Petrología y geoquímica del plutón aplopegmatítico de Peña Madrid (Sierra de Guadarrama, S.C.E.)

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dc.contributor.authorHuertas, María José
dc.contributor.authorVillaseca, Carlos
dc.date.accessioned2017-07-31T10:47:05Z
dc.date.available2017-07-31T10:47:05Z
dc.date.issued1994
dc.description.abstractThe Peña Madrid aplo-pegmatitic pluton is a very fractionated l-type granite with typically MgO, Ti02, Ba, Sr, Nb and XREE low contents. They intrude as a sheet-like body in the Las Navas del Marqués batholith developing an «in situ» differentiation from the roof margins towards the inner parts. The roof granites show the most primitive magmatic characteristics: the Ti and Mg richest biotites and higher MgO, Ti02, Ba, (Sr, Zr) whole-rock contentses_ES
dc.identifier.urihttp://hdl.handle.net/10272/14006
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.otherPetrographyes_ES
dc.subject.otherGeochemistrees_ES
dc.subject.otherFractionated l-type graniteses_ES
dc.subject.otherIn situ differentiatioes_ES
dc.subject.otherHercynian orogenies_ES
dc.titlePetrología y geoquímica del plutón aplopegmatítico de Peña Madrid (Sierra de Guadarrama, S.C.E.)es_ES
dc.titlePetrology and geochemistry of the Peña Madrid aplopegmatitìc pluton (Sierra de Guadarrama, S.C.Eeng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 15, (1993)