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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Isotopes
transition zone
Archean
basalt
isotope
mantle
age structure
oceanic crust
Chemical analysis

Cite this

Nebel, O. ; Arculus, R.J. ; van Westrenen, W. ; Woodhead, J.D. ; Jenner, F.E. ; Nebel-Jacobsen, Y.J. ; Wille, M. ; Eggins, S.M. / Coupled Hf-Nd-Pb isotope co-variations of HIMU oceanic island basalts suggest an Archean source component in the mantle transition zone. In: Geochimica et Cosmochimica Acta. 2013 ; No. 112. pp. 87-101.
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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",
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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.

In: Geochimica et Cosmochimica Acta, No. 112, 2013, p. 87-101.

Research output: Contribution to JournalArticleAcademicpeer-review

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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 -