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Heterogeneity of phonolitic pumice deposits from Tenerife, Canary Islands

dc.contributor.authorWolff, John A.
dc.date.accessioned2018-11-28T13:06:58Z
dc.date.available2018-11-28T13:06:58Z
dc.date.issued1982-07
dc.descriptionInternational Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.en
dc.description.abstractThe island of Tenerife has an extensive Quaternary phonolitic pyroclastic series, comprising plinian pumice-fall deposits, ignimbrites, and pyroclastic surges. The dominant petro­logical feature of these pumice deposits is their geochemical and petrographical heterogeneity. Evidence is presented for three causes of heterogeneity: assimilation of roof-rock by the magma, resulting in less evolved compositions of the first erupted pumice; zonation of the magma chamber, causing a change to intermediate compositions among the last products of an eruption; and magma mixing, where mafic and banded tephra are distributed more or less randomly through a particular pumice deposit.en
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationWOLFF, John A. (1982). Heterogeneity of phonolitic pumice deposits from Tenerife, Canary Islands. "Arquipélago. Série Ciências da Natureza", 3: 231-232.pt_PT
dc.identifier.urihttp://hdl.handle.net/10400.3/4897
dc.language.isoengpt_PT
dc.publisherUniversidade dos Açorespt_PT
dc.subjectPetrologyen
dc.subjectTenerifeen
dc.subjectCanary Islandsen
dc.titleHeterogeneity of phonolitic pumice deposits from Tenerife, Canary Islandsen
dc.typejournal article
dspace.entity.typePublication
oaire.citation.conferencePlacePonta Delgada, Açorespt_PT
oaire.citation.endPage232pt_PT
oaire.citation.startPage231pt_PT
oaire.citation.titleArquipélago. Série Ciências da Naturezapt_PT
oaire.citation.volume3pt_PT
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT

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