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dc.contributor.authorColtice, N.
dc.contributor.authorBertrand, H.
dc.contributor.authorRey, P.
dc.contributor.authorJourdan, Fred
dc.contributor.authorPhillips, B. R.
dc.contributor.authorRicard, Y.
dc.date.accessioned2017-01-30T15:39:06Z
dc.date.available2017-01-30T15:39:06Z
dc.date.created2009-06-21T20:01:34Z
dc.date.issued2009
dc.identifier.citationColtice, Nicolas and Bertrand, Herve and Rey, Patrice and Jourdan, Fred and Phillips, Benjamin R. and Ricard, Yanick. 2009. Global warming of the mantle beneath continents back to the Archaean. Gondwana Research 15: pp. 254-266.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/48350
dc.identifier.doi10.1016/j.gr.2008.10.001
dc.description.abstract

Throughout its history, the Earth has experienced global magmatic events that correlate with the formationof supercontinents. This suggests that the distribution of continents at the Earth's surface is fundamental inregulating mantle temperature. Nevertheless, most large igneous provinces (LIPs) are explained in terms ofthe interaction of a hot plume with the lithosphere, even though some do not show evidence for such amechanism. The aggregation of continents impacts on the temperature and flow of the underlying mantlethrough thermal insulation and enlargement of the convection wavelength. Both processes tend to increasethe temperature below the continental lithosphere, eventually triggering melting events without theinvolvement of hot plumes. This model, called mantle global warming, has been tested using 3D numericalsimulations of mantle convection [Coltice, N., Phillips, B.R., Bertrand, H., Ricard, Y., Rey, P. (2007) Globalwarming of the mantle at the origin of flood basalts over supercontinents. Geology 35, 391–394.]. Here, weapply this model to several continental flood basalts (CFBs) ranging in age from the Mesozoic to theArchaean. Our numerical simulations show that the mantle global warming model could account for thepeculiarities of magmatic provinces that developed during the formation of Pangea and Rodinia, as well asputative Archaean supercontinents such as Kenorland and Zimvaalbara.

dc.publisherElsevier Science BV
dc.titleGlobal warming of the mantle beneath continents back to the Archaean
dc.typeJournal Article
dcterms.source.volume15
dcterms.source.startPage254
dcterms.source.endPage266
dcterms.source.issn1342937X
dcterms.source.titleGondwana Research
curtin.note

The link to the journal’s home page is: http://www.elsevier.com/wps/find/journaldescription.cws_home/706719/description#description

curtin.note

Copyright © 2009 Elsevier B.V. All rights reserved

curtin.accessStatusOpen access
curtin.facultyDepartment of Applied Geology
curtin.facultyFaculty of Science and Engineering
curtin.facultyWA School of Mines


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