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    Please use this identifier to cite or link to this item: https://tkuir.lib.tku.edu.tw/dspace/handle/987654321/94807

    Title: 斷層引致地震之一種原因探討:滯動現象
    Other Titles: A Study on the Cause of Earthquake Induced by Fault Slip: Stick Slip
    Authors: 楊長義
    Contributors: 淡江大學土木工程學系
    Keywords: 地震;斷層面;斷層碎屑;摩擦;節瘤;脆性斷裂;滯動;節理;岩體模擬;Earthquake;Fault Plane;Fault Debris;Friction;Asperity;Brittle Fracture;Stick Slip;Joint;Rock Body Simulation
    Date: 1996-04
    Issue Date: 2014-02-08 19:34:18 (UTC+8)
    Abstract: 本文由室內節理岩體模擬結果之滯動現象,探討引起此種地震的原因。研究結果發現引起規則滯動或地震的原因可能是斷層間碎屑之相互摩擦行為所控制,而非僅由斷層面靜、動摩擦係數差異引起,尚必須考慮節瘤破碎後對節理面摩擦性質之改變。
    This paper aims at the topic of earthquakes induced by stick-slip friction on faults. It shows that The stick- slip behavior is dominated by the motion of fault debris. To clarify the mechanism of earthquake, the effect on frictional properties of faults by asperity rupture is suggested to be taken into account.
    Relation: 中國地質學會八十五年年會大會手冊及論文摘要=Program with Abstracts 1996 Annual Meeting of Geological Society of China
    Appears in Collections:[土木工程學系暨研究所] 會議論文

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    斷層引致地震之一種原因探討:滯動現象_中文摘要.docx摘要16KbMicrosoft Word249View/Open
    斷層引致地震之一種原因探討:滯動現象_英文摘要.docx摘要16KbMicrosoft Word149View/Open

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