文學院

Permanent URI for this communityhttp://rportal.lib.ntnu.edu.tw/handle/20.500.12235/2

院成立於民國44年,歷經50餘年的銳意發展,目前設有國文、英文、歷史、地理、臺文等5個學系、翻譯和臺灣史2個獨立所,以及全球華人寫作中心和國際臺灣學研究中心。除臺史所僅設碩士班,其餘6個系所均設有碩、博士班;目前專兼任教師近250人,學生約2500餘人。

本院早期以培養優秀中學國文、英文、歷史和地理教師為鵠的,臺灣中學語文和史地教育的實踐與成功,本院提供不可磨滅的貢獻。近年來,本院隨師範體系轉型而調整發展方向,除維持中學師資培育的優勢外,也積極朝理論研究和實務操作等面向前進。目前,本院各系所師培生的教師檢定通過率平均在95%以上;非師培生在文化、傳播、文學、應用史學及環境災害、地理資訊系統等領域發展,也已卓然有成。

本院各系所教師的研究能量極為豐富,參與國內外學術活動相當活躍。根據論文數量、引用次數等指標所作的學術力評比,本院居人文領域全國第2名。各系所之間,無論是教師的教學與研究,或學生的生活與學習,都能相輔相成、榮辱與共,彼此渾然一體,足堪「為師、為範」而無愧。

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Now showing 1 - 6 of 6
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    海岸山脈東坡河階的地形學研究
    (地理學系, 1991-03-??) 張瑞津; 石再添; 曾正雄; 高鵬飛; 陳美鈴
    Owing to the continuous uplift since Quaternary, rejuvenated terraces, gorges and raised alluvial fans are developed well in the eastern slope of Coastal Range. The river terraces in this area are distributed below 200 m generally. The scarps of higher level terrace are larger than that of lower level one. The gravel deposits in higher level terrace are thicker than that of lower level one. Comparing the terrace between six studied rivers, meander terraces are significant both in Mawuku River, Fengpin River, Shuilien Riverand Fanshuliao River whereas fan terraces are developed well in Sanhsien River. In contrary, the terrace in Shuimuting River is undeveloped due to down cutting into hard rock which restricts the widening of terrace. By correlating to marine terraces, most of the terraces in this area are formed in Holocene. The detailed correlation of each step or dating still needs more envidences.
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    以折射震測法探討新社河階群
    (地理學系, 2004-11-??) 葛滿龍; 張瑞津; 王乾盈
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    利用淺層反射震測法探討公荖坪斷層
    (地理學系, 2006-05-??) 葛滿龍; 張瑞津; 王乾盈
    九二一大地震之後,車籠埔斷層及其相關構造引起學界熱烈的討論。本文探討豐原附近之公荖坪階地內的公荖坪斷層,該斷層鄰近車籠埔斷層北段轉彎處及地表破裂達九公尺的位置。過去的研究曾以航照判釋與野外調查指出該階地內有一明顯的斷層小崖,並推測公荖坪段層存在,且為車籠埔斷層的副斷層,但其地下構造卻始終從未被偵測。本研究以地形資料及淺層反射震測法 ,仔細檢查公荖坪斷層及其週遭的地下構造形貌,結果證實該斷層確實存在,並推測其可能的形成機制是受車籠埔斷層向西及向北逆衝而上時所伴生的副斷層;同時亦受到北側TT-boundary之障礙阻擋,以致上盤地層因錯動擠壓而撓曲變形,甚至衍生一條小規模的背衝逆斷層與部分的地層陷落。
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    新店溪河階之地形學研究
    (地理學系, 2000-11-??) 張瑞津; 鄧國雄; 劉明錡
    River terraces including six lateritic surfaces (LH、LT1-LT5) and three non-Iateritic surfaces (FT1-FT3) have been recognized along Hsin-tien River. Most of lateritic surfaces distributed concentrately at Ping-lin, Shen-chang-Pan and Hsin-tien. Comparatively speaking, surfaces LT4, LT5 and FT2 distributed more widely and continuously than the others. Under the effect of tilting, the channel tended to shift from south to north and became sinuos. Sinuosity increased to the maximum in the LT4 stage that imp1ied the river had a significant lateral erosion in relatively stable stage. FT terraces have been formed under the controlling effect eustatic fluctuation and subsidence of Taipei Basin. The meander cut occurred during the lowering base level stage (FT1-FT2). Referring the results of climatic and eustatic fluctuation, the LT5 and three FT surfaces have been formed respectively in high sea level around 40000, 10000, 6000 and 3000 years before present.
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    花東縱谷北段河階的地形學研究
    (地理學系, 1992-03-??) 張瑞津; 石再添; 沈淑敏; 張政亮
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    苗栗丘陵河階之地形學研究
    (地理學系, 1998-11-??) 張瑞津; 鄧國雄; 劉明錡
    苗栗丘陵區之階地至今仍殘存者,概分三義、銅苗及通霄等三區。三義區主要為高位紅壤階地,其階面高度 590 ~ 350m,對比為 LH、LT1、LT2 等三段。銅苗區的階地分布於後龍溪及西湖溪兩側, 其中高位紅壤階地的階面高度 300 ~ 150m,分為 LT3 ~ LT5三段,而非紅壤的低位階地分為 FT1 ~ FT3 三段;通霄區高位階地分布於南勢溪上游,階面高度 220 ~ 70m,分為 LT4、LT5 二段,低位階地分布於苑裡溪至大安溪之間。 階地的紅壤礫層一般厚約數公尺至十數公尺,上覆於頭嵙山層,其與火炎山相礫層不易分出界面,但與香山相砂頁岩層之界面較為清楚。 紅壤粒徑中數( Md φ)大部份介於 6.5 φ~ 7.0φ,各階地紅壤粒度並無規律變化。階地受新期斷層、背斜、向斜構造之影響,部份階面產生變形。三義區階地向東及向北傾動,八甲一帶的階地呈向斜變位。通霄東南之階地於倒梯崎則成反斜崖現象。 至於三義至銅鑼的階地西側陡崖有 100 ~ 330m 的落差,狀似斷層崖,再經侵蝕而成,但其斷層面可能發生在火炎山相巨厚的礫層中,故不易直接找到變位證據。依本區階地高度、紅壤粒度、礫石覆瓦的特徵,三義南段階地及通霄階地似為大安溪階地的殘面,而三義以北的階地由後龍溪逐次堆積而成。古後龍溪由南轉向北,階地可分為九階,紅壤六階,非紅壤三階,西湖溪為其舊流路。