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Seismic and electric anisotropy as the stress state indicator in a fractured rock mass

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Journal of Mining Science Aims and scope

Abstract

The present paper offers the parameter of anisotropy for the use in processing experimental data of the joint seismic and electric monitoring with the aim of studying the process of consolidation in a fractured rock mass under a strong seismic load. Based on the interpreted experimental results, a seismic-electrical model is constructed for the epicenter zone of the Altai earthquake occurred on September 27, 2003.

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Authors and Affiliations

  1. Institute of Geophysics, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russia

    Yu. A. Dashevskii, V. A. Kulikov, N. N. Nevedrova, B. E. Moiseev & M. Yu. Podberezhny

  2. Federal State Unitary Enterprise, Siberian Scientific-Research Institute of Geology, Geophysics and Mineral Raw Material, Novosibirsk, Russia

    O. M. Sagaidachnaya & K. A. Dunaeva

Authors
  1. Yu. A. Dashevskii
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  2. V. A. Kulikov
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  3. N. N. Nevedrova
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  4. B. E. Moiseev
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  5. M. Yu. Podberezhny
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  6. O. M. Sagaidachnaya
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  7. K. A. Dunaeva
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Translated from Fiziko-Tekhnicheskie Problemy Razrabotki Poleznykh Iskopaemykh, No. 4, pp. 31–46, July–August, 2006.

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Dashevskii, Y.A., Kulikov, V.A., Nevedrova, N.N. et al. Seismic and electric anisotropy as the stress state indicator in a fractured rock mass. J Min Sci 42, 335–348 (2006). https://doi.org/10.1007/s10913-006-0062-3

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  • DOI: https://doi.org/10.1007/s10913-006-0062-3

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