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 987654321/103586
English  |  正體中文  |  简体中文  |  Items with full text/Total items : 94201/94201 (100%)
Visitors : 81558072      Online Users : 3295
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/987654321/103586


    Title: Evidence for non-self-similarity of microearthquakes recorded at a Taiwan borehole seismometer array
    Authors: 林彥宇;Lin, Yen-Yu;Ma, Kuo-Fong;Kanamori, Hiroo;Song, Teh-Ru Alex;Lapusta, Nadia;Tsai, Victor C.
    Contributors: 地球科學學院地球科學學系
    Date: 2016-08-01
    Issue Date: 2026-04-23 11:33:22 (UTC+8)
    Publisher: Oxford University Press;Oxford University Press (OUP)
    Abstract: 摘要: We investigate the relationship between seismic moment M 0 and source duration tw of microearthquakes by using high-quality seismic data recorded with a vertical borehole array installed in central Taiwan. We apply a waveform cross-correlation method to the three-component records and identify several event clusters with high waveform similarity, with event magnitudes ranging from 0.3 to 2.0. Three clusters—Clusters A, B and C—contain 11, 8 and 6 events with similar waveforms, respectively. To determine how M 0 scales with tw , we remove path effects by using a path-averaged Q. The results indicate a nearly constant tw for events within each cluster, regardless of M 0, with mean values of tw being 0.058, 0.056 and 0.034 s for Clusters A, B and C, respectively. Constant tw , independent of M 0, violates the commonly used scaling relation ${t_w} \propto M_0^{1/3}$ . This constant duration may arise either because all events in a cluster are hosted on the same isolated seismogenic patch, or because the events are driven by external factors of constant duration, such as fluid injections into the fault zone. It may also be related to the earthquake nucleation size.
    出版者: Oxford University Press (OUP)
    出版日期: 2016-08-01
    出處: Geophysical Journal International, 2016-08, Vol.206 (2), p.757-773
    版權: The Authors 2016. Published by Oxford University Press on behalf of The Royal Astronomical Society. 2016
    識別號: ISSN: 0956-540X
    識別號: ISSN: 1365-246X
    識別號: EISSN: 1365-246X
    識別號: DOI: 10.1093/gji/ggw172
    Appears in Collections:[Department of Earth Sciences ] journal & Dissertation

    Files in This Item:

    File Description SizeFormat
    index.html0KbHTML17View/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