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dc.contributor.authorNotario del Pino, J. S.
dc.contributor.authorRodríguez Losada, J. A.
dc.contributor.authorQueralt Mitjans, I.
dc.contributor.authorGarcía Hernández, J. E.
dc.date.accessioned2016-06-22T10:35:01Z
dc.date.available2016-06-22T10:35:01Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/12410
dc.description.abstractThe different types of zeolites occurring in the hydromagmatic volcano called Montana Escachada or Montana Pelada (Southern Tenerife), have been studied. The instrumental techniques of study include X-ray diffraction, scanning electron microscopy, X-ray fluorescence and microprobe analysis. Phillipsite and analcime were detected in amounts inversely proportional from the basis (more phillipsite) to the top (more analcime) of the volcano. A selective enrichment of the phillipsite in potassium and of the analcime in sodium was also observed. The abundance and the genesis of these zeolites are related to the eruptive mechanism and the physico-chemical conditions of the zone. Their formation is, in high degree, irrespective of the composition of the parent magmaen_US
dc.language.isoengen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherMontana Escachadaen_US
dc.subject.otherHydromagmatismen_US
dc.subject.otherZeolitasen_US
dc.subject.otherFilipsitaen_US
dc.subject.otherAnalcimaen_US
dc.titleZeolites in hydromagmatic volcanoes. A case study of montaña Escachada (Tenerife)en_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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