保持類似的垂直變動趨勢，另比對陳國華等(Chen et al., 2011)施測水準資料，
推測成功沿海自 2003 年地震事件後，於 2007-2010 間抬升行為轉為趨緩，抬
岩與舞鶴礫岩出露高角度斷層則展現不同的地表變形特徵，除應力應變的差 異，斷層上、下盤岩性也是影響地表變形主因，縱谷南、北兩側地表變形性 型態有快速大幅度的轉變，推測可能與其地下地層分布或構造環境有關。
(6) 根據地震-地表變形剖面顯示，池上斷層地下地震數量愈多、震源深度分布愈 淺，近斷層地表變形就會變得更劇烈，瑞穗斷層具有撓曲式地表變形，並地 下無明顯無震特性，推測為瑞穗斷層淺部鎖定造成的變形特徵。
90
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