Abstract
| Original language | English |
|---|---|
| Pages (from-to) | 87-101 |
| Journal | Geochimica et Cosmochimica Acta |
| Issue number | 112 |
| DOIs | |
| Publication status | Published - 2013 |
Fingerprint
Cite this
}
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 Journal › Article › Academic › peer-review
TY - JOUR
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 -