淡江大學機構典藏:Item 987654321/18647
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    Please use this identifier to cite or link to this item: https://tkuir.lib.tku.edu.tw/dspace/handle/987654321/18647


    Title: 新化斷層與左鎮斷層之形成機制
    Other Titles: The fracture mechanism of hsinhua fault and tzuoojenn fault
    Authors: 楊長義;蘇建彰
    Contributors: 淡江大學土木工程學系
    Keywords: 新化斷層;左鎮斷層;破裂機制;觸口斷層;活斷層;剪裂破裂;張裂破裂;Hsinhua Fault;Tzuoojenn Fault;Fracture Mechanism;Chukou Fault;Active Fault;Shear Fracture;Tensile Fracture
    Date: 1996-04-18
    Issue Date: 2009-09-16 18:13:21 (UTC+8)
    Abstract: 本文由破裂力學理論與模擬試驗分析斷層破裂機制結果,再與觸口、左鎮、新化斷層間相互分布關係比較,以探究新化斷層與左鎮斷層之形成機制。結果得知左鎮斷層與新化斷層,分別為觸口斷層受剪力錯動在斷層尖端先後產生之張裂與剪裂破裂面,且新化斷層未來活動度可能較左鎮斷層大。
    This paper focuses the fracture mechanism between Shinhau, Tzuoojenn and Chukou faults based on the fracture mechanics theory and experimental testing. The Hsinhua fault is concluded as a shear fracture and Tzuoojenn fault is a tensile fracture of Chukou fault under shearing. The Hsinhua fault is more active than Tzuoojenn fault.
    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
    ，頁283-287
    Appears in Collections:[Graduate Institute & Department of Civil Engineering] Proceeding

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