中大學術數位典藏-NCU Institutional Repository-提供博碩士論文、考古題、期刊論文、研究計畫等下載:Item 987654321/103223
English  |  正體中文  |  简体中文  |  Items with full text/Total items : 94201/94201 (100%)
Visitors : 81574466      Online Users : 2977
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: https://ir.lib.ncu.edu.tw/handle/987654321/103223


    Title: A deep outer-rise reverse-fault earthquake immediately triggered a shallow normal-fault earthquake: The 7 December 2012 off-Sanriku earthquake (M W 7.3)
    Authors: 佐竹健治;Harada, Tomoya;Murotani, Satoko;Satake, Kenji
    Contributors: 地球科學學院地球科學學系
    Keywords: Earth sciences;Earth, ocean, space;earthquake triggering;Earthquakes;Exact sciences and technology;Fault lines;finite-fault slip model;General Earth and Planetary Sciences;Geophysics;outer-rise earthquake;Plate tectonics;Seismic activity;Seismology;static change in the ΔCFF;teleseismic body-wave analysis;the 2011 Tohoku earthquake;Wave analysis
    Date: 2013-08-28
    Issue Date: 2026-04-23 11:26:04 (UTC+8)
    Publisher: Wiley-Blackwell;Washington, DC: Blackwell Publishing Ltd
    Abstract: 摘要: AbstractTeleseismic body wave analysis revealed that the 7 December 2012 off‐Sanriku earthquake (MW 7.3) at the outer rise of Japan Trench consisted of two successive subevents. The first subevent with reverse‐fault mechanism (Event 1, MW 7.1) at 56 km depth was followed by, approximately 20 s later, the second subevent with normal‐fault mechanism (Event 2, MW 7.2) at 6 km depth. Finite‐fault slip models show that the slip of Event 1 was concentrated around the initial rupture point with the maximum of 2.7 m and that Event 2 had two asperities with the maximum of 4.5 m at both sides of the initial rupture point. The static Coulomb Failure Function analyses suggested that Event 1 triggered Event 2 and that both subevents were promoted by the 2011 Tohoku earthquake (MW 9.1).
    其他題名: Geophys. Res. Lett
    出版者: Washington, DC: Blackwell Publishing Ltd
    出版日期: 2013-08-28
    出處: Geophysical Research Letters, 2013-08, Vol.40 (16), p.4214-4219
    資源來源: Wiley Online Library - AutoHoldings Journals
    版權: 2013. American Geophysical Union. All Rights Reserved.
    版權: 2014 INIST-CNRS
    識別號: ISSN: 0094-8276
    識別號: ISSN: 1944-8007
    識別號: EISSN: 1944-8007
    識別號: DOI: 10.1002/grl.50808
    識別號: CODEN: GPRLAJ
    Appears in Collections:[Department of Earth Sciences ] journal & Dissertation

    Files in This Item:

    File Description SizeFormat
    index.html0KbHTML14View/Open


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

    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