2017
DOI: 10.1007/s10346-017-0845-4
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Understanding the triggering mechanism and possible kinematic evolution of a reactivated landslide in the Three Gorges Reservoir

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Cited by 95 publications
(22 citation statements)
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“…The landslide boundary was determined by the landslide deformation and adjacent terrain (Gu et al, 2017;Pánek et al, 2008). The ancient landslide is generally like W in shape, with slope of about 21°.…”
Section: Characteristics Of Ancient Landslidementioning
confidence: 99%
“…The landslide boundary was determined by the landslide deformation and adjacent terrain (Gu et al, 2017;Pánek et al, 2008). The ancient landslide is generally like W in shape, with slope of about 21°.…”
Section: Characteristics Of Ancient Landslidementioning
confidence: 99%
“…In recent literature, some authors have applied the correlation and sensitivity analysis methods to explain the triggering mechanism of landslides [28][29][30], while others have proposed kinematic models on the basis of movement identification to predict landslide risks [31,32]. However, few studies use integrated in situ data to uncover the time-variable patterns of slow-moving colluvial landslides in the TGR area.…”
Section: Introductionmentioning
confidence: 99%
“…The pile-landslide interaction highlights landslide evolution, which is controlled by internal and external factors and involves multi-field interaction parameters, such as stress, displacement, and temperature [6,7]. The deformation characteristics are different at different evolution stages [8][9][10]. Therefore, it is essential to identify the evolutionary stage to understand the deformation and failure process of a pile-reinforced landslide.…”
Section: Introductionmentioning
confidence: 99%