English  |  正體中文  |  简体中文  |  全文筆數/總筆數 : 94201/94201 (100%)
造訪人次 : 81564164      線上人數 : 3960
RC Version 7.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
搜尋範圍 查詢小技巧:
  • 您可在西文檢索詞彙前後加上"雙引號",以獲取較精準的檢索結果
  • 若欲以作者姓名搜尋,建議至進階搜尋限定作者欄位,可獲得較完整資料
  • 進階搜尋


    請使用永久網址來引用或連結此文件: https://ir.lib.ncu.edu.tw/handle/987654321/103215


    題名: 1909 Taipei earthquake ground motion simulation
    作者: 馬國鳳;Liao, Yi-Wun;Yen, Yin-Tung;Lee, Shiann-Jong;Ma, Kuo-Fong
    貢獻者: 地球科學學院地球科學學系
    關鍵詞: 1909 Taipei earthquake;Components;Computer simulation;Earthquake damage;Earthquakes;Empirical Green’s function method;Geological hazards;Ground motion;Hazard assessment;Hybrid simulation;Metropolitan areas;Motion simulation;P-waves;Relocation;Seismic activity;Seismic hazard;Shaking;Simulation;Spectral element method;Stresses;Subduction;Subduction (geology);Subduction zones;Wave motion;Waves
    日期: 2016-06-01
    上傳時間: 2026-04-23 11:25:53 (UTC+8)
    出版者: Chinese Geoscience Union;Taiwan: Springer Nature B.V
    摘要: 摘要: The 1909 Taipei earthquake (M 7.3) occurred beneath the Taipei metropolitan area (TMA) causing substantial damage according to the historical literature. According to the hypocenter relocation and tectonic implications provided in a previous study, we simulated ground motions within the TMA using a hybrid simulation method involving the spectral-element method (SEM) and the empirical Green’s function method (EGFM). We used the SEM for simulating low-frequency components and the EGFM for simulating high-frequency components. These high and low frequency components were subsequently combined. For the EGFM we used the records from a recent ML 4.9 earthquake (11 October 2013, depth = 143.8 km) in the Taipei area as the empirical Green’s function. According to the historical literature, the observed PGA (peak ground acceleration) values are 59.2 and 67.0 gal at ancient stations TAP and KEE, with periods of 1.21 and 1.34 s, respectively. By comparing the simulated PGA values at modern stations TAPB and WFSB to the historical documented ones for 12 different models, our result suggests that the 1909 Taipei earthquake was an event with a magnitude of about Mw 7.3 and stress drop of approximately 30 bars, or a smaller equivalent magnitude between Mw 6.8 - 7.3 but with much higher average stress drop of more than 100 bars. For a deep event beneath TMA a larger vertical P-wave motion and longer period shaking wave, as addressed in the historical literature, might be expected with prolonged shaking as found in the simulation. A seismic hazard assessment is necessary for metropolitan Taipei to better understand the long period shaking from deep subduction zone intra plate events. Key points • Ground motions with full spectra for the 1909 Taipei earthquake were simulated • Possible magnitude and stress drop of the 1909 Taipei earthquake were assessed • Concern on intra-plate event beneath Taipei
    出版者: Taiwan: Springer Nature B.V
    出版日期: 2016-06-01
    出處: TAO : Terrestrial, atmospheric, and oceanic sciences, 2016-06, Vol.27 (3), p.415-430
    資源來源: Agricultural & Environmental Science Collection
    版權: 2016. This work is licensed under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.
    識別號: ISSN: 1017-0839
    識別號: ISSN: 2223-8964
    識別號: ISSN: 2311-7680
    識別號: EISSN: 2311-7680
    識別號: EISSN: 1017-0839
    識別號: DOI: 10.3319/TAO.2016.03.02.01(TEM)
    顯示於類別:[地球科學學系] 期刊論文

    文件中的檔案:

    檔案 描述 大小格式瀏覽次數
    index.html0KbHTML17檢視/開啟


    在NCUIR中所有的資料項目都受到原著作權保護.

    社群 sharing

    ::: Copyright National Central University. | 國立中央大學圖書館版權所有 | 收藏本站 | 設為首頁 | 最佳瀏覽畫面: 1024*768 | 建站日期:8-24-2009 :::
    DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - 隱私權政策聲明