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Mineralogical and geochemical differences of the initial volcanism of Fuerteventura

dc.contributor.authorMuñoz, Mercedes
dc.contributor.authorSagredo, J.
dc.contributor.authorIgnacio, Cristina de
dc.date.accessioned2014-06-04T08:20:24Z
dc.date.available2014-06-04T08:20:24Z
dc.date.issued2008
dc.identifier.urihttp://hdl.handle.net/10272/8249
dc.description.abstractThe initial growth stage of the Fuerteventura Island is represented by submarine, transitional and subaerial volcanics. Among the submarine types, two can be distinguished: a basaltic (s.l.) one, and a basanitic one. The latter is characterized by the presence of hydrous ferromagnesian minerals (kaersutite, phlogopite) and a more alkaline character, whereas the former shows a less alkaline character that brings it closer to the subaerial group. All these groups would be generated from different partial melt degrees of a garnetbearing mantle source. However, for the basanitic group, also a shallower (oceanic lithosphere) melting and an amphibole-bearing source have to be invokeden_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherSubmarine-subaerialen_US
dc.subject.otherBasaltic-basanitic volcanismen_US
dc.subject.otherMineralogyen_US
dc.subject.otherGeochemistryen_US
dc.subject.otherFuerteventuraen_US
dc.titleDiferencias mineralógicas y geoquímicas del vulcanismo inicial de Fuerteventuraen_US
dc.titleMineralogical and geochemical differences of the initial volcanism of Fuerteventuraeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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