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 987654321/103489
English  |  正體中文  |  简体中文  |  全文笔数/总笔数 : 94201/94201 (100%)
造访人次 : 81793323      在线人数 : 1611
RC Version 7.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
搜寻范围 查询小技巧:
  • 您可在西文检索词汇前后加上"双引号",以获取较精准的检索结果
  • 若欲以作者姓名搜寻,建议至进阶搜寻限定作者字段,可获得较完整数据
  • 进阶搜寻


    jsp.display-item.identifier=請使用永久網址來引用或連結此文件: https://ir.lib.ncu.edu.tw/handle/987654321/103489


    题名: Crustal thickening and extension induced by the Great Sumatra–Andaman earthquake of 26 December 2004: revealed by the seismic moment tensor element Mrr
    作者: 羅仲良;Lin, J.-Y.;Lo, C.-L.;Wu, W.-N.;Sibuet, J.-C.;Hsu, S.-K.;Wen, Y.-Y.
    贡献者: 地球科學學院地球科學學系
    关键词: Continental margins;Earth and Environmental Science;Earth Sciences;Earthquakes;Geology;Geophysics/Geodesy;Oceanography;Offshore Engineering;Original Research Paper;Seismic activity;Seismology
    日期: 2014-01-01
    上传时间: 2026-04-23 11:31:29 (UTC+8)
    出版者: Springer Netherlands;Dordrecht: Springer Netherlands
    摘要: 摘要: In a complex geological environment, it is generally difficult to assimilate a complete understanding of the main stress regime without being distracted by various fault configurations. In this study, we examine the changes in radial seismic moment (Mrr) of earthquakes that occurred in the Sumatra area. This approach allows for simplification of the various focal mechanism solutions by compressive and extensional slip vectors. The results show that the epicenter of the 2004 mainshock is located near the area where the accumulated Mrr was highest during the inter-seismic period. Simultaneously, a pattern of negative accumulated Mrr observed at depths between 40 and 100 km suggests a down-dip extension mechanism caused by the slab pull effect, which could be strengthened by the locking procedure in shallow portions of the slab. Moreover, the right-lateral strike-slip Sumatra Fault and the left-lateral oceanic fracture zones exhibited positive and negative accumulated Mrr prior to and immediately after the 2004 mainshock. This transform of Mrr indicates stress release associated with the unlocking of the asperities during the earthquake. Therefore, the distinctly different Mrr patterns for the inter- and post-seismic period suggest that the occurrence of a substantial earthquake could change the intraplate stress state.
    其他題名: Mar Geophys Res
    出版者: Dordrecht: Springer Netherlands
    出版日期: 2015-09-01
    出處: Marine geophysical researches, 2015-09, Vol.36 (2-3), p.187-195
    資源來源: SpringerLink Journals
    版權: Springer Science+Business Media Dordrecht 2014
    版權: Springer Science+Business Media Dordrecht 2015
    識別號: ISSN: 0025-3235
    識別號: EISSN: 1573-0581
    識別號: DOI: 10.1007/s11001-014-9240-x
    显示于类别:[地球科學學系] 期刊論文

    文件中的档案:

    档案 描述 大小格式浏览次数
    index.html0KbHTML20检视/开启


    在NCUIR中所有的数据项都受到原著作权保护.

    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