Application of D-CRDM Method in Columnar Jointed Basalts Failure Analysis

Figure 4

Evolution characteristics of the successive yielding in CRDM.

(a)   Evolution of the yielding surface in the 𝜋 surface

(b) Isoclinic scaling of the yielding surface in the 𝜋 surface

(c) Isoclinic scaling of the yielding surface