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資料類型 學位論文 
主要題名 湖口斷層淺層反射震測之研究 
作者 林良安 
出版日期 2000 
頁碼或冊數 109 
中文摘要 湖口斷層位於湖口台地北緣,南側湖口台地已知為湖口背斜,北邊依序為楊梅地塹、平鎮背斜及雙連坡向斜(Hsiao,1967),經此後一直向北方外海之觀音高區抬升,讓人不禁懷疑其中與弧陸碰撞所造成之碰撞前緣的關連性.湖口斷層由於鮮少露頭被發現,斷層位置多為台地堆積層所覆蓋,前人所作之震測研究於淺層構造因解析度不足較為模糊不清,故本研究施以淺層反射震測調查,期能明瞭地下淺層構造以及地層錯動情形. 
英文摘要 The Hukou fault is located at the northern border of the Hukou terrace. It runs almost in the east-western direction. Physiographically, the fault looks like a scarp along the terrace’s boundary and is generally attributed as an active fault.The purpose of this study is to detect the Hukou fault and the structures in its vicinity using the shallow seismic reflection method. Several long-range seismic lines (400 m long) are distributed perpendicular to the fault trace with the visible seismic images down to the depth of 700 meters. Besides this, we also used five short-range seismic lines across the Hukou anticline, from the edge of the terrace to Tienzuhu, to investigate the structure of this fault-related anticline. After carefully reserving the characteristics of each reflector, we are able to correlate different layers on different seismic profiles. 
出版者 國立中央大學地球物理研究所 
出版地 桃園縣 
關鍵詞 新竹縣;湖口鄉;湖口斷層;活動斷層;淺層反射震測