Magnetoestratigrafía y origen de la remanencia del Triásico en la Cordillera Ibérica

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dc.contributor.authorRey, Daniel
dc.contributor.authorTurner, P.
dc.contributor.authorRamos, A.
dc.date.accessioned2020-05-19T08:14:41Z
dc.date.available2020-05-19T08:14:41Z
dc.date.issued1991
dc.description.abstractDetailed palaeomagnetic sampling has been made of two units of the Middle Triassic in the western Cordillera Ibérica in Central Spain. Thermal demagnetization reveals the preservation of characteristic Triassic remanence. A recent overprint is also present, but it is almost completely removed after 5000 C. A magnetostratigraphic section was constructed based upon the isolated stab/e components related to the higher unblocking temperaturees_ES
dc.identifier.urihttp://hdl.handle.net/10272/18002
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherMagnetostratigraphyes_ES
dc.subject.otherTriassices_ES
dc.subject.otherCentral Spaines_ES
dc.titleMagnetoestratigrafía y origen de la remanencia del Triásico en la Cordillera Ibéricaes_ES
dc.titleMagnetostratigraphy and origin of remanence of the Triassic in the Cordillera Ibéricaeng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 11, (1991)