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 987654321/103483
English  |  正體中文  |  简体中文  |  Items with full text/Total items : 94201/94201 (100%)
Visitors : 81584982      Online Users : 2450
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/987654321/103483


    Title: Crustal thickening and extension induced by the Great Sumatra–Andaman earthquake of 26 December 2004: revealed by the seismic moment tensor element Mrr
    Authors: 林靜怡;Lin, J.-Y.;Lo, C.-L.;Wu, W.-N.;Sibuet, J.-C.;Hsu, S.-K.;Wen, Y.-Y.
    Contributors: 地球科學學院地球科學學系
    Keywords: Continental margins;Earth and Environmental Science;Earth Sciences;Earthquakes;Geology;Geophysics/Geodesy;Oceanography;Offshore Engineering;Original Research Paper;Seismic activity;Seismology
    Date: 2014-01-01
    Issue Date: 2026-04-23 11:31:23 (UTC+8)
    Publisher: Springer Netherlands;Dordrecht: Springer Netherlands
    Abstract: 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: Springer Nature Link 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
    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