研究生: |
楊惠君 |
---|---|
論文名稱: |
泰國西北部達府地區之構造史研究 |
指導教授: |
李通藝
Lee, Tung-Yi |
學位類別: |
碩士 Master |
系所名稱: |
地球科學系 Department of Earth Sciences |
論文出版年: | 2007 |
畢業學年度: | 95 |
語文別: | 中文 |
論文頁數: | 98 |
中文關鍵詞: | 泰國 、達府 、構造 、王朝斷層 |
論文種類: | 學術論文 |
相關次數: | 點閱:147 下載:16 |
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本研究測量泰國西北部達府 (Tak) 附近的藍山 (Lansang) 片麻岩帶及普密蓬 (Bhumibol) 水壩區之野外構造,並採集定向標本。製成定向薄片後,測量顯微構造的基質葉理走向及傾角,利用電腦軟體計算出最符合數據的葉理面位態。將野外構造與顯微構造測量結果加以比對與分析後,顯示二區域都各觀測到三期的葉理及一期斷層。因此,本研究對於此地區提出以下四期構造史:第一期可能在晚白堊紀~早第三紀時,因緬甸板塊和撣邦地塊 (Shan - Thai) 的碰撞,造成清邁-臨滄 (Chiang Mai - Lincang) 之間南-北向的褶皺帶,而形成南-北向且傾角大的葉理;第二期可能在32.5~30.5 Ma時,因王朝 (Wang Chao) 斷層帶發生塑性左移運動,造成陡峭且帶有左移剪切的褶皺,形成藍山片麻岩上西北-東南向且傾角大的葉理;第三期為地殼增厚造成垂直方向上強烈的岩壓,形成偃臥褶皺和水平的葉理;第四期為斷層活動,藍山片麻岩帶為左移斷層,普密蓬水壩區則為向東逆衝的斷層活動。由此研究方法所量得之葉理面位態或許有些許誤差,但在許多測量結果比對下所推論的大構造是明確的。
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