新近系黄土-红层滑坡典型控滑斜坡结构及其致灾机理：综述与展望

李坤; 孙萍; 王浩杰; 张帅; 李冉; 桑康云

doi:10.3799/dqkx.2025.265

Volume 51 Issue 2

Feb. 2026

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Article Navigation > Earth Science > 2026 > 51(2): 578-601

Li Kun, Sun Ping, Wang Haojie, Zhang Shuai, Li Ran, Sang Kangyun, 2026. Typical SlopeStructures and Their Sliding Control Mechanisms of Neogene Loess-Red Bed Landslides: A Review and Prospects. Earth Science, 51(2): 578-601. doi: 10.3799/dqkx.2025.265

Citation:

Li Kun, Sun Ping, Wang Haojie, Zhang Shuai, Li Ran, Sang Kangyun, 2026. Typical SlopeStructures and Their Sliding Control Mechanisms of Neogene Loess-Red Bed Landslides: A Review and Prospects. Earth Science, 51(2): 578-601. doi: 10.3799/dqkx.2025.265

Citation:

Li Kun, Sun Ping, Wang Haojie, Zhang Shuai, Li Ran, Sang Kangyun, 2026. Typical SlopeStructures and Their Sliding Control Mechanisms of Neogene Loess-Red Bed Landslides: A Review and Prospects. Earth Science, 51(2): 578-601. doi: 10.3799/dqkx.2025.265

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Typical SlopeStructures and Their Sliding Control Mechanisms of Neogene Loess-Red Bed Landslides: A Review and Prospects

doi: 10.3799/dqkx.2025.265

Li Kun^{1, 2, 3
,
,},
Sun Ping^{1, 2
,
,
,},
Wang Haojie^{1, 2},
Zhang Shuai^{1, 2},
Li Ran^{1, 2},
Sang Kangyun^{1, 2}

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
Observation and Research Station of Geological Disaster in Baoji, Shaanxi Province, Ministry of Natural Resources, Baoji 721001, China
3.
Chengdu Center, China Geological Survey, Chengdu 610218, China

Received Date: 2025-05-11
Publish Date: 2026-02-25

Abstract

Abstract

Neogene loess-red bed landslides are the most typical and concerning disaster in the Loess Plateau. Their failure mechanisms have become a frontier scientific challenge in the field of engineering geology that requires urgent breakthroughs. This study adopts landslide-controlling slope structures as the analytical framework to systematically examine geological structure types and occurrence characteristics of loess-red bed slopes from two perspectives: stratigraphic structures and geological interfaces. It elaborates on the triple control effects of structural planes in landslide formation-boundary confinement, hydraulic channelization, and mechanical weakening and summarizes landslide types and corresponding failure modes based on structure control effects.The evolutionary mechanisms of landslides under the influence of slope-control structures are comprehensively analyzed. Based on the current state of research, four critical issues are identified: ①How to quantifythe spatiotemporal coupling effects between geodynamic forces and the evolution of structural planes?②How slope structures induce slope instability via cross-scale energy transfer and damage accumulation?③At what critical state of key physical-mechanical parameters do controlling structures trigger slope failures?④How to develop multi-field coupled numerical models integrating structural control mechanisms with landslide kinematic linkages? To address these challenges, this study proposes prioritized research directions, which include dynamic evolution processes and governing mechanisms of sliding-control structures under multi-field coupling effects, mechanical deterioration mechanisms of red bed structure planes driven by water-rock interactions, critical state thresholds and diagnostic criteria for structure control in loess-red beds landslides, kinematic evolution modeling of loess-red bed landslides incorporating structure control effects.
- Loess Plateau,
- Neogene loess-red beds,
- landslide,
- structural plane,
- sliding-control structure

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References(193)

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Typical SlopeStructures and Their Sliding Control Mechanisms of Neogene Loess-Red Bed Landslides: A Review and Prospects

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