Published June 25, 1992
| public
Journal Article
Water in mantle minerals
- Creators
- Bell, David R.
Abstract
New experiments suggest that olivine, probably the most abundant mineral in the Earth to a depth of 400 km, can incorporate substantial amounts of hydrogen under water-rich, high-pressure conditions. This work, reported by Bai and Kohlstedt on page 672 of this issue, addresses two basic questions facing those looking at the role of water in the evolution of the Earth: how much is there and where is it stored?
Additional Information
© 1992 Nature Publishing Group.Additional details
- Eprint ID
- 56607
- DOI
- 10.1038/357646a0
- Resolver ID
- CaltechAUTHORS:20150413-133817746
- Created
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2015-04-14Created from EPrint's datestamp field
- Updated
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2021-11-10Created from EPrint's last_modified field