| 英文摘要 |
The underground geometries the active faults are very complex in the western foothills (WF) of central Taiwan. In previous studies, it has been difficult to identify the correlations between the seismogenic structures and active faults in the area using geophysical explorations or theoretical seismological modes. Therefore, if a three-dimensional geometric model of the décollement in the WF could be constructed, it would benefit morphological studies of this region. |
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