RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 19, ES2002, doi:10.2205/2019ES000659, 2019
Figure 6. Changes in the stress intensity from the time recorded at the point $A$ which is 1.2 m away from the center of the shaft with HLRW.
Citation: Tatarinov V. N., V. N. Morozov, A. S. Batugin (2019), An underground research laboratory: new opportunities in the study of the stress-strain state and dynamics of rock mass destruction, Russ. J. Earth Sci., 19, ES2002, doi:10.2205/2019ES000659.
Copyright 2019 by the Geophysical Center RAS.
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