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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W. Westrenen | S. Eggins | R. Arculus | M. Wille | J. Woodhead | F. Jenner | O. Nebel | Y. Nebel-Jacobsen