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GEOMECHANICAL MONITORING OF A ROCK MASS IN AREAS OF GEOLOGIC FAILURES
Abstract
Deforming processes in areas of geologic failures (tectonic faults, boundary zones of block structures etc.) have the singularities in comparison with those, flowing past on "quiet" sites of rock masses. The intensive assimilation of underground space in most cases reduces in a modification of structural organization of a mining massif. In turn development of new structures or "revival" old is accompanied by adjustments on growing or available faults and is exhibited as strains of a surface and seismic pushes (in a general sense of this word) different force. The hazard of origin of extreme situations especially will increase at assimilation of underground space in zones of geodynamic activity. For safe assimilation of underground space especially in the special zones are necessary organization of an effective system of tracing, forecasting and controls by deformation processes and know by the mechanism of deformation processes in such areas.
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References3
1. Zhuravkov M.A. Deforming processes and failure processes in block-layered mas- sif. // Int. symp. on deformation and progressive failure in geomechanics. Nagoya. Japan. 1997.
2. Zhuravkov M.A., Smuchnic A.D. The design of geomonitoring systems. Minsk. Pub. by BelABG, 1997. 189 p.
3. Zhuravkov M.A., Andreyko S.S., Martunenko M.D. The system of geomechanical moni-toring for block-layered massif of salt rock.// Mine planning and equipment selection'95. Ed. by Singhal. Balkema, Rotterdam. Brook-field., 1995. P.1109-1113
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