Theory and Numerical Simulation of Deep Rock Mass Based on a Non-Euclidean Model

<div>Location of the crest internal stress in surrounding rock mass with different non-Euclidean parameters. (a) <i>ξ</i> = 5.01 GPa. (b) <i>ξ</i> = 5.57 GPa. (c) <i>ξ</i> = 6.13 GPa.</div>

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Figure 11

Figure 11: Theory and Numerical Simulation of Deep Rock Mass Based on a Non-Euclidean Model 