2023 Jishishan Earthquake-triggered river terrace landslide enabled by tectonic and human activities

Zonglin Zhang, Runqiang Zeng, Shufen Zhao, Ziran Wei, Xingmin Meng, Zhao Long, Xiaorui Wang, Tianjun Qi, Ruihuan Su, Bing Wu, Jianhua Ma, Dongxia Yue, Guan Chen, Yi Zhang, Yajun Li, Yan Zhao
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Abstract

The continued increase in demand for food is such that flood-irrigation-based agricultural techniques are not expected to change in the future. Consequently, in cultivated areas dominated by river terraces that experience neotectonic movements, catastrophes caused by earthquakes that trigger material liquefaction may continue to occur. Among such catastrophes, low-angle, ultra-long-distance landslides induced by synergistic effects of tectonic and human activities are events that are not fully understood but can potentially be mitigated. A landslide-mudflow that occurred on December 18, 2023, during an Ms 6.2 earthquake in Jishishan, China, on the tertiary terrace of the Yellow River. We reveal the causal mechanisms by which geomorphology, tectonics, and human activities controlled the landslide-mudflow, and outline a new, potentially widespread, dual liquefaction layer-dominated failure mode for earthquake-induced landslides on river terraces. Our findings serve as a warning that urgent landslide-potential assessments should be conducted across river terrace irrigation areas in tectonically active regions.

Abstract Image

2023 年 积石山地震引发的河流阶地滑坡 地质构造和人类活动造成的滑坡
由于对粮食的需求持续增长,预计未来以洪水灌溉为主的农业技术不会改变。因此,在以河流阶地为主、经历新构造运动的耕地地区,由地震引发的物质液化灾难可能会继续发生。在这些灾难中,由构造运动和人类活动的协同效应引发的低角度、超长距离滑坡是尚未完全了解但有可能减轻的事件。2023 年 12 月 18 日,在中国积石山发生的 Ms 6.2 级地震中,黄河三级阶地发生了滑坡泥石流。我们揭示了地貌、构造和人类活动控制滑坡-泥石流的因果机制,并概述了地震诱发河流阶地滑坡的一种新的、可能广泛存在的、以双液化层为主的破坏模式。我们的发现警示人们,应在构造活跃地区的河流阶地灌区开展紧急滑坡潜力评估。
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