The structure of 2D mantle convection and stress fields: Effects of viscosity distribution
Author:
Publisher
Pleiades Publishing Ltd
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
http://link.springer.com/content/pdf/10.1134/S1069351311060012.pdf
Reference25 articles.
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2. Bobrov, A.M. and Trubitsyn, A.P., Numerical Model of the Supercontinental Cycle Stages: Integral Transfer of the Oceanic Crust Material and Mantle Viscous Shear Stresses, Stud. Geophys. Geod, 2008, vol. 52, pp. 87–100.
3. Brunei, D. and Machetel, P., Large-Scale Tectonic Feature Induced by Mantle Avalanches with Phase, Temperature, and Pressure Lateral Variations of Viscosity, J. Geophys. Res., 1998, vol. 103, pp. 4929–4945.
4. Bunge, H.-P., Richards, M.A., and Baumgardner, J.R., Effect of Depth-Dependent Viscosity on the Planform of Mantle Convection, Nature, 1996, vol. 379, pp. 436–438.
5. Bunge, H.-P., Richards, M.A., and Baumgardner, J.R., A Sensitivity Study of Three-Dimensional Spherical Mantle Convection at 108 Rayleigh Number: Effects of Depth-Dependent Viscosity, Heating Mode, and An Endothermic Phase Change, J. Geophys. Res., 1997, vol. 102, pp. 11 991–12 007.
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1. The mantle convection model with non-Newtonian rheology and phase transitions: The flow structure and stress fields;Izvestiya, Physics of the Solid Earth;2016-01
2. The structure of mantle flows and stress fields in a two-dimensional convection model with non-Newtonian viscosity;Russian Geology and Geophysics;2014-07-01
3. Horizontal stresses in the mantle and in the moving continent for the model of two-dimensional convection with varying viscosity;Izvestiya, Physics of the Solid Earth;2011-08-23
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