Paleowattmeters: A scaling relation for dynamically recrystallized grain size

By N. Austin, B. Evans. 2007

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Mechanisms for the generation of plate tectonics by two-phase grain-damage and pinning (2012, methodology): “…invariably entails an increase in surface free energy, which is drawn from deformational work (Bercovici and Ricard, 2005; Landuyt et al., 2008; Ricard and Bercovici, 2009; Rozel et al., 2011) and this has been verified with experiments and the “paleowattmeter” relations of Austin and Evans (2007).”
Implications of grain size evolution on the seismic structure of the oceanic upper mantle (2008, methodology): “196 Behn et al.: Grain-size evolution in the oceanic upper mantle, revised for EPSL March 2008 We compare the Hall & Parmentier (2003) and Austin & Evans (2007) models to 197 experimental data on wet (600 H/106Si) and dry (50 H/106Si) olivine (Karato et al., 1980; Van 198 der Wal et al., 1993).”