Abstract
A mathematical model is offered to describe thermofluctuation processes of plastic deformation and fissuring in a geomedium. The kinetic coefficients are functions of temperature, mean pressure and stress deviator intensity.
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Translated from Fiziko-Tekhnicheskie Problemy Razrabotki Poleznykh Iskopaemykh, No. 3, pp. 47–52, May–June, 2011.
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Miroshnikov, V.I., Rasskazov, I.Y. & Saksin, B.G. Modeling of anisotropic fissuring process in rocks. J Min Sci 47, 307–311 (2011). https://doi.org/10.1134/S1062739147030063
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DOI: https://doi.org/10.1134/S1062739147030063