2020
DOI: 10.1016/j.enggeo.2019.105391
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Relationship between earthquake-induced excess pore water pressure and strong ground motion observed in a monitored fill slope

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Cited by 8 publications
(1 citation statement)
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“…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.…”
Section: Introductionmentioning
confidence: 99%
“…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.…”
Section: Introductionmentioning
confidence: 99%