Bell, David R. (1992) Water in mantle minerals. Nature, 357 (6380). pp. 646-647. ISSN 0028-0836. doi:10.1038/357646a0. https://resolver.caltech.edu/CaltechAUTHORS:20150413-133817746
Full text is not posted in this repository. Consult Related URLs below.
Use this Persistent URL to link to this item: https://resolver.caltech.edu/CaltechAUTHORS:20150413-133817746
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?
| Item Type: | Article | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| Related URLs: |
| |||||||||
| Additional Information: | © 1992 Nature Publishing Group. | |||||||||
| Issue or Number: | 6380 | |||||||||
| DOI: | 10.1038/357646a0 | |||||||||
| Record Number: | CaltechAUTHORS:20150413-133817746 | |||||||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20150413-133817746 | |||||||||
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | |||||||||
| ID Code: | 56607 | |||||||||
| Collection: | CaltechAUTHORS | |||||||||
| Deposited By: | Tony Diaz | |||||||||
| Deposited On: | 14 Apr 2015 04:30 | |||||||||
| Last Modified: | 10 Nov 2021 21:01 |
Repository Staff Only: item control page
