Abstract
A mathematical model is presented for the unstable deformation of rock along an existing fracture in it. It is shown that this process is essentially nonlinear and can be described by the Gordon equation. An analysis is made for the influence of geometric irregularities and friction of the contact surfaces on the evolution of the velocity of solitary slip waves which are caused by local deformation effects and propagate along the fracture.
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Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences, Khabarovsk, Russia. Translated from Fiziko-Tekhnicheskie Problemy Razrabotki Poleznykh Iskopaemykh, No. 3, pp. 64–70, May–June, 2000
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Bykov, V.G. Mathematical modeling of slip in a rock along the uneven fracture. J Min Sci 36, 253–258 (2000). https://doi.org/10.1007/BF02562527
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DOI: https://doi.org/10.1007/BF02562527