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Magma mixing at oceanic transform fracture zones

dc.contributor.authorFlower, Martin F. J.
dc.date.accessioned2018-11-29T09:39:01Z
dc.date.available2018-11-29T09:39:01Z
dc.date.issued1982-07
dc.descriptionInternational Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.en
dc.description.abstractOcean ridge eruptive chemistry reflects isochronic compositional «gradients», often attributed to the interaction of lithophile element-rich mantle plumes with the relatively depleted asthenosphere. Inspection of Atlantic and Pacific axial gradients shows lithophile-rich eruptions do not correspond exclusively to proposed loci for mantle upwelling. In contrast, transform fracture zones appear to mark the majority of lithophile-enrichment peaks, suggesting relatively superficial tectonic phenomena influence magma chemistry. A general association of lithophile and radiogenic isotope enrichment with increasingly frequent offset spreading culminates at major fracture zone ridge axis intersections (e.g., Galapagos, Iceland, Azores, Jan Mayen, and Siqueiros, Oceanographer and Romanche fracture zones). Major element and normative compositions show that enrichment also coincides with increased depth of melt segregation in the mantle. […].en
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationFLOWER, Martin F. J. (1982). Magma mixing at oceanic transform fracture zones. "Arquipélago. Série Ciências da Natureza", 3: 199-200.pt_PT
dc.identifier.urihttp://hdl.handle.net/10400.3/4899
dc.language.isoengpt_PT
dc.publisherUniversidade dos Açorespt_PT
dc.subjectGeochemistryen
dc.subjectVolcanic Soilsen
dc.titleMagma mixing at oceanic transform fracture zonesen
dc.typejournal article
dspace.entity.typePublication
oaire.citation.conferencePlacePonta Delgada, Açorespt_PT
oaire.citation.endPage200pt_PT
oaire.citation.startPage199pt_PT
oaire.citation.titleArquipélago. Série Ciências da Naturezapt_PT
oaire.citation.volume3pt_PT
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT

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