旗山斷層與車瓜林斷層位在國道三號中寮隧道與田寮三號高架橋一帶，長年已經造成此工程嚴重的抬升擠壓問題，中寮隧道北端隧道口受旗山斷層影響，除了導致隧道隆起，也造成隧道淨高不足；田寮高架橋橋梁因車瓜林斷層擠壓損壞，可能會有落橋之危險，且地表變形還持續進行中，此使得長期改善工程更加艱困。本研究目的為了解當地的地質條件，利用岩石物理性質與礦物組成研究造成岩石破壞的機制，且加以探討造成斷層潛移作用加速的原因。透過野外採樣與岩礦組構分析，觀察岩體中裂縫發展趨勢與相對應力分析以了解研究區域整體變形模式。
當斷層活動時，若沒有產生應力下降的現象，而是在該特定應力下，滑動速率大致保持一定者，稱之為潛移作用，潛移作用為非震性滑動，在旗山斷層與車瓜林斷層中因潛移運動影響，岩石礦物中的變形機制主要是壓碎和摩擦滑移作用與錯動潛移作用；同時也觀察到少數黃鐵礦產生晶粒間滑移與方解石形成的機械雙晶。水(H2O)的相關結果反映：旗山斷層屬於富水環境，有益於裂縫的孕育與生長，水與裂縫兩者互為影響的物理性質加劇潛變的行為；車瓜林斷層有著升溫脫水的證據，意味著此處曾有熱液活動的事實。
另外，國道三號於旗山斷層及車瓜林斷層間路段的垂直地表位移明顯抬升，本研究認為：此局部抬升現象係屬於東南-西北向板塊擠壓所造成之結果，但周圍的應力場可能逐漸轉變中。此局部塊體岩性為古亭坑泥岩，此區含水量高且屬於不易排水的阻水層，因此在側向應力的擠壓狀況下，容易形成塑性強烈的變性體，最終造成塊體產生由下往上抬升的垂直分量。

The Chishan Fault and Chekualin Fault revealed the deformation mechanism of mineral rocks is cracking and frictional sliding as well as dislocation creep. Due to the formation of Chishan Fault’s cracks, methane gas is strongly reduced. Pyrite is formed to fill the cracks, and the auxiliary deformation mechanism is grain boundary sliding. Calcite form mechanical twining in Chekualin Fault. The H2O result indicate the Chishan Fault in the water-rich environment, which is beneficial to the formation of fractures. The physical properties caused the creep deformation behavior. The Chekualin Fault has evidence of dehydration and belongs to strongly active fault.
In addition, the vertical segment of displacement between the Chishan Fault and Chekualin Fault is obviously uplifted. In this study, it is believed that uplift of block 2 is caused by the southeast to northwest direction of plate compression. The block lithology is Gutingkeng mudstone. The experimental results show that this area has higher water content and caused water-blocking layer which is not easy to drain. Therefore, under the extrusion of lateral stress, it is easy to form a degenerative body with strong plasticity.

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