Coupled Hf-Nd-Pb isotope co-variations of HIMU oceanic island basalts suggest an Archean source component in the mantle transition zone
- Nebel, O.
- Arculus, R.J.
- van Westrenen, W.
- Woodhead, J.D.
- Jenner, F.E.
- Nebel-Jacobsen, Y.J.
- Wille, M.
- Eggins, S.M.
DOIAbstract
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
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