A Seismic Investigation of the Chelungpu Fault

• Main Authors: Hsuan-Chung Chen, 陳璿臣
• Other Authors: Chien-Ying Wang
• Format: Others
• Language: zh-TW
• Published: 2002
• Online Access: http://ndltd.ncl.edu.tw/handle/49850975404330780133

碩士 === 國立中央大學 === 地球物理研究所 === 90 === A Seismic Investigation of the Chelungpu Fault Hsuan-Chung Chen ABSTRACT The 1999 Chi-Chi earthquake (Mw=7.6) occurred in center Taiwan marks the island’s largest inland seismic event in the twentieth century. It triggered an existing active fault, the Chelungpu fault. The fault was a reverse type dipping 20-50 degrees to the east and extending north-south about 90 km . The observed vertical displacements increased from the south (0.6m) to the north (7m), and the maximum horizontal displacement was 9.6m. Most of fault segments were characterized by pure thrust with minor lateral slip, but the left-lateral component of slip increased in the northern part near Shihkang. The Chelungpu fault developed along the topographic scarp running mosty in the north-south direction. However, it bended toward the northeast near Fengyuan and Shihkang, crossed the Ta-anhsi and the Tachiahsi rivers, finally stopped at the town of Cholan. In geology, the Chelungpu fault was a bed-plane fault sliding along a sedimentary layer, the Chinshui shale. The purpose of this study is to detect the underground structure in the vicinity of the Chelungpu fault by the shallow seismic reflection method. The obtained seismic sections enable us to examine the detailed faulting mechanism along the fault. The following conclusions are obtained: 1)The structures in the study area are surprisingly simple, with layers dipping regularly to the east. They are controlled by the background structural fold systems. 2)The up-dip movement of the Chelungpu fault along the Chinshui shale layer has lifted the structures above it, and at certain weak places the fractures cut through the beds with a 45o angle and thus make a 60o-70o dip, in relation to the surface. These fractures caused the ground to buckle and break. 3)The fault surface within the Chinshui shale has a dipping angle of 20o -50o to the east and 10o to the south. Some up and down undulation of this surface may exist. 4)The abnormal behavior of the fault at the northern tip can be explained as a result of the fault surface shape changes there. The structural variation of layers directed the thin-skinned thrust faulting. 5)The shallow reflection seismic method can be useful to study large-scale structures, if applied along with appropriate geologic theories.