.contributor.authorMuñoz, J. A.
dc.date.accessioned2016-06-30T11:32:19Z
dc.date.available2016-06-30T11:32:19Z
dc.date.issued1996
dc.description.abstractStrain determinations in the Paleogene rocks of the Ter-Freser section give values 1,1 <Y/Z<1,95 assuming plane strain conditions. Subhorizontal materials of the southern part of the Ebro basin exhibit a remarkable degree of internal deformation, about 35 % shortening. Strain integration all along this section has to be considered in order to obtain a more reliable value of the shortening related to the Alpine deformationen_US
dc.identifier.urihttp://hdl.handle.net/10272/12453
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherStrainen_US
dc.subject.otherPyreneesen_US
dc.subject.otherEbro basinen_US
dc.titleDeterminación de la deformación finita en la vertiente sur del Pirineo oriental a lo largo de la transversal del rio Teren_US
dc.titleFinite strain determination along the Ter section in the southern Pyreneeseng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-4, (1996)