Ratios of S, Se and Te in the silicate Earth require a volatile-rich late veneer
Zaicong Wang () and
Harry Becker ()
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Zaicong Wang: Freie Universität Berlin, Institut für Geologische Wissenschaften, Malteserstrasse 74-100, 12249 Berlin, Germany
Harry Becker: Freie Universität Berlin, Institut für Geologische Wissenschaften, Malteserstrasse 74-100, 12249 Berlin, Germany
Nature, 2013, vol. 499, issue 7458, 328-331
Abstract:
Newly determined ratios and abundances of sulphur, selenium and tellurium in mantle peridotites are consistent with the view that a ‘late veneer’ of slightly volatile-depleted, carbonaceous-chondrite-like material supplied between 20 and 100 per cent of the silicate Earth’s highly volatile elements, such as hydrogen and carbon.
Date: 2013
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Persistent link: https://EconPapers.repec.org/RePEc:nat:nature:v:499:y:2013:i:7458:d:10.1038_nature12285
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DOI: 10.1038/nature12285
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