Engrosamiento de la corteza y relieve intraplaca en el centro de Iberia

dc.contributor.authorVegas Martínez, Ramón
dc.contributor.authorSuriñach Cornet, Emma
dc.date.accessioned2023-06-21T02:17:44Z
dc.date.available2023-06-21T02:17:44Z
dc.date.issued1987
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 thickeníng - 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 deformatíon already descríbed. In addition, the present model is in agreement with the intraplate uplíft, the reverse faults that bound the relief and to sorne extent with the intraplate shortening of Iberia.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/70198
dc.identifier.issn0213-683X
dc.identifier.officialurlhttps://sociedadgeologica.org/publicaciones/geogaceta/geogaceta-2-1987/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/65262
dc.journal.titleGeogaceta
dc.language.isospa
dc.page.final42
dc.page.initial40
dc.publisherSociedad Geológica de España
dc.rights.accessRightsopen access
dc.subject.cdu551.24(234.1)
dc.subject.keywordCrustal thickenníng
dc.subject.keywordIntraplate uplift
dc.subject.keywordCentral Iberian Península
dc.subject.ucmGeodinámica
dc.subject.unesco2507 Geofísica
dc.titleEngrosamiento de la corteza y relieve intraplaca en el centro de Iberia
dc.typejournal article
dc.volume.number2
dspace.entity.typePublication
relation.isAuthorOfPublicationc552d3fa-f581-450e-aa53-d1382e0cd6ba
relation.isAuthorOfPublication90ba3196-1671-4c5e-9ee9-045c8ddacf1b
relation.isAuthorOfPublication.latestForDiscovery90ba3196-1671-4c5e-9ee9-045c8ddacf1b
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