2014
DOI: 10.1007/s11069-014-1038-2
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Statistical analysis of landslides caused by the Mw 6.9 Yushu, China, earthquake of April 14, 2010

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Cited by 74 publications
(21 citation statements)
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“…The distance effect of the seismogenic fault and the different paragraph effects have significant control effects on the landslide. For example, in terms of a distance effect, landslides are mostly distributed along the seismogenic fault [2,38,39]. Regarding the effect of different paragraphs, the ability to trigger landslides is also significantly different due to the different nature of the seismogenic faults and the amount of energy released.…”
Section: Influence Factorsmentioning
confidence: 99%
“…The distance effect of the seismogenic fault and the different paragraph effects have significant control effects on the landslide. For example, in terms of a distance effect, landslides are mostly distributed along the seismogenic fault [2,38,39]. Regarding the effect of different paragraphs, the ability to trigger landslides is also significantly different due to the different nature of the seismogenic faults and the amount of energy released.…”
Section: Influence Factorsmentioning
confidence: 99%
“…Each definition was classified as either frequency-independent or frequency-dependent according to whether the entire accelerogram is employed in the calculation of duration or whether it is first passed through a narrowband fitter. Furthermore, each definition was also classified according to whether the criteria used to distinguish the strong motion portion of the accelerograms are absolute or their relative values applied to the accelerogram [34][35][36][37][38][39][40].…”
Section: Classification Of Duration Definitionsmentioning
confidence: 99%
“…In 2008, about 197,481 slope failures were triggered by Wenchuan earthquake of China (M w 7.9 or M s 8.0) Xu et al 2014c), and the phenomena of seismic liquefaction and subsidence were also observed (Huang and Jiang 2010;Huang et al 2011Huang et al , 2012b. The Yushu, China, earthquake in 2010 (M w 6.9) triggered more than 2,036 coseismic landslides with a total coverage area of 1.194 km 2 (Xu and Xu 2014). The Port-auPrince, Haiti earthquake in 2010 (M w 7.0) induced more than 30,828 slope failures, which distributed in an area larger than 3,000 km 2 , and covered about 15.736 km 2 with an estimated landslide erosion volume about 29,700,000 m 3 (Xu et al 2014a).…”
Section: Introductionmentioning
confidence: 99%