2.58-2.88 公釐，若將可能的誤差加入考慮之中，滑移速率範圍則為每年 2.58-3.30 公釐。
參考文獻
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中文與日文文獻
水利署(2009) 表 18 縣(市)管河川，取自 https://www.wra.gov.tw/media/14209/f-temp-attachment-071615533971.pdf。
台中州政府（1936，日文）昭和十年臺中州震災誌。台灣：台中州政府。
說明書（第一版）。臺北縣：經濟部中央地質調查所。
張麗旭(1955)臺灣之地層。臺灣銀行季刊，第七卷，第 2 期，26-49 頁。
陳于高(1987)大漢溪下游河階台地碳十四定年與對比之研究（碩士論文），國立台 灣大學，臺北市。
陳培中(2005)以 GPS 觀測資料探討鐵砧山地區地表變動與地下構造（碩士論文）。
國立中央大學，桃園縣。
附錄一、定年報告
HWJ-08(14C)
HWJ2-09(OSL)
附錄二、階地判釋結果及文中照片位置
各圖之相對位置，a-g 各圖之等高線間距為 10 公尺。
a：西湖溪下游段與好望角北部
b：西湖溪銅鑼至西湖段
c：西湖溪銅鑼附近河段
d：好望角群南部
e：北勢窩溪流域
f：南勢溪下游段
g：南勢溪上游段
附錄三、謝誌
註1除了從書籍當中學習的知識層以外，在新生國小所培育出的學習態度也同樣
有條理的邏輯整理，讓我得以將這些片段的知識融為一體，並接觸到許多足以應付
準備這次考試的過程中，必須要特別感謝葉昭松老師的指導，並提供我們校隊念
除此之外，也要特別感謝鄧屬予老師在各種課程當中，利用他那獨到的講課方
因為大學四年都在打混摸魚中度過的緣故，我一直到很後來才決定要考研究
構造地形學、階地 mapping，這些東西基本上就是我大學時候最感興趣，也學最多 的東西，就像是把整個大學四年所學到的東西做一個總結，也因為這個緣故，在這
陳承鴻、元禄、劉司捷等前輩的建議，以及 Cai 原閔學長所精心準備的零食，讓我
當然隨著研究進展到最後，進入論文撰寫的階段，需要許多複雜的軟體運用以
而在最後，我必須感謝一直陪伴我的女朋友鐘萱，在地質系的這七年半得過得 這麼開心，很大一部份是因為有妳。無論是一起在面對作業以及考試上奮鬥，或只 是單純的聊天打屁，都是我相當重要的精神支柱。在研究所期間，甚至願意幫我海 報做排版、畫論文的圖、修改論文的錯別字、承受我那些暴躁以及遷怒、甚至花錢 陪我一起到歐洲朝聖一個鳥不生蛋的小鎮。這六年半來，甚至未來還有很多年，真 是辛苦妳了。
從天文一路到地質，我在科學這條路上能夠走到今天，完成這篇論文，必須感 謝這篇文章當中提到的每一個人事物，讓我對科學以及知識的熱誠從未熄滅。接下 來如果沒意外的話，我應該是會離開學術這條道路，若哪天遇到童年的自己，我想 對他說：
抱歉，科學這條路可能要暫停一下了 這篇論文當作個交待，應該還算是及格吧
還有，我要在此感謝黃怡穎，喜歡上你這件事也給我很多意料之外的動力，遇 見妳在我大學時代的重要性，可能不比鐘萱差多少。
註：「致謝」是指對他人表達謝意，「謝誌」則是為了表達謝意而寫的文章。因此，
本研究認為「謝誌」更適合作為這篇文章的標題。