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dc.contributor.authorVegas, Ramón
dc.contributor.authorSuriñach, Emma
dc.date.accessioned2020-07-06T11:09:21Z
dc.date.available2020-07-06T11:09:21Z
dc.date.issued1987
dc.identifier.urihttp://hdl.handle.net/10272/18452
dc.description.abstractA moderate thickening of the crust beneath the Spanish Central System has been determined by means of a wide angle seismic experiment The value of this thickening — 5 km in form of 3 km of the Moho topography, 2 km of surface relief — is coherent with the surface model of intracontinental distributed deformation already described. In addition, the present model is in agreement with the intraplate uplift, the reverse faults that bound the relief and to some extent with the intrap/ate shortening of Iberiaes_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.otherCrustal thickenninges_ES
dc.subject.otherIntraplate upliftes_ES
dc.subject.otherCentral Iberian Peninsulaes_ES
dc.titleEngrosamiento de la corteza y relieve intraplaca en el centro de Iberiaes_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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