Horizontal stresses in the mantle and in the moving continent for the model of two-dimensional convection with varying viscosity
Author:
Publisher
Pleiades Publishing Ltd
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
http://link.springer.com/content/pdf/10.1134/S1069351311090023.pdf
Reference16 articles.
1. Baranov, A.A. and Bobrov, A.M., The Structure of 2D Mantle Convection and Stress Fields: Effects of Viscosity Distribution, Izv. Phys. Earth, 2011, vol. 47, no. 7, pp. 575–585.
2. Bobrov, A.M., Jacoby, W., and Trubitsyn, V.P., Effects of Rayleigh Number, Length and Thickness of Continent on Time of Mantle Flow Reversal, J. Geodynam., 1999, vol. 27, pp. 133–145.
3. 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.
4. Davaille, A., Stutzmann, E., Silveira, G., Besse, J. and Courtillot, V., Convective Patterns under the Indo-Atlantic “Box,” Earth Planet. Sci. Lett., 2005, vol. 239, pp. 233–252.
5. Gurnis, M., Large-Scale Mantle Convection and the Aggregation and Dispersal of Supercontinents, Nature, 1988, vol. 332, pp. 696–699.
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