Estimación de las condiciones del metamorfismo hercínico de alta presión de la Sierra de Guadarrama

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dc.contributor.authorVillaseca, Carlos
dc.contributor.authorBarbero, Luis
dc.date.accessioned2017-07-19T09:40:00Z
dc.date.available2017-07-19T09:40:00Z
dc.date.issued1994
dc.description.abstractA revision of the P-T conditions of the first metamorphic episode, based on new data on the mineral chemistry of the residual high pressure paragenesis of the metabasic and metapelitic rocks from the Sierra de Guadarrama, has been made. The results show that this conditions were previously clearly underestimated, and that the minimun pressure achieved is around 9 kb, probably reaching up to 12-15 kb, for temperatures in the range 650-750°Ces_ES
dc.identifier.urihttp://hdl.handle.net/10272/13939
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.otherMineral chemistryes_ES
dc.subject.otherP-T conditionses_ES
dc.subject.otherHigh-P metamorphismes_ES
dc.subject.otherHercynian Iberian Beltes_ES
dc.titleEstimación de las condiciones del metamorfismo hercínico de alta presión de la Sierra de Guadarramaes_ES
dc.titleEstimation of the hercynian high-pressure metamorphic conditions in the Sierra de Guadarrama (Spain)eng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 16, (1994)