Journal of Mining Science

, Volume 31, Issue 2, pp 87–96 | Cite as

Shock capacity of the “southern” polymetallic deposit in Primor'ye

  • Y. Y. Pilenkov
Rock Mechanics


1. The tendency of the rock mass of the Southern Deposit to mine shocks is a result of leftward-shifting tectonic dislocations of the earth's core, which are characteristic for Primor'ye, and which were caused by the following: recrystallization of rocks as a result of their contact metamorphism, effected by deep magmatic injections formed in the area of separations in the sedimentary cover; an accumulation of potential tectonic-strain energy in the body of the intrusion; and, discrete settlement of the underworked structural blocks in the worked space of the deposit, which occurs along the planes of tectonic faults.

2. The development of mine shocks in the deposit is basically the result of activation of the neotectonic mobility of disjunctive faults making up the Eldorado fault zone, and definable working of the ore veins.

3. Seasonal influxes of surface water to mine workings increases the number of manifestations of mine pressure in dynamic form.


Rock Mass Fault Zone Sedimentary Cover Structural Block Dynamic Form 
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  1. 1.
    Yu. Yu. Pilenkov and V. I. Doroshenko, Shock Risk of the Southern Deposit, System Modeling of Mining Technology [in Russian], Institut Gornogo Dela, Sibirskoe Otdelenie Rossiiskogo Akademii Nauk SSSR, Novosibirsk (1989).Google Scholar
  2. 2.
    Yu. Yu. Pilenkov and A. V. Antipov, “Shock-risk situation in the Primorsk Mine,” Tsv. Metal., No. 8 (1990).Google Scholar
  3. 3.
    Yu. Yu. Pilenkov, A. M. Freidin, V. I. Doroshenko, and A. V. Antipov, "Assessment of natural factors in the formation of shock risk in the Southern Deposit," in: Mine Pressure and the Technology of Underground Ore Excavation at Great Depths [in Russian], Akademii Nauk SSSR, Moscow (1990).Google Scholar
  4. 4.
    Yu. Yu. Pilenkov, V. V. Doroshenko, and A. M. Freidin, "Geomechanical assessment and refinement of mining technology in the Southern Polymetallic Deposit," in: Improving the Efficiency of Underground Mining of Ore Deposits in Siberia And the Far East [in Russian], Nauka, Novosibirsk (1992).Google Scholar
  5. 5.
    P. N. Nikolaev, Procedure for Tectonodynamic Analysis [in Russian], Nedra, Moscow (1992).Google Scholar
  6. 6.
    V. P. Utkin, Shear Dislocations, Magmatism, and Ore Formation [in Russian], Nauka, Moscow (1989).Google Scholar
  7. 7.
    D. Rice, Mechanics of the Earthquake Center [Russian translation], Mir, Moscow (1982).Google Scholar
  8. 8.
    D. N. Osokina, O. V. Gushchenko, V. I. Lykov, et al., "Modeling local fields of tectonic stresses caused by systems of deep fractures," in: Stress Fields and Deformations in the Lithosphere [in Russian], Nauka, Moscow (1979).Google Scholar
  9. 9.
    A. V. Mikhailova, Deformation Fields During Overthrust Formation in Models of Structures in Longitudinal Compression, ibid.Google Scholar
  10. 10.
    I. M. Petukhov and I. M. Patugina, Geodynamic Zoning for the Design and Operation of Mines [in Russian], Nedra, Moscow (1988).Google Scholar
  11. 11.
    V. Wittke, Rock Mechanics [Russian translation], Nedra, Moscow (1990).Google Scholar
  12. 12.
    Introduction to Rock Mechanics [Russian translation], edited by C. Bock, Mir, Moscow (1983).Google Scholar
  13. 13.
    E. Isaacson, Rock Pressure in Mines [Russian translation], Gosgortekhizdat, Moscow (1961).Google Scholar

Copyright information

© Plenum Publishing Corporation 1995

Authors and Affiliations

  • Y. Y. Pilenkov
    • 1
  1. 1.Ural Mine BureauEkaterinburg

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