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Trace element evidence for the origin of ocean-island basalts
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1991
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Marine GeologyEngineeringTrace Element GeochemistryPaleoceanographyMantle SourcesGeologyGeological DataGeochemistryOklahoma 73019GeochronologyTrace Element EvidenceEarth ScienceRegional GeologyMantle GeochemistryTectonics
Research Article| February 01, 1991 Trace element evidence for the origin of ocean-island basalts Barry L. Weaver Barry L. Weaver 1School of Geology and Geophysics, University of Oklahoma, Norman, Oklahoma 73019 Search for other works by this author on: GSW Google Scholar Author and Article Information Barry L. Weaver 1School of Geology and Geophysics, University of Oklahoma, Norman, Oklahoma 73019 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1991) 19 (2): 123–126. https://doi.org/10.1130/0091-7613(1991)019<0123:TEEFTO>2.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Barry L. Weaver; Trace element evidence for the origin of ocean-island basalts. Geology 1991;; 19 (2): 123–126. doi: https://doi.org/10.1130/0091-7613(1991)019<0123:TEEFTO>2.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Ocean-island basalt (OIB) suites display significant and consistent differences in highly incompatible trace element ratios between islands which have end-member radiogenic isotope signatures. OIB derived from sources with a high U/Pb ratio have trace element characteristics consistent with a source dominated by recycled ancient oceanic crust. OIB derived from the isotopically distinct enriched mantle sources have trace element characteristics best interpreted in terms of sources which are mixtures of high U/Pb OIB with minor amounts (a few percent) of recycled sedimentary (pelagic and terrigenous) components. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.