A thermodynamically self-consistent damage equation for grain size evolution during dynamic recrystallization
Author:
Affiliation:
1. aboratoire des Sciences de la Terre, CNRS, Université de Lyon 1, ENSL 46 allée d'Italie, F-69364 Lyon, Cedex 07, France. E-mail: antoinerozel@yahoo.fr
2. Department of Geology and Geophysics, Yale University, New Haven, Connecticut, USA
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/184/2/719/27639131/184-2-719.pdf
Reference81 articles.
1. Theories of normal grain growth in pure single phase systems;Atkinson;Acta. Metall.,1988
2. Paleowattmeters: a scaling relation for dynamically recrystallized grain size;Austin;Geology,2007
3. A simple model of plate generation from mantle flow;Bercovici;Geophys. J. Int.,1993
4. A source-sink model of the generation of plate tectonics from non-newtonian mantle flow;Bercovici;J. geophys. Res.,1995
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