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The Horizontal Basalts of Agulo (La Gomera)

dc.contributor.authorHerrera, Raquel
dc.contributor.authorAncochea, Eumenio
dc.contributor.authorHuertas, María José
dc.date.accessioned2014-11-19T09:43:26Z
dc.date.available2014-11-19T09:43:26Z
dc.date.issued2002
dc.identifier.urihttp://hdl.handle.net/10272/9351
dc.description.abstractThe "Horizontal Basalts" in the Agulo area are made up of a more than 600m thick succession of basaltic flows that filled a SW-NE trending paleo-valley. Compositions vary between picrite and trachybasalt. The lithologic and geochemical variability of these rocks indicates that they were generated mainly by fractional crystallization. The recognition of several evolution cycles suggests the involvement of other processes that modify the general fractional crystallization trenden_US
dc.language.isospaen_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.otherHorizontal Basaltsen_US
dc.subject.otherFractional crystallizationen_US
dc.subject.otherLa Gomeraen_US
dc.subject.otherCanary Islandsen_US
dc.titleLos Basaltos Horizontales de Agulo (La Gomera)en_US
dc.titleThe Horizontal Basalts of Agulo (La Gomera)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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