2011
DOI: 10.1016/j.enggeo.2011.03.013
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Landslides induced by the Wenchuan earthquake and the subsequent strong rainfall event: A case study in the Beichuan area of China

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Cited by 208 publications
(108 citation statements)
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“…The source magnitude controls the area affected by landslides [1] relating the ground motion decay with distance to the epicenter or to the fault plane (e.g., [3]). However this generic law is affected by different factors: (1) a significant over-abundance of landslides in the hanging walls of ruptured thrust faults relative to the footwalls rate are reported (e.g., [4,5]), showing the effect of the dynamics of the fault rupture on the landslide distribution; (2) the greater erosion rate due to precipitations observed after the earthquake [8,10] shows that earthquakes are found to interact non-linearly with precipitations; (3) the site effect, or amplification of the seismic waves due to shear-wave velocity contrast between the landslide material and the stable material [11,12] or topographical particularities like ridges [9]. This topographic control on co-seismic landslides has also been pointed out through different parameters: convexity [7], slopes, proximity from ridges and crests [6,9].…”
Section: Introductionmentioning
confidence: 99%
“…The source magnitude controls the area affected by landslides [1] relating the ground motion decay with distance to the epicenter or to the fault plane (e.g., [3]). However this generic law is affected by different factors: (1) a significant over-abundance of landslides in the hanging walls of ruptured thrust faults relative to the footwalls rate are reported (e.g., [4,5]), showing the effect of the dynamics of the fault rupture on the landslide distribution; (2) the greater erosion rate due to precipitations observed after the earthquake [8,10] shows that earthquakes are found to interact non-linearly with precipitations; (3) the site effect, or amplification of the seismic waves due to shear-wave velocity contrast between the landslide material and the stable material [11,12] or topographical particularities like ridges [9]. This topographic control on co-seismic landslides has also been pointed out through different parameters: convexity [7], slopes, proximity from ridges and crests [6,9].…”
Section: Introductionmentioning
confidence: 99%
“…Data from the forestry department of Sichuan Province, China showed that forest land deteriorated by 32.867 × 10 4 ha, with a direct economic loss of the forest system estimated to be as much as 23 billion RMB [6]. Most of the damaged vegetation was distributed along both sides of the river, causing erosion and formation of debris flows [2,7]. Currently, the areas of damaged vegetation are at various stages of recovery, and some fully recovered within only a few years of the earthquake.…”
Section: Introductionmentioning
confidence: 99%
“…Several studies have been conducted worldwide during the last few decades that report on ground failures triggered by earthquakes (Bommer and Rodriguez, 2002;Sepulveda et al, 2005;Porfido et al, 2007;Tosatti et al, 2008;Gorum et al, 2011;Tang et al, 2011;Alfaro et al, 2012; among many others) and that forecast, using predictive models, the distribution scenarios of earthquake-induced ground effects (Sassa et al, 1996;Jibson et al, 2000;Prestininzi and Romeo, 2000;Romeo, 2000;Jibson, 2007;Hsieh and Lee, 2011;among others). These studies provide inventory maps of the effects that have occurred or susceptibility maps of expected ground failures.…”
Section: Introductionmentioning
confidence: 99%