Morfología y Zonación de los Granates en el plutón granítico de Ponferrada (España)

dc.contributor.authorSanto, G del
dc.contributor.authorCorretgé Castañón, Luis Guillermo
dc.contributor.authorSuárez Hernando, Oier
dc.date.accessioned2019-06-05T12:32:00Z
dc.date.available2019-06-05T12:32:00Z
dc.date.issued1992
dc.description.abstractCarnet occurs as an accesory phase mainly in the aplitlc facies of the Ponferrada Pluton (BoatLos Ancares Belt) (LeDuc, 1970; Su&rez, 1970). Three different types of garnet have been recognized on the basis of their morphology and textural relationships. Electron micropobe analyses reveal several zonation patterns mainly defined by the variation of Mn and Fe contents. The study of chemical zonation in garnet also proved to be useful in timing the growth of garnet with respect to quartzes_ES
dc.identifier.urihttp://hdl.handle.net/10272/16354
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.otherGarnetes_ES
dc.subject.otherAplitices_ES
dc.subject.otherPlutones_ES
dc.subject.otherMorphologyes_ES
dc.subject.otherChemical zonationes_ES
dc.subject.otherGrowthes_ES
dc.subject.otherPonferradaes_ES
dc.subject.otherQuartzes_ES
dc.titleMorfología y Zonación de los Granates en el plutón granítico de Ponferrada (España)es_ES
dc.titleGarnet Morphology and Chemical Zonation in the Ponferrada pluton (Spain)eng
dc.typejournal articlees_ES
dspace.entity.typePublication

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