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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 龔源成 | |
| dc.contributor.author | Alex Chih-Hsuan Su | en |
| dc.contributor.author | 蘇志軒 | zh_TW |
| dc.date.accessioned | 2021-06-16T04:07:01Z | - |
| dc.date.available | 2014-09-03 | |
| dc.date.copyright | 2014-09-03 | |
| dc.date.issued | 2014 | |
| dc.date.submitted | 2014-08-30 | |
| dc.identifier.citation | 英文部分：
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Soh, W., Tokuyama, H., (2002) Rejuvenation of submarine canyon associated with ridge subduction, Tenryu Canyon, off Tokai, central Japan. Mar. Geol. 187: 203-220. Teng, L.S. (1990) Geotectonic evolution of late Cenozoic arc-continent collision in Taiwan. Tectomophysics 183: 57-76. Twichell, D. C., Knebel, H.J., Folger, D.W., (1977) Delaware river: evidence for its former extension to Wilmington submarine canyon. Science 195: 483-485. Paul Wessel and Walter H. F. Smith, (1998) The generic mapping tools. School of ocean and earth science and technology, University of Hawaii at Manoa. Yu, H.S., Liu, C.S., Lee, J.T., (1992) The Kao hsiung submarine canyon: A modern aborted canyon and its morphology and echo character. Acta Oceanogr. Taiwanica 28: 19-30. Yu, H.S., Lu, J.C., (1995) Developmeant of the shale diaper-controlled Fangliao Canyon on the continental slope off southwestern Taiwan. Jour. SE Asian Earth Sci. 11: 265-276. 中文部分： 潘玉生、陳讚煌、鐘火盛、游銘銳，1992，震測資料之認識與解釋，中油探採叢 書，共127頁。 黃譯增，1998，台灣西南海域壽山海底峽谷的形貌及其在斜坡上的意義，國立台 灣大學海洋研究所碩士論文。 高溥聲，2008，恆春半島西側與南側海底地形特徵初步探討，國立台灣大學海洋 研究所碩士論文，共140頁 曾世霖，2011，台灣西南外海高屏峽谷沉積物及沉積機制研究，國立中央大學地 球物理研究所碩士論文。 共153頁 倪錦江，2012，南海北部大陸邊緣斜坡海脊含天然氣水合物地層的構造與沉積特 徵。共94頁 | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/55518 | - |
| dc.description.abstract | 過去研究對於高屏海底峽谷整個區域已經有一定程度的了解，然而對於下游部分是否有海底沖積扇以及峽谷下游曲流的環境和演進尚未有明確的結果和解釋。本研究目的在於提供過去較缺乏資料的下游段新的地質資訊，並且驗證海底扇的存在與否以及建立一個曲流可能的演進過程。
本研究使用多頻道反射震測資料來分析，運用「層序分析」為主要解釋震測剖面資料的觀念，觀察各震測相特徵並且辨識層序邊界，發現本研究區域於峽谷下游頭部存在一海底扇，主要可分成「水道堆積物」、「溢堤堆積物」、以及「峽谷底部堆積物」3種沉積物，並且可分成4個時期討論。藉由沉積物於各個時期沉積的情形，推論包括前人指出的褶皺「R3.4」(Lin et al., 2008)以及本研究新發現的「褶皺A」和「褶皺B」的活動時期，加以由震測剖面上觀察到古峽谷的分布情形，進一步推論峽谷與水道於各個時期的行經路徑。 沉積物由陸地經由高屏海底峽谷輸送，於高屏海底峽谷下游堆積形成海底扇，峽谷兩側斜坡盆地將沉積物限制於其中，峽谷本身也受構造影響而以曲流方式行進，因此海底扇形貌上與一般情形略有不同。 | zh_TW |
| dc.description.abstract | The Kaoping Submarine Canyon offshore southwestern Taiwan has been widely studied, however, the submarine fan distribution and the cause of canyon meandering of the Kaoping Submarine Canyon lower section are still unclear. The purposes of this study are to investigate the sediment distribution of the submarine fan and to develop a model for canyon meandering process.
In this study, multi-channel seismic reflection data are analyzed by using the “Sequence analysis” approach. The submarine fan sediment can be classified into 3 types: “channel deposits”, “overbanking deposits”, and “Canyon thalweg”. We have identified 4 deposition stages from seismic sequence analysis. The active stages of Fold R3.4, Fold A, and Fold B have all affected the development of the submarine fan. Further with analyzing the paleo-canyon and paleo-channle on the seismic profiles, evolution of the canyon and channel has been established in this study. Sediments has been transported from land to deep sea and deposited at lower section Kaoping Submarine Canyon. Two slope basins confine the overbanking sediments. Canyon is meandering due to the activities of Folding. Therefore, the shape of submarine fan is different from general cases. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-16T04:07:01Z (GMT). No. of bitstreams: 1 ntu-103-R99224104-1.pdf: 27252942 bytes, checksum: 8b8e94b80cc706c2adc3841b860db0c9 (MD5) Previous issue date: 2014 | en |
| dc.description.tableofcontents | 口試委員會審定書……………………………………………………i
謝誌……………………………………………………………………ii 摘要……………………………………………………………………iv Abstract………………………………………………………………v 目錄……………………………………………………………………vi 圖目………………………………………………………………viii 表目…………………………………………………………………xi 第一章 序言……………………………………………………………1 1.1 海底峽谷與海底扇……………………………………………1 1.2 高屏海底峽谷…………………………………………………3 1.3 研究區域………………………………………………………5 1.4 研究動機與目的……………………………………………5 第二章 區域地質背景………………………………………………… 11 2.1 大地構造……………………………………………………11 2.2 台灣西南海域………………………………………………11 第三章 研究方法…………………………………………………… 16 3.1 資料來源……………………………………………………16 3.2 震測資料處理與解釋方法…………………………………16 3.2.1資料處理流程簡述………………………………… 16 3.2.2震測資料解釋方法……………………………………18 第四章 研究結果與討論…………………………………………… 25 4.1 剖面解釋…………………………………………………… 25 4.2 各時期沉積物分布………………………………………… 31 4.3 各時期構造作用…………………………………………… 33 4.4 峽谷演進…………………………………………………… 35 4.5 綜合解釋 ……………………………………………………36 第五章 結論………………………………………………………… 75 參考文獻………………………………………………………………77 英文部分 …………………………………………………………77 中文部分……………………………………………………………79 | |
| dc.language.iso | zh-TW | |
| dc.title | 台灣西南海域高屏峽谷下游段之沉積物分布與峽谷演進 | zh_TW |
| dc.title | Sediment Distribution and Canyon Evolution of the Lower Section Kaoping Submarine Canyon, Offshore South West Taiwan | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 102-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.coadvisor | 劉家瑄 | |
| dc.contributor.oralexamcommittee | 李通藝,林殿順 | |
| dc.subject.keyword | 海底扇,高屏海底峽谷,震測剖面解釋,台灣西南海域, | zh_TW |
| dc.subject.keyword | Submarine fan,Kaoping Submarine Canyon,Multi-channel seismic reflection data,Offshore Southwest Taiwan, | en |
| dc.relation.page | 78 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2014-09-01 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 地質科學研究所 | zh_TW |
| 顯示於系所單位： | 地質科學系 | |
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