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Investigation of rock slope deformation with time

  • Stepanov V. Y. 
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Summary

An analysis of rheologic processes in slopes is considered on the basis of in situ investigations of deformation development in rock slopes. The value of irreversible and seasonal deformations is determined. Seismic influence on deformation is estimated and the coefficient of viscosity for variously fractured rocks is evaluated.

Keywords

Rock Mass Creep Deformation Rock Slope Maximum Shear Stress Slope Deformation 

Recherches sur les Deformations de Pentes Rocheuses en Fonction du Temps

Résumé

L’article analyse les processus rhéologiques de pentes en se basant sur des recherches in situ concernant le progrès des déformations des talus rocheux. On distingue les valeurs des déformations irréversibles et saisonnières; on estime l’influence des séismes sur la déformation et on évalue le coefficient de viscosité pour des roches diversement fracturées.

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References

  1. GRIGGS D.T. (1939): Creep of rocks. J. Geol. 47, 3.CrossRefGoogle Scholar
  2. GZOVSKY M.V. (1975): Bases of tectonophysics. Science Publishers, Moscow.Google Scholar
  3. LOMNITZ C. (1956): Creep measurements in igneous rocks. J. Geol., 64, 5.CrossRefGoogle Scholar
  4. PHILLIPS D.W. (1948): Tectonics of mining. Colliery Engr., June–Oct.Google Scholar
  5. UKHOV S.B. (1975): Rock foundations of hydrotechnical constructions. Energy Publishers, Moscow.Google Scholar
  6. YERZHANOV Zh.S. (1964): Theory of creep in rock and its application. Science Publishers, Alma-Ata.Google Scholar
  7. YERZHANOV Zh.S. et al. (1970): Creep in sedimentary rock. Science Publishers, Alma-Ata.Google Scholar

Copyright information

© International Association of Engineering Geology 1978

Authors and Affiliations

  • Stepanov V. Y. 
    • 1
  1. 1.Institute of Rock Physics and Rock MechanicsAcademy of Sciences of the Kirghiz S.S.R.FrunzeUSSR

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