Coupled Hf-Nd-Pb isotope co-variations of HIMU oceanic island basalts suggest an Archean source component in the mantle transition zone

O. Nebel, R.J. Arculus, W. van Westrenen, J.D. Woodhead, F.E. Jenner, Y.J. Nebel-Jacobsen, M. Wille, S.M. Eggins

Research output: Contribution to JournalArticleAcademicpeer-review

Abstract

Although it is widely accepted that oceanic island basalts (OIB) sample geochemically distinct mantle reservoirs including recycled oceanic crust, the composition, age, and locus of these reservoirs remain uncertain. OIB with highly radiogenic Pb isotope signatures are grouped as HIMU (high-μ, with μ=
Original languageEnglish
Pages (from-to)87-101
JournalGeochimica et Cosmochimica Acta
Issue number112
DOIs
Publication statusPublished - 2013

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