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Paleoseismology of the Chelungpu Fault during the past 1900 years

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Fig. 1. The Chi-Chi earthquake causes a surface rupture in front of the Western Foothills, which is subdivided into the Chushan, Tsaotun, Shihkang, andCholan segments along the Shihkang-Chelungpu-Tajienshan Fault (Chen et al., 2001e)
Fig. 2. Location map of the trenches excavatedacross a terrace scarp along the Chelungpu Fault.
Fig. 3. (a, b) Five types of deposits, the 1999 ruptures, and three paleo-coseismic thrusts of F1, F2, and F3 are observed in the trench
Fig. 4. The fault scarp offsets the river terrace. The height of the fault scarp is 2.1 m in trench B
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