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Journal article

Iron isotope fractionation and the oxygen fugacity of the mantle.

Abstract:
The oxygen fugacity of the mantle exerts a fundamental influence on mantle melting, volatile speciation, and the development of the atmosphere. However, its evolution through time is poorly understood. Changes in mantle oxidation state should be reflected in the Fe3+/Fe2+ of mantle minerals, and hence in stable iron isotope fractionation. Here it is shown that there are substantial (1.7 per mil) systematic variations in the iron isotope compositions (delta57/54Fe) of mantle spinels. Spinel delta57/54Fe values correlate with relative oxygen fugacity, Fe3+/sigmaFe, and chromium number, and provide a proxy of changes in mantle oxidation state, melting, and volatile recycling.
Publication status:
Published

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Publisher copy:
10.1126/science.1095679

Authors


More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author


Journal:
Science (New York, N.Y.) More from this journal
Volume:
304
Issue:
5677
Pages:
1656-1659
Publication date:
2004-06-01
DOI:
EISSN:
1095-9203
ISSN:
0036-8075


Language:
English
Pubs id:
pubs:152096
UUID:
uuid:7e96a4c2-ac4d-4ba1-9262-8659a7ce487a
Local pid:
pubs:152096
Source identifiers:
152096
Deposit date:
2012-12-19

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