Publication:
Mecanismos de evolución magmática en los diques microdioríticos de la sierra de Guadarrama

dc.contributor.authorHuertas Coronel, María José
dc.contributor.authorAncochea Soto, Eumenio
dc.date.accessioned2023-06-20T17:28:03Z
dc.date.available2023-06-20T17:28:03Z
dc.date.issued1991-11
dc.description.abstractIn the Central System of Spain outcrop se vera I dyke swarms of late-hercynian age. They are mainly composed by granitic porphyry and microdioritic dykes. The last one, when globaly considered, show scattering in the contents of most of the major and trace elements. When we study the individual microdioritic swarms, it can be observed that they exhibit more defined compositional and evolutionary trends. These trends are different from one microdioritic swarm to another. The variations can be justified by different crystal fractionation models and reflect heterogeneities in the source or differences on the melting process.
dc.description.departmentDepto. de Mineralogía y Petrología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/9904
dc.identifier.issn0213-683X
dc.identifier.officialurlhttp://www.sociedadgeologica.es/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/58274
dc.issue.number10
dc.journal.titleGeogaceta
dc.language.isospa
dc.page.final97
dc.page.initial93
dc.publisherSociedad Geológica de España
dc.rights.accessRightsopen access
dc.subject.cdu552.3(234.1)
dc.subject.keywordCentral System of Spain
dc.subject.keywordMicrodioritic dykes
dc.subject.keywordFractionation crystal
dc.subject.ucmPetrología
dc.titleMecanismos de evolución magmática en los diques microdioríticos de la sierra de Guadarrama
dc.typejournal article
dspace.entity.typePublication
relation.isAuthorOfPublicationc39a1f37-2172-44cf-81b2-a56171ec7b5f
relation.isAuthorOfPublication5a353ace-8a94-4f6e-8a98-20878931274b
relation.isAuthorOfPublication.latestForDiscoveryc39a1f37-2172-44cf-81b2-a56171ec7b5f
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