請用此 Handle URI 來引用此文件：
http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/31914完整後設資料紀錄
| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 劉家瑄(Char-Shine Liu) | |
| dc.contributor.author | Li-Chung Feng | en |
| dc.contributor.author | 馮力中 | zh_TW |
| dc.date.accessioned | 2021-06-13T03:24:20Z | - |
| dc.date.available | 2006-08-01 | |
| dc.date.copyright | 2006-08-01 | |
| dc.date.issued | 2006 | |
| dc.date.submitted | 2006-07-28 | |
| dc.identifier.citation | 中文部分
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(1995) Fission-track dating of volcanics in the northern part of the Taiwan–Luzon arc: eruption ages and evidence for crustal contamination. J. SE Asian Earth Sci., 11, 81–93. Yeh, Y.C. and Hsu, S.K. (2004) Crustal structures of the northernmost South China Sea: seismic reflection and gravity modeling. Mar. Geophys. Res., 25, 45-61. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/31914 | - |
| dc.description.abstract | 台灣南部海域北緯21度20分以南，歐亞板塊上的南中國海岩石圈，沿馬尼拉海溝向東隱沒至菲律賓海板塊下，形成呂宋島弧隱沒系統。南中國海洋地殼上的沉積物在加入隱沒系統時被刮積形成增積岩體，並有北呂宋海槽發育；北緯21度20分以北，隱沒逐漸轉為初始碰撞作用，增積岩體西側承接來自台灣造山帶及歐亞大陸之大量沉積物，東側由背向逆衝斷層將弧前盆地沉積物併入，往北發展成寬廣的楔形體，為台灣南部海域最主要的大地構造單元之ㄧ。
由馬尼拉海溝至恆春海脊，增積岩體可依地形及構造的特性，區分為上部、下部斜坡帶。下部斜坡帶位於增積岩體前緣，坡面相當平緩，水深約由3500公尺減少至2500公尺，覆瓦狀的褶皺及逆衝斷層為主要的構造特徵；上部斜坡帶位於增積岩體核心部份，水深由2500公尺驟減為1500公尺，因受到強烈的擠壓變形，使內部反射信號不連續，幾乎難以找到反射層。上部、下部斜坡帶之間，有一主要的脫序逆衝斷層發育，是為上部、下部斜坡帶的分界。 增積岩體上的褶皺與逆衝斷層，由南往北斷層彼此之間的間距增加，應是由於往北接近台灣造山帶及中國大陸邊緣時，沉積速率增加，使得輸入隱沒系統的沉積物增厚，因而造成逆衝斷層彼此之間的間距也有增加的趨勢。 當隱沒作用轉為碰撞作用時，部份的弧前基盤被俯衝至島弧之下，觸發了切過上部斜坡帶底部的主要脫序逆衝斷層。我們推測當弧前基盤向東俯衝的同時，主要的脫序逆衝斷層亦將上部斜坡帶這個較老且硬的岩體向西逆衝，在此岩體的推擠之下部斜坡帶最東側的部份受到變形並被抬昇，最終將這個部份併入了上部斜坡帶。這個藉由脫序逆衝斷層將下部斜坡帶逐步併入上部斜坡帶的行為，可能在台灣南部海域增積岩體上反覆地運行，並向西傳遞。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2021-06-13T03:24:20Z (GMT). No. of bitstreams: 1 ntu-95-R92241313-1.pdf: 7133706 bytes, checksum: 17082663903c9c3f2104bb97c4e7c0dd (MD5) Previous issue date: 2006 | en |
| dc.description.tableofcontents | 摘要 ……………..……………………………………………………… I
目錄 ……………...…………………………………………………… III 圖目 …………………………………………………………………… V 表目 …………………………………………………………………... VI 第一章 緒論 …………………………………………………………... 1 1-1 地質背景 …………………………………………………...... 1 1-2 研究動機及目的 ………………………………………….... 12 第二章 研究方法 ................................................................................. 15 2-1 資料來源 …………………………………………………… 15 2-2 資料處理 ................................................................................ 18 2-2.1 EW9509-46震測資料處理 ……………………………... 18 2-2.2 MCS579航次震測資料處理 …..………………………... 28 第三章 構造形態與震測剖面解釋 …………………………………. 31 3-1 構造形態概述 …………..………………………………….. 31 3-2 北緯21度20分以南以隱沒作用為主之區域 …………….. 33 3-2.1 MW9006-76震測剖面 …………………………...……... 33 3-2.2 EW9509-46震測剖面 ……………………………...…… 33 3-2.3 脫序逆衝斷層 …………………………………………... 37 3-3 北緯21度20分以北以最初碰撞作用為主之區域 ……….. 40 3-3.1 MCS579-1震測剖面 ……………………………………. 40 3-3.2 脫序逆衝斷層 …………………………………………... 42 3-4 區域性的構造特徵-基盤突起的隱沒 ……………………... 42 第四章 討論 …………………………………………………………. 49 4-1 逆衝斷層的間距由南往北增加 …………………………… 49 4-2 增積岩體的構造演化 ……………………………………… 50 4-3 主要的脫序逆衝斷層與台灣陸上斷層的連接 …………… 59 第五章 結論 ………….……………………………………………… 63 參考文獻 ……………………………………………………………... 65 | |
| dc.language.iso | zh-TW | |
| dc.title | 台灣南部海域增積岩體的構造特徵 | zh_TW |
| dc.title | Structural Features of the Accretionary Wedge Offshore Southern Taiwan | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 94-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 許樹坤(Shu-Kun Hsu),胡植慶(Jyr-Ching Hu),盧佳遇(Chia-Yu Lu) | |
| dc.subject.keyword | 增積岩體,褶皺,逆衝斷層,脫序逆衝斷層,反射震測,台灣南部海域, | zh_TW |
| dc.subject.keyword | Accretionary wedge,Fold and thrust,Out-of-sequence thrust,seismic reflection,South offshore Taiwan, | en |
| dc.relation.page | 68 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2006-07-29 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 海洋研究所 | zh_TW |
| 顯示於系所單位： | 海洋研究所 | |
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