Coupled Hf-Nd-Pb isotope co-variations of HIMU oceanic island basalts from Mangaia, Cook-Austral islands, suggest an Archean source component in the mantle transition zone

Nebel, Oliver; Arculus, Richard; van Westrenen, Wim; Woodhead, Jonathan; Jenner, Frances; Nebel-Jacobsen, Yona; Wille, Martin; Eggins, Stephen

doi:10.1016/j.gca.2013.03.005

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Coupled Hf-Nd-Pb isotope co-variations of HIMU oceanic island basalts from Mangaia, Cook-Austral islands, suggest an Archean source component in the mantle transition zone

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Nebel, Oliver; Arculus, Richard ; van Westrenen, Wim; Woodhead, Jonathan; Jenner, Frances; Nebel-Jacobsen, Yona; Wille, Martin; Eggins, Stephen

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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

Collections	ANU Research Publications
Date published:	2013
Type:	Journal article
URI:	http://hdl.handle.net/1885/72523
Source:	Geochimica et Cosmochimica Acta
DOI:	10.1016/j.gca.2013.03.005

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Coupled Hf-Nd-Pb isotope co-variations of HIMU oceanic island basalts from Mangaia, Cook-Austral islands, suggest an Archean source component in the mantle transition zone

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