Redox-influenced seismic properties of upper-mantle olivine
C. J. Cline (),
U. H. Faul,
E. C. David,
A. J. Berry and
I. Jackson
Additional contact information
C. J. Cline: Research School of Earth Sciences, Australian National University
U. H. Faul: Earth Atmospheric and Planetary Sciences, Massachusetts Institute of Technology
E. C. David: Research School of Earth Sciences, Australian National University
A. J. Berry: Research School of Earth Sciences, Australian National University
I. Jackson: Research School of Earth Sciences, Australian National University
Nature, 2018, vol. 555, issue 7696, 355-358
Abstract:
Redox conditions and associated defect chemistry rather than water content, as previously thought, strongly influence the seismic properties of olivine, the main constituent mineral of Earth’s upper mantle.
Date: 2018
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Persistent link: https://EconPapers.repec.org/RePEc:nat:nature:v:555:y:2018:i:7696:d:10.1038_nature25764
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DOI: 10.1038/nature25764
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