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Alpine exhumation of the Pedriza - La cabrera morphotectonic block (Sierra del Guadarrama, Spanish Central System): potentiality of fission - track thermochronology in apatite

dc.contributor.authorSell, I.
dc.contributor.authorPoupeau, G.
dc.contributor.authorCasquet Martín, César
dc.contributor.authorGalindo, Carmen
dc.contributor.authorGonzález Casado, J. M.
dc.date.accessioned2017-03-23T11:39:47Z
dc.date.available2017-03-23T11:39:47Z
dc.date.issued1995
dc.identifier.urihttp://hdl.handle.net/10272/13518
dc.description.abstractThe principles of Apatite Fission Track Analysis (AFTA), which allows to decipher the time-temperature paths of apatites since their last cooling below about 110°C are given and one example, from a Pedriza - La Cabrera block, is discussed. It is suggested from AFTA that the cooling history of this sample followed three steps: from 45 Ma to 35 Ma, slow cooling at a rate of 2,5 - 5° C/Ma between 110° C and 60° C, followed by a quasi-plateau at 70-80°C up to about 70 Ma ago, where a new cooling episode started, with a mean 6 -7 ° C/Ma cooling rate up to the present timeen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherFission Tracken_US
dc.subject.otherTermocronologiaen_US
dc.subject.otherEvolución tectonotermaen_US
dc.subject.otherSierra del Guadarramaen_US
dc.subject.otherSistema Central Españolen_US
dc.titleExhumación alpina del bloque morfotectónico Pedriza - La Cabrera (Sierra del Guadarrama, Sistema Central Español): potencialidad de la termocronometría por trazas de fisión en apatitosen_US
dc.titleAlpine exhumation of the Pedriza - La cabrera morphotectonic block (Sierra del Guadarrama, Spanish Central System): potentiality of fission - track thermochronology in apatiteeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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