English  |  正體中文  |  简体中文  |  Items with full text/Total items : 17776/20117 (88%)
Visitors : 12204421      Online Users : 325
RC Version 7.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
Scope Tips:
  • please add "double quotation mark" for query phrases to get precise results
  • please goto advance search for comprehansive author search
  • Adv. Search
    HomeLoginUploadHelpAboutAdminister Goto mobile version
    Please use this identifier to cite or link to this item: http://ir.cnu.edu.tw/handle/310902800/29616


    標題: Monet Wavelet Analysis of M-L >= 3 Earthquakes in the Taipei Metropolitan Area
    作者: Chen, Kou-Cheng
    Wang, Jeen-Hwa
    Kim, Kwang-Hee
    Huang, Win-Gee
    Chang, Kao-Hao
    Wang, Jeng-Cheng
    Leu, Pei-Ling
    貢獻者: 應用空間資訊系
    關鍵字: Seismicity
    Number of monthly events
    Morlet wavelet analysis
    Wavelet power spectrum
    Global power spectrum
    Dominant period
    日期: 2015-04
    上傳時間: 2016-04-19 19:02:09 (UTC+8)
    出版者: Chinese Geoscience Union
    摘要: M-L >= 3 earthquakes (M-L = local magnitude) that occurred in the Taipei Metropolitan Area (TMA) from 1973 - 2013 are selected to study the dominant seismicity period of this area. The epicentral distribution and temporal sequences of earthquake magnitudes are simply described. These earthquakes can be divided into two groups: one for events shallower than 40 km and one for events deeper than 60 km. Shallow earthquakes are located mainly in the 0 - 10 km depth range north of 25.1 degrees N, and down to 35 km for those south of 25.1 degrees N. Deep events are located in the subduction zone, with a dip angle of about 70 degrees. The Morlet wavelet technique is applied to analyze the dominant periods of temporal variations in numbers of monthly earthquakes in the shallow and deep ranges for three magnitude ranges, i.e., M-L >= 3, 4, and 5. The results show that for shallow earthquakes the dominant periods are 15.4, 30.8, 66.1, and 132.2 months when M-L >= 3 and 30.8 months when M-L >= 4; while for deep earthquakes, the dominant periods are 16.5 and 141.7 months when M-L >= 3 and 141.7 months when M-L >= 4. The dominant period cannot be obtained for both shallow and deep M-L >= 5 earthquakes.
    關聯: Terrestrial Atmospheric And Oceanic Sciences, v.26 n.2, pp.83-94
    Appears in Collections:[應用空間資訊系(所)] 期刊論文

    Files in This Item:

    File Description SizeFormat
    29616.pdf6830KbAdobe PDF484View/Open
    index.html0KbHTML516View/Open


    All items in CNU IR are protected by copyright, with all rights reserved.


    DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - Feedback