Hirschmann, Marc (1995) Melt pathways in the mantle. Nature, 375 (6534). pp. 737-738. ISSN 0028-0836. doi:10.1038/375737a0. https://resolver.caltech.edu/CaltechAUTHORS:20150610-111023835
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Abstract
OCEANIC ridges are the dominant sites of energy and mass transfer from the Earth's interior to the crust, hydrosphere and atmosphere, but many key processes beneath ridges remain poorly understood. One outstanding problem is how partial melts in the asthenosphere concentrate into channels - initially, melts must leave their source by intergranular percolation, but there is considerable evidence that they are rapidly channelled into larger pathways.
| Item Type: | Article | |||||||||
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| Additional Information: | © 1995 Nature Publishing Group. | |||||||||
| Issue or Number: | 6534 | |||||||||
| DOI: | 10.1038/375737a0 | |||||||||
| Record Number: | CaltechAUTHORS:20150610-111023835 | |||||||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20150610-111023835 | |||||||||
| Official Citation: | Melt pathways in the mantle 737-738 Marc Hirschmann doi:10.1038/375737a0 | |||||||||
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | |||||||||
| ID Code: | 58157 | |||||||||
| Collection: | CaltechAUTHORS | |||||||||
| Deposited By: | Ruth Sustaita | |||||||||
| Deposited On: | 10 Jun 2015 18:24 | |||||||||
| Last Modified: | 10 Nov 2021 22:00 |
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