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Influence of the structure of the current-density function in borehole-electrometry diagnostics of the stress-strain state of rock

  • Rock Mechanics and Mine Pressure
  • Published:
Journal of Mining Science Aims and scope

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Literature Cited

  1. V. N. Oparin, “Determining the orientation of the quasiprincipal stresses by borehole electrometry. Theory of the method, I,” Fiz.-Tekh. Probl. Razrab. Polezn. Iskop., No. 2 (1985).

  2. V. N. Oparin, M. V. Kurlenya, A. P. Tapsiev, and G. G. Matasova, “Determining the orientation of the quasiprincipal stress by borehole electrometry. II. Monitoring apparatus, full-scale tests,” Fiz.-Tekh. Probl. Razrab. Polezn. Iskop., No. 4 (1985).

  3. V. N. Oparin, “Problem of rock geophysics,” Fiz.-Tekh. Probl. Razrab. Polezn. Iskop. No. 1 (1978).

  4. M. V. Kurlenya and V. N. Oparin, “Electrometric method of diagnostics of the stress-strain state of rock masses,” Dokl. Akad. Nauk SSSR,313, No. 1 (1990).

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Authors
  1. V. N. Oparin
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Additional information

Institute of Mining, Siberian Branch, Academy of Sciences of the USSR, Novosibirsk. Translated from Fiziko-Tekhnicheskie Problemy Razrabotki Poleznykh Iskopaemykh, No. 2, pp. 30–34, March–April, 1991.

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Oparin, V.N. Influence of the structure of the current-density function in borehole-electrometry diagnostics of the stress-strain state of rock. Soviet Mining Science 27, 104–108 (1991). https://doi.org/10.1007/BF02500928

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  • DOI: https://doi.org/10.1007/BF02500928

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