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 987654321/103611
English  |  正體中文  |  简体中文  |  Items with full text/Total items : 94201/94201 (100%)
Visitors : 81685955      Online Users : 3905
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/987654321/103611


    Title: Fault mirrors in seismically active fault zones: A fossil of small earthquakes at shallow depths
    Authors: 郭力維;Kuo, Li‐Wei;Song, Sheng‐Rong;Suppe, John;Yeh, En‐Chao
    Contributors: 地球科學學院地球科學學系
    Keywords: Active mirrors;Basins;Boreholes;Deformation;Earthquake damage;Earthquakes;Fault lines;fault mirror;Fault zones;Faults;flash heating;fossil earthquakes;Fossils;Gels;Geological faults;Geology;Geosciences, Multidisciplinary;Hanging walls;Heating;Indicators;melt;Melts;Mirrors;Physical Sciences;Science & Technology;Seismic activity;Silica;Silica gel;Slip
    Date: 2016-03-16
    Issue Date: 2026-04-23 11:33:50 (UTC+8)
    Publisher: Wiley-Blackwell;WASHINGTON: American Geophysical Union (AGU)
    Abstract: 摘要: AbstractFault mirrors (FMs) are naturally polished and glossy fault slip surfaces that can record seismic deformation at shallow depths. They are important for investigating the processes controlling dynamic fault slip. We characterize FMs in borehole samples from the hanging wall damage zone of the active Hsiaotungshi reverse fault, Taiwan. Here we report the first documented occurrence of the combination of silica gel and melt patches coating FMs, with the silica gel resembling those observed on experimentally formed FMs that were cataclastically generated. In addition, the melt patches, which are unambiguous indicators of coseismic slip, suggest that the natural FMs were produced at seismic rates, presumably resulting from flash heating at asperities on the slip surfaces. Since flash heating is efficient at small slip, we propose that these natural FMs represent fossils of small earthquakes, formed in either coseismic faulting and folding or aftershock deformation in the active Taiwan fold‐and‐thrust belt.
    出版者: WASHINGTON: American Geophysical Union (AGU)
    出版日期: 2016-03
    出處: Geophysical Research Letters, 2016-03, Vol.43 (5), p.1950-1959
    資源來源: Wiley Online Library - AutoHoldings Journals;Web of Science Primary (SCIE, SSCI & AHCI);Scopus
    識別號: ISSN: 0094-8276
    識別號: ISSN: 1944-8007
    識別號: EISSN: 1944-8007
    識別號: DOI: 10.1002/2015gl066882
    Appears in Collections:[Department of Earth Sciences ] journal & Dissertation

    Files in This Item:

    File Description SizeFormat
    index.html0KbHTML16View/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