Published June 2010
| public
Journal Article
Oxygen and carbon isotope systematics during natural mineral carbonation in peridotite of the Samail Ophiolite, Oman
Chicago
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Abstract
We are investigating peridotite alteration in the mantle section of the Samail ophiolite in Oman. Understanding the natural system provides insights into design of enhanced, in situ mineral carbonation for CO_2 storage, and 'negative emissions' via enhanced CO_2 capture from surface waters.
Additional Information
© 2010 Published by Elsevier Ltd.Additional details
- Eprint ID
- 39697
- Resolver ID
- CaltechAUTHORS:20130801-092028055
- Created
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2013-08-19Created from EPrint's datestamp field
- Updated
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2021-11-09Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences (GPS)