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

doi:10.1016/j.gca.2013.03.005

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

Geology and Geochemistry

Research output: Contribution to Journal › Article › Academic › peer-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 language	English
Pages (from-to)	87-101
Journal	Geochimica et Cosmochimica Acta
Issue number	112
DOIs	https://doi.org/10.1016/j.gca.2013.03.005
Publication status	Published - 2013

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10.1016/j.gca.2013.03.005

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

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=",

author = "O. Nebel and R.J. Arculus and {van Westrenen}, W. and J.D. Woodhead and F.E. Jenner and Y.J. Nebel-Jacobsen and M. Wille and S.M. Eggins",

year = "2013",

doi = "10.1016/j.gca.2013.03.005",

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pages = "87--101",

journal = "Geochimica et Cosmochimica Acta",

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T1 - Coupled Hf-Nd-Pb isotope co-variations of HIMU oceanic island basalts suggest an Archean source component in the mantle transition zone

AU - Nebel, O.

AU - Arculus, R.J.

AU - van Westrenen, W.

AU - Woodhead, J.D.

AU - Jenner, F.E.

AU - Nebel-Jacobsen, Y.J.

AU - Wille, M.

AU - Eggins, S.M.

PY - 2013

Y1 - 2013

N2 - 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=

AB - 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=

U2 - 10.1016/j.gca.2013.03.005

DO - 10.1016/j.gca.2013.03.005

M3 - Article

SP - 87

EP - 101

JO - Geochimica et Cosmochimica Acta

JF - Geochimica et Cosmochimica Acta

SN - 0016-7037

IS - 112

ER -

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

Abstract

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