Shear-wave velocity model of the Chukuo fault zone, Southwest Taiwan, from cross correlation of seismic ambient noise

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• 作者：Yu-Lien Yeh ; Strong Wen ; Kung-Jer Lee ; Chau-Huei Chen
• 关键词：P-wave travel time ; Seismic ambient noise ; Green&rsquo ; s function ; Rayleigh wave ; Shear-wave velocity structure ; Chukuo fault
• 刊名：Journal of Asian Earth Sciences
• 出版年：2013
• 出版时间：5 October, 2013
• 年：2013
• 卷：75
• 期：Complete
• 页码：174-182
• 全文大小：2847 K

文摘

The Chia-Nan (Chiayi-Tainan) area is in the southwestern Taiwan, and is located at the active deformation front of the collision of the Eurasian continental plate and the Philippine Sea plate, which causes complex folds as well as thrust fault systems in the area. The Chukuo fault zone is a boundary between the Western Foothill and the Western Coastal Plain in the Chia-Nan area. The nature of the crustal structure beneath the fault zone, especially the eastern part of the fault zone with mountain topography, has not been well known in detailed due to lack of drilling data as well as its limitation in using other geophysical methods, such as active source survey. In this study, we deployed an array with 11 broadband seismic stations to monitor the seismicity of the Chukuo fault zone. The array has recorded more than 1000 microearthquakes around this area. It provides an opportunity to use P- and S-wave travel time data to investigate the both the crustal P- and S-velocity in the fault zone, however due to the nature of the earthquake distribution, the ray density is relatively low at depth between 0 and 7 km. In addition, the uncertainty of S-wave reading for small earthquake also a limit in building precise S-velocity profile, Thus, we take the advantages of using cross-correlation of seismic ambient noise to investigate crustal S-velocity profile in the Chukuo fault area, especially in the mountain area where crustal faulting is a dominated phenomenon. The results indicate that S-wave velocity in the uppermost crust in the Chukuo fault zone is shown to be slower than previous studies. A low velocity layer exists at depth between 1 and 2 km in the east of the Chukuo Fault. The low S-velocity is related to a highly fractured upper crust due to intensive deformation caused by the orogenic process.