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Tungsten isotopes as tracers of core-mantle interactions: The influence of subducted sediments

Nebel, Oliver; Vroon, P.Z.; Wiggers de Vries, D.F.; Jenner, Frances; Mavrogenes, John

Description

The postulated difference in W isotopic composition of the Earth's core of ∼2 εW units, compared to the bulk silicate earth (BSE) has previously been used to search for evidence of core-mantle interaction (CMI) in ocean island basalts (OIB). The absenc

CollectionsANU Research Publications
Date published: 2010
Type: Journal article
URI: http://hdl.handle.net/1885/53080
Source: Geochimica et Cosmochimica Acta
DOI: 10.1016/j.gca.2009.10.017

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