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經濟部中央地質調查所 臺灣活動斷層

認識活動斷層

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池上斷層

池上斷層,為逆移斷層兼具左移分量,約呈北北東走向,由花蓮縣玉里鎮春日里向南南西方向經台東縣池上鄉萬安,再向南延伸至鹿野鄉瑞隆村,長約67公里。

總結與評估

池上斷層除了1951年地震造成的地表破裂外,另外2003年12月10日地震也造成部分地區地表破裂的現象,可能與斷層的活動有關,而斷層有持續的潛變現象。池上斷層在過去800年以來,至少有5次的古地震事件,每次事件斷層垂直位移數十公分,最大位移量約60公分。池上斷層長期的抬升速率超過20公厘/年,水平位移速率約為30公厘/年,推估斷層的活動周期為50-160年。

池上斷層條帶地質圖。A:北幅。(座標系統:TWD67)
池上斷層條帶地質圖。B:南幅。(座標系統:TWD67)

劉彥求、林啟文、鄭力瑋、陳柏村,池上斷層調查。活動斷層精查報告,網路版。http://fault.moeacgs.gov.tw/TaiwanFaults_2009/PageContent.aspx ?type=C&id=36

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