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Processes of transformation and heoformation of smectites in the volcaniclastic deposits from the La Palma (Canary Islands)

dc.contributor.authorVegas Salamanca, J.
dc.contributor.authorGarcía Romero, E.
dc.contributor.authorMarfil Pérez, Rafaela
dc.date.accessioned2015-03-27T11:25:41Z
dc.date.available2015-03-27T11:25:41Z
dc.date.issued1998
dc.identifier.urihttp://hdl.handle.net/10272/10191
dc.description.abstractClay minerals from the volcaniclastic deposits of the three different sedimentary settings (paleosols, continental lacustrine and transitional, fan delta) have been studied by X-ray, MEB y TEM. The clay fraction of this sediments consist largely of smectite (saponite) with minor irregular chlorite-smectite mixed layers and illite; they occur as replacement of ferromagnesian minerals, plagioclase microlites and glass matrix of the volcarenite and they are inferred to be direct diagenetic alteration products of volcanic componentsen_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.otherSmectiteen_US
dc.subject.otherSaponiteen_US
dc.subject.otherVolcaniclastic depositsen_US
dc.subject.otherDiagenetic alterationen_US
dc.subject.otherCaldera de Taburienteen_US
dc.subject.otherLa Palmaen_US
dc.subject.otherCanary Islandsen_US
dc.titleProcesos de transformación y neoformación de esmectitas en los materiales volcanoclásticos de la isla de La Palma (Canarias)en_US
dc.titleProcesses of transformation and heoformation of smectites in the volcaniclastic deposits from the La Palma (Canary Islands)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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