Crustal and upper mantle S-wave velocity structures across the Taiwan Strait from ambient seismic noise and teleseismic Rayleigh wave analyses

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• 作者：Yu-Chih Huang ; Huajian Yao ; Francis T. Wu ; Wen-Tzong Liang ; Bor-Shouh Huang ; Cheng-Horng Lin ; Kuo-Liang Wen
• 关键词：S-wave velocity structure ; Crust and upper mantle ; Taiwan Strait ; Ambient seismic noise ; Surface wave two-station method
• 刊名：Journal of Asian Earth Sciences
• 出版年：25 February, 2014
• 年：2014
• 卷：81
• 期：Complete
• 页码：38-52
• 全文大小：5099 K

文摘

Although orogeny tapers off in western Taiwan large and small earthquakes do occur in the Taiwan Strait, a region largely untouched in previous studies owing mostly to logistical reasons. But the overall crustal structure of this region is of particular interest as it may provide a hint of the proto-Taiwan before the orogeny.

By combining time domain empirical Green鈥檚 function (TDEGF) from ambient seismic noise using station-pairs and traditional surface wave two-station method (TS) we are able to construct Rayleigh wave phase velocity dispersion curves between 5 and 120 s. Using Broadband Array in Taiwan for Seismology (BATS) stations in Taiwan and in and across the Strait we are able to derive average 1-D Vs structures in different parts of this region. The results show significant shear velocity differences in the upper 15 km crust as expected. In general, the highest Vs in the upper crust observed in the coastal area of Mainland China and the lowest Vs appears along the southwest offshore of the Taiwan Island; they differ by about 0.6-1.1 km/s. For different parts of the Strait, the upper crust Vs structures are lower in the middle by about 0.1-0.2 km/s relative to those in the northern and southern parts. The upper mantle Vs structure (Moho - 150 km) beneath the Taiwan Strait is about 0.1-0.3 km/s lower than the AK135 model. The overall crustal thickness is approximately 30 km, much thinner and less variable than under the Taiwan Island. The inversion of seismic velocity structures using shorter period band dispersion data in the sea areas with water depth deeper than 1000 m should take water layer into consideration except for the continental shelves.