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    jsp.display-item.identifier=請使用永久網址來引用或連結此文件: https://irlib.pccu.edu.tw/handle/987654321/30755


    题名: S-wave velocity structures of the Taipei Basin, Taiwan, using microtremor array measurements
    作者: Huang, Huey-Chu
    Wu, Cheng-Feng
    Lee, Feng-Mei
    Hwang, Ruey-Der
    贡献者: Dept Geol
    关键词: Taipei Basin
    Microtremor array measurement
    Frequency-wavenumber (F-K) spectrum method
    Surface wave inversion technique
    日期: 2015-04
    上传时间: 2015-10-30 13:43:28 (UTC+8)
    摘要: The S-wave velocity structures of the Taipei Basin in Taiwan are investigated using the array records of microtremors at 15 sites. Dispersion curves at these sites are calculated using the frequency-wavenumber (F-K) spectrum method. The S-wave velocity structures in the Taipei Basin are then estimated by employing surface wave inversion technique. Harder strata sites have higher phase velocities than softer sites. If the S-wave velocity of the Tertiary Basement is assumed to be 1000 m/s, then the Quaternary alluvial thicknesses in the Taipei Basin are between about 100 m and 650 m. The thickness of the alluvium gradually increases from the southeast to the northwest. The inversion results are also in good agreement with well-logging data and seismic reflection studies of the Taipei Basin. The study concludes that microtremor array measurement is a useful tool for estimating S-wave velocity structure. (C) 2015 Elsevier Ltd. All rights reserved.
    關聯: JOURNAL OF ASIAN EARTH SCIENCES 卷: 101 頁碼: 1-13
    显示于类别:[地質系] 期刊論文

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