中大機構典藏-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 987654321/50514
English  |  正體中文  |  简体中文  |  Items with full text/Total items : 80990/80990 (100%)
Visitors : 40249729      Online Users : 313
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.lib.ncu.edu.tw/handle/987654321/50514


    Title: Analysis of Rupture Directivity for the 2004 Sumatra Earthquake from the Rayleigh-Wave Phase Velocity
    Authors: Chang,JP;Hwang,RD;Wang,CY;Yu,GK;Chang,WY;Lin,TW
    Contributors: 地球物理研究所
    Keywords: ANDAMAN EARTHQUAKE;SCALING RELATIONS;ENERGY;SPEED
    Date: 2010
    Issue Date: 2012-03-27 17:35:52 (UTC+8)
    Publisher: 國立中央大學
    Abstract: The rupture directivity for the 2004 Sumatra earthquake is analyzed by examining differences between the phase-delay times of Rayleigh-waves (in the 140 - 160 sec period range) arising from the main shock and reference earthquakes. A long source-process time (similar to 463.0 sec) and large rupture length (similar to 1164.0 km) are derived from this analysis of rupture directivity. The source-process time for this earthquake is larger than for either the 1960 Chile or 1964 Alaska earthquakes. This might be due to the length of the rupture that occurred during earthquake faulting. The estimated rise time for the 2004 Sumatra earthquake, 92.0 sec, is approximately 20% of the whole source duration and also larger than those for the 1960 Chile and 1964 Alaska earthquakes. This likely reflects a fundamental difference between the frictional properties of these earthquakes. When the rise time is taken into account, an estimated rupture velocity of approximately 3.1 km sec(-1) is obtained. This value is higher than that found in previous studies carried out on the basis of hydroacoustic data and regional seismic networks. In this study, we obtain additional evidence from analysis of the surface-wave phase-delay time which confirms the basic features of the rupturing of the 2004 Sumatra earthquake. The results can also provide some constraints for the study of source rupturing for this earthquake.
    Relation: TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES
    Appears in Collections:[Graduate Institute of Geophysics] journal & Dissertation

    Files in This Item:

    File Description SizeFormat
    index.html0KbHTML658View/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