Melting during late-stage rifting in Afar is hot and deep

Ferguson, D. J. and Maclennan, J. and Bastow, I. D. and Pyle, D. M. and Jones, S. M. and Keir, D. and Blundy, J. D. and Plank, T. and Yirgu, G. (2013) Melting during late-stage rifting in Afar is hot and deep. Nature, 499 (7456). pp. 70-73. ISSN 0028-0836, ESSN: 1476-4687 DOI 10.1038/nature12292

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Official URL: http://www.nature.com/nature/journal/v499/n7456/fu...

Abstract

Investigations of a variety of continental rifts and margins worldwide have revealed that a considerable volume of melt can intrude into the crust during continental breakup, modifying its composition and thermal structure. However, it is unclear whether the cause of voluminous melt production at volcanic rifts is primarily increased mantle temperature or plate thinning. Also disputed is the extent to which plate stretching or thinning is uniform or varies with depth with the entire continental lithospheric mantle potentially being removed before plate rupture. Here we show that the extensive magmatism during rifting along the southern Red Sea rift in Afar, a unique region of sub-aerial transition from continental to oceanic rifting, is driven by deep melting of hotter-than-normal asthenosphere. Petrogenetic modelling shows that melts are predominantly generated at depths greater than 80 kilometres, implying the existence of a thick upper thermo-mechanical boundary layer in a rift system approaching the point of plate rupture. Numerical modelling of rift development shows that when breakup occurs at the slow extension rates observed in Afar, the survival of a thick plate is an inevitable consequence of conductive cooling of the lithosphere, even when the underlying asthenosphere is hot. Sustained magmatic activity during rifting in Afar thus requires persistently high mantle temperatures, which would allow melting at high pressure beneath the thick plate. If extensive plate thinning does occur during breakup it must do so abruptly at a late stage, immediately before the formation of the new ocean basin.

Item Type: Article
Uncontrolled Keywords: 2013AREP, IA66,
Subjects: 05 - Petrology - Igneous, Metamorphic and Volcanic Studies
Divisions: 05 - Petrology - Igneous, Metamorphic and Volcanic Studies
Journal or Publication Title: Nature
Volume: 499
Page Range: pp. 70-73
Identification Number: 10.1038/nature12292
Depositing User: Sarah Humbert
Date Deposited: 07 Jul 2013 01:56
Last Modified: 08 Aug 2013 12:12
URI: http://eprints.esc.cam.ac.uk/id/eprint/2829

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