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首页> 外文期刊>Bulletin of the Seismological Society of America >Comment on 'A vertical exposure of the 1999 surface rupture of the Chelungpu Fault at Wufeng, western Taiwan: Structural and paleoseismic implications for an active thrust fault,' by Jian-Cheng Lee, Yue-Gau Chen, Kerry Sieh, Karl Mueller, Wen-Shan Ch
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Comment on 'A vertical exposure of the 1999 surface rupture of the Chelungpu Fault at Wufeng, western Taiwan: Structural and paleoseismic implications for an active thrust fault,' by Jian-Cheng Lee, Yue-Gau Chen, Kerry Sieh, Karl Mueller, Wen-Shan Ch

机译：李建成，陈月高，谢家辉，谢凯，Karl Mueller，Wen发表的评论“台湾西部五峰切龙普断裂1999年表面破裂的垂直暴露：活动逆冲断层的结构和古地震意义” -山Ch

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摘要

Lee et al. (2001) applied the line-length balance method on the deformed soil to calculate the shortening of the surface rupture on Chelungpu Fault at Wufeng, Western Taiwan. Their results showed a shortening of 3.3 m and a total slip of 4 m. We, on the other hand, calculated the slip vector of the surface rupture by restoring the deformed concrete fence and found that the horizontal slip is 1.77 m and the slip direction is 279degrees. We then combined the horizontal slip vector with the vertical slip (2.1 m) to get a net slip of 2.75 m. The shortening we had in hand was 1.76 m, which was only half of Lee et al.'s (2001) data. We thus applied the area-balance method to check whether the data measured by line-balance method are reasonable. [References: 2]
机译：Lee等。 （2001）在变形的土壤上应用线长平衡法来计算台湾西部五峰切隆普断裂的地表破裂缩短。他们的结果显示缩短了3.3 m，总滑移了4 m。另一方面，我们通过恢复变形的混凝土围栏来计算表面破裂的滑移矢量，发现水平滑移为1.77 m，滑移方向为279度。然后，我们将水平滑移矢量与垂直滑移（2.1 m）相结合，得出净滑移为2.75 m。我们手头的缩短量为1.76 m，仅为Lee等人（2001）数据的一半。因此，我们应用了面积平衡法来检查通过线平衡法测得的数据是否合理。 [参考：2]

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