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Evidence for subduction at 3.8 Ga: Geochemistry of arc-like metabasalts from the southern edge of the Isua Supracrustal Belt

Autor: Jenner, F.E., Bennett, V.C., Nutman, A.P., Friend, C.R.L., Norman, M.D., Yaxley, G.

Publikováno v: In Chemical Geology 2009 261(1):83-98

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The use of geochemistry for placing constraints on mantle melting processes and the evolution of mantle heterogeneity

Autor: Jenner, F.E., Jennings, E.S.

Publikováno v: In Reference Module in Earth Systems and Environmental Sciences 2013

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

Autor: Nebel, O., Arculus, R.J., van Westrenen, W., Woodhead, J.D., Jenner, F.E., Nebel-Jacobsen, Y.J., Wille, M., Eggins, S.M.

Publikováno v: Nebel, O, Arculus, R J, van Westrenen, W, Woodhead, J D, Jenner, F E, Nebel-Jacobsen, Y J, Wille, M & Eggins, S M 2013, ' Coupled Hf-Nd-Pb isotope co-variations of HIMU oceanic island basalts suggest an Archean source component in the mantle transition zone ', Geochimica et Cosmochimica Acta, no. 112, pp. 87-101 . https://doi.org/10.1016/j.gca.2013.03.005
Geochimica et Cosmochimica Acta, 87-101. Elsevier Limited
ISSUE=112;STARTPAGE=87;ENDPAGE=101;ISSN=0016-7037;TITLE=Geochimica et Cosmochimica Acta

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 iso

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::a587f979f7208fd465584ef4f8eac89d
https://hdl.handle.net/1871.1/9127cfca-4980-44d1-a911-4f03bf30a0a6