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Los Basaltos Horizontales de Agulo (La Gomera)

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dc.contributor.authorHerrera, R.
dc.contributor.authorAncochea Soto, Eumenio
dc.contributor.authorHuertas Coronel, María José
dc.date.accessioned2023-06-20T17:28:51Z
dc.date.available2023-06-20T17:28:51Z
dc.date.issued2002-11
dc.description.abstractThe "Horizontal Basalts" in the Agulo area are made up of a more than 600m thick succession of basaltie 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 crystalization. The recognition of several evolution cycles suggests the involvement of other processes that modify the general fractional crystallization trend.
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/9937
dc.identifier.issn0213-683X
dc.identifier.officialurlhttp://www.sociedadgeologica.es/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/58289
dc.issue.number32
dc.journal.titleGeogaceta
dc.language.isospa
dc.page.final70
dc.page.initial67
dc.publisherSociedad Geológica de España
dc.rights.accessRightsopen access
dc.subject.cdu552.3(460.411)
dc.subject.keywordHorizontal Basalts
dc.subject.keywordFractional crystallization
dc.subject.keywordLa Gomera
dc.subject.keywordCanary Islands
dc.subject.ucmPetrología
dc.titleLos Basaltos Horizontales de Agulo (La Gomera)
dc.typejournal article
dspace.entity.typePublication
relation.isAuthorOfPublication5a353ace-8a94-4f6e-8a98-20878931274b
relation.isAuthorOfPublicationc39a1f37-2172-44cf-81b2-a56171ec7b5f
relation.isAuthorOfPublication.latestForDiscovery5a353ace-8a94-4f6e-8a98-20878931274b

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