“…Slopes in complex geological conditions, e.g., fractured rocks, veins, interfaces, near an active fault zone, are prone to fail due to various triggering factors, especially earthquake hazards [23][24][25][26][27][28][29][30]. Therefore, the stability of slopes should be carefully evaluated by considering different working scenarios, for example, long-term, transient, and accidental cases [21,22] with the utilization of different analysis methods.…”