Wyllie, Peter J. and Huang, Wuu-Liang (1975) Influence of mantle CO_2 in the generation of carbonatites and kimberlites. Nature, 257 (5524). pp. 297-299. ISSN 0028-0836. https://resolver.caltech.edu/CaltechAUTHORS:20160129-130856739
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Abstract
The explanation of why partial fusion of mantle peridotite sometimes yields basalts, sometimes kimberlites and sometimes carbonatites is given by the phase relationships in the system CaO–MgO–SiO_2–CO_2. The key is the intersection of a sub-solidus carbonation reaction with the solidus, which introduces carbonates as primary minerals alongside silicates on the surface of the liquidus.
| Item Type: | Article | |||||||||
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| Alternate Title: | Influence of mantle CO2 in the generation of carbonatites and kimberlites | |||||||||
| Additional Information: | © 1975 Nature Publishing Group. Received July 2; accepted July 22, 1975. This work was supported by the NSF. | |||||||||
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| Issue or Number: | 5524 | |||||||||
| Record Number: | CaltechAUTHORS:20160129-130856739 | |||||||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20160129-130856739 | |||||||||
| Official Citation: | Influence of mantle CO2 in the generation of carbonatites and kimberlites PETER J. WYLLIE & WUU-LIANG HUANG Nature 257, 297 - 299 (25 September 1975); doi:10.1038/257297a0 | |||||||||
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | |||||||||
| ID Code: | 64097 | |||||||||
| Collection: | CaltechAUTHORS | |||||||||
| Deposited By: | Tony Diaz | |||||||||
| Deposited On: | 29 Jan 2016 21:46 | |||||||||
| Last Modified: | 03 Oct 2019 09:34 |
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