Maclennan, John (2010) Mid-ocean ridges: Widening the goal-posts. Nature Geoscience, 3 (4). pp. 229-230. ISSN 1752-0894 EISSN:1752-0908 DOI doi:doi:10.1038/ngeo833
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Official URL: http://dx.doi.org/10.1038/ngeo833
Abstract
Oceanic crust forms through the addition of volcanic rock to mid-ocean ridges. Widely dispersed, young lavas observed at an ultraslow-spreading ridge provide impetus for the redevelopment of models of oceanic magmatism.
Item Type: | Article |
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Uncontrolled Keywords: | 2010AREP; IA60; |
Subjects: | 02 - Geodynamics, Geophysics and Tectonics |
Divisions: | 02 - Geodynamics, Geophysics and Tectonics |
Journal or Publication Title: | Nature Geoscience |
Volume: | 3 |
Page Range: | pp. 229-230 |
Identification Number: | doi:doi:10.1038/ngeo833 |
Depositing User: | Sarah Humbert |
Date Deposited: | 23 Apr 2010 18:40 |
Last Modified: | 23 Jul 2013 09:57 |
URI: | http://eprints.esc.cam.ac.uk/id/eprint/1369 |
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