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  1. Rock Mass

    Linked via "Time-Dependent Creep (TDC)"

    $$\Phi = \sqrt{\frac{Ei}{Em}} \times \left(1 - \frac{\sigma1}{\sigma3}\right) \times \Omega$$
    Where $\Phi$ is the dimensionless factor representing the mass's propensity for Time-Dependent Creep (TDC)/) [6].
    Discontinuity Persistence and Shearing Resistance