A kinematic model for recrystallization and texture development in olivine polycrystals

By É. Kaminski, N. Ribe. 2001

176 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/2932415e089dddbe2d50534aed59bf431f2c1a9d

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In Geophysics

Citations in the corpus

Texture and Anisotropy (2004, methodology): “A similar approach was applied by Thorsteinsson (2001, 2002) to ice, and Kaminski and Ribe (2001) applied a kinematic model to olivine.”
Global mantle flow and the development of seismic anisotropy: Differences between the oceanic and continental upper mantle (2007, background): “This is particularly true if the effects of dynamic recrystallization [Kaminski and Ribe, 2001; Kaminski et al., 2004] are taken into account along with finite strain [Becker et al., 2006a].”
Statistical properties of seismic anisotropy predicted by upper mantle geodynamic models (2006, unknown): “Moreover, when using the [Kaminski and Ribe, 2001; Kaminski et al., 2004] approach, the statistical properties of the predicted anisotropic fabrics resemble those of natural samples.”
Importance of crustal corrections in the development of a new global model of radial anisotropy (2010, methodology): “Kinematic modeling of LPO [Kaminski and Ribe, 2001] produced through mantle flow models [e.g., Becker et al., 2008] suggest that upper mantle anisotropy can be well modeled using such an approach, but care must be taken in interpreting the results as different LPO deformation modes are possible…”
Timescales for the evolution of seismic anisotropy in mantle flow (2001, background): “They indicate that l* = 5 and that M* lies between 50 and 200 as a function of temperature [Kaminski and Ribe, 2001].”
Comparison of azimuthal seismic anisotropy from surface waves and finite strain from global mantle-circulation models (2003, methodology): “A coupled model that uses the strain history predicted from a, possibly more sophisticated, circulation model as input for fabric development algorithms such as that of Kaminski & Ribe (2001) should be attempted next.”
D-Rex, a program for calculation of seismic anisotropy due to crystal lattice preferred orientation in the convective upper mantle (2004, methodology): “If χ is close to 0, then the fraction of grains deformed dominantly by grain-boundary sliding is negligible and the model is equivalent to Kaminski & Ribe (2001).”
Radial seismic anisotropy as a constraint for upper mantle rheology (2007, methodology): “Mineral physics theories are able to reproduce laboratory results on the development of olivine LPO (Wenk and Tomé, 1999; Kaminski and Ribe, 2001).”