Magmatismo postorogénico y anorogénico en el Sistema Central Español

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dc.contributor.authorVillaseca, Carlos
dc.contributor.authorHuertas, María José
dc.contributor.authorNuez, J. de la
dc.date.accessioned2020-05-19T08:04:11Z
dc.date.available2020-05-19T08:04:11Z
dc.date.issued1991
dc.description.abstractThis work is a summary of the last magmatism in the Spanish Central System, which range in age from Permian to Jurassic times. During Permian the magmas change from peraluminous and calcalkaline to shoshonitic affinities, essentially as small plutons and later dike intrusions. This postorogenic magmatism could be related to latehercynian shear faults. At Iower Mesozoic age there are some dike intrusions ofalka/ine to tholeitic magmas in an anorogenic environnement related to Pangea transform zones of pre-At/antic openinges_ES
dc.identifier.urihttp://hdl.handle.net/10272/18001
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.otherPermian-]urassic periodes_ES
dc.subject.otherPosthercynian to anorogenic transitiones_ES
dc.subject.otherDike-swarmses_ES
dc.subject.otherGeochemistryes_ES
dc.titleMagmatismo postorogénico y anorogénico en el Sistema Central Españoles_ES
dc.titlePostorogenic and anorogenic magmatism in the Spanish Central Systemeng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 11, (1991)