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Deformation of salt rock joints in time

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Abstract

The results are presented for the deformation testing of joints of salt rocks. The tests on shear with compression were conducted at creep and various loading rates. A structural rheological model of the joint deformation is constructed. Basing on the linear heredity theory, the relations are obtained for describing the process of creep and relaxation.

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REFERENCES

  1. A. A. Baryakh, S. A. Konstantinova, and V. A. Asanov, Deformation of Salt Rocks [in Russian], UrO RAN, Ekaterinburg (1996).

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  2. A. A. Baryakh, V. A. Asanov, I. N. Dudyrev, and I. L. Pan’kov, “Interaction of layers in salt deposit. Report 1. Mechanical properties of joints,” Fiz.-Tekh. Probl. Razrab. Polezn. Iskop., No. 2 (1992).

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  4. I. L. Pan’kov and V. V. Anikin, “Modeling of shear over a clayey interlayer at different loading rates,” in: Proceedings of the International Conference on Geodynamics and Stress State of the Earth’s Bowels [in Russian], IGD SO RAN, Novosibirsk (1999).

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Authors and Affiliations

  1. Mining Institute, Ural Branch, Russian Academy of Sciences, Perm, Russia

    V. A. Asanov & I. L. Pan’kov

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  1. V. A. Asanov
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  2. I. L. Pan’kov
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Additional information

Translated from Fiziko-Tekhnicheskie Problemy Razrabotki Poleznykh Iskopaemykh, No. 4, pp. 40–45, July–August, 2004.

The study was conducted with financial support from the Russian Foundation for Basic Research, Projects Nos. 03-05-64326 and 04-05-96031; Siberian Branch of the Russian Academy of Sciences, Integration Projects Nos. 129 and 191; and Ural Branch of the Russian Academy of Sciences, Integration Project No. 05-11-04.

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Asanov, V.A., Pan’kov, I.L. Deformation of salt rock joints in time. J Min Sci 40, 355–359 (2004). https://doi.org/10.1007/s10913-004-0017-5

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  • DOI: https://doi.org/10.1007/s10913-004-0017-5

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