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Resonance effect existence or not for landslides triggered by 2008 Wenchuan earthquake: A reply to the comment by Drs. Xu Chong and Xu Xiwei

机译:2008年汶川地震引发的滑坡是否存在共振效应:对Dr.徐冲徐锡伟

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We are very grateful to receive these remarks about our paper. In our paper, we found that more landslides occurred in the block located between F2 and F3 than that in the hanging wall of the seismogenic fault of F2 (see Figure 6 in our paper) based on a database of 13,085 landslides in a distributed area of 418.85 km2 (the smallest landslide in this inventory covers an area of 306.5 m2), and we thought that this is maybe the result of resonance of the block between F2 and F3 under the combination movement of the seismogenic faults F2 and F3 and then the motion there is amplified. In their discussion, Xu and Xu (2012) point out that there is no resonance effect of the block between F2 and F3 combination movement, or the resonance effect is rather small based on a more detailed database, with landslides of 197,000 and an area of 1160 km~2.
机译:我们非常感谢收到关于我们论文的这些评论。在我们的论文中,根据一个分布于该地区的13,085个滑坡的数据库,我们发现F2和F3之间的区块中发生的滑坡比F2的地震成因断层的悬挂壁中的滑坡要多(参见本文的图6)。 418.85 km2(此清单中最小的滑坡占地306.5 m2),我们认为这可能是在地震发动断层F2和F3组合运动然后运动的情况下F2和F3之间的块体共振的结果。有放大。在他们的讨论中,Xu和Xu(2012)指出,F2和F3组合运动之间的块没有共振效应,或者基于更详细的数据库,该共振效应很小,滑坡为197,000,面积为1160公里〜2。

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