“…Discontinuities play a critical role in creating a complex fracture network, and the influence of dynamic tension on the evolution of the fracturing network, which should be deeply investigated. Among the published literature, the Brazilian test [10,11], flattened Brazilian disc tests [12][13][14][15][16], Semicircular bending (SCB) test [17], and the split Hopkinson pressure bar (SHPB) tests [18][19][20][21] were mainly adopted to research the mechanical properties of rock material under dynamic tension. It was found that the strength of rock presented rate dependency; rock strength increases with the increase of strain rate, and almost all the studies are focused on dolerite [22], limestone [10], granite [17,19], tuff [21], sandstone [23], and basalt [21].…”