Thallium isotopes in Iceland and Azores lavas — Implications for the role of altered crust and mantle geochemistry

Details Thallium isotopes in Iceland and Azores lavas — Implications for the role of altered crust and mantle geochemistry Thallium isotopes in Iceland and Azores lavas — Implications for the role of altered crust and mantle geochemistry

Dec 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007e%26psl.264..332n&link_type=abstract

Earth and Planetary Science Letters, Volume 264, Issue 1-2, p. 332-345.

Computer Science

2

Scientific paper

Mantle plumes are commonly perceived to have both a chemical and dynamic link with the subduction of ocean crust into the mantle. In principle, this should lead to the observation of chemical and isotopic signatures that are characteristic of ocean crust and marine sediments in ocean island basalts. This study investigates the thallium (Tl) isotope systematics of lavas from Iceland and the Azores archipelago, in order to determine if their compositions were affected by admixing of ferromanganese sediments or upper ocean crust altered at low temperature. Such materials are known to display strongly fractionated Tl isotope signatures relative to the ambient upper mantle. Two samples from the island of Terceira in the Azores archipelago have Tl isotope compositions significantly different from normal mantle, and this suggests the presence of Fe Mn sediments. Combined Pb and Tl isotope modelling indicates that the Tl anomalies are not a feature of the Azores plume but produced by assimilation of modern Fe Mn sediments during magma ascent through the ocean crust. Excluding these two anomalous lavas from Terceira, the Iceland and Azores samples have identical Tl isotope compositions, with an overall mean of ɛ205Tl = - 1.5 ± 1.4 (2SD, n = 30) that is indistinguishable from the previously estimated upper mantle average (ɛ205Tl = - 2.0 ± 0.5). The near-constant Tl isotope compositions of the Iceland and Azores lavas may indicate that the respective mantle plume sources contain virtually no Fe Mn sediments or altered upper ocean crust. Alternatively, it is possible that the lack of Tl isotope variation reflects quantitative removal of fractionated Tl from the slab during subduction and dehydration. A less straightforward explanation is that past marine environments produced sediments and altered marine basalts with nearly unfractionated Tl isotope compositions. All three scenarios have important implications and future Tl isotope studies will be able to identify the most feasible interpretation.

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