Dynamic compression properties of a saturated white sandstone under ambient sub-zero temperatures

Dynamic Mechanical Properties of Dry and Water-Saturated

Comparison of Mechanical Properties of Dry, Saturated and Frozen Porous Rocks

The inside‐out model of fracture propagation. (a) Locations of the

Rock stress–strain curve under different temperature (left) and

Effect of sub-zero temperature on dynamic mode II fracture

Dynamic mode I fracture properties of saturated white sandstone

Dynamic Tensile Mechanical Properties and Fracture Characteristics

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Comparisons of the dynamic stress–strain curves between the dry and