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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 | Jhih-Hong Wang | en |
dc.contributor.author | 王志宏 | zh_TW |
dc.date.accessioned | 2021-06-17T04:25:38Z | - |
dc.date.available | 2028-12-31 | |
dc.date.copyright | 2018-08-18 | |
dc.date.issued | 2018 | |
dc.date.submitted | 2018-08-14 | |
dc.identifier.citation | 參考文獻
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dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/70310 | - |
dc.description.abstract | 中文摘要
本研究藉由臺灣西部前陸盆地系統之震測剖面,了解臺灣海峽東部自被動大陸邊緣環境而轉進入前陸盆地系統之沈積地層與前陸層序演化之構造意義。地體架構上,臺灣海峽東部係為上新世以來臺灣造山帶重壓歐亞板塊邊緣,致使地殼撓曲沉降所形成之臺灣西部前陸盆地的一部分。在前陸盆地的外緣,地殼則因撓曲抬升而成為伸張環境,並在其淺部形成一系列的上新世-第四紀撓曲型正斷層,是臺灣西部前陸盆地在構造活動上的重要特徵。此構造廣泛出現於臺灣海峽,本研究即對於撓區形成的正斷層、其空間分布和傾角的特徵,以及形成機制進行探討。 本研究利用臺灣海峽地區新收集的反射震測資料與已發表的鑽探井位以及反射震測剖面進行對比,根據不整合面的分布,確立區域內主要的地層年代架構,同時了解該區域內斷層構造的特徵與分布。除了繪製前陸基底不整合面的分布,亦發現許多上新世以來的正斷層,其分布的深度較淺。本區域的正斷層切過的地層,上下地層間的斷距小,側向延伸的距離短,從形貌上推測,此區域的斷層可能為撓區型正斷層,主要分布在臺灣海峽中部至彰濱外海彰雲沙脊的地區。 本研究透過震測剖面來探討此區域的斷層分布以及其傾角數值,以對此區域的海床穩定度做一個評估,並可以提供工程界在於沙箱模擬實驗上提供所需的關鍵數據(例如:斷層傾角),讓此區域穩定度的評估可更加準確,亦可將地質與工程做一個銜接。因近來政府在此區域內域發展風力發電,故希望研究之成果對於風場計畫選址方面可以提供些許貢獻。 | zh_TW |
dc.description.abstract | Abstract
The western Taiwan Foreland Basin lies on the eastern part of Taiwan Strait. Structures in this region are dominated by crustal stretching and a series of flexural normal faults have been developed since Late Miocene owing to the flexural of the Eurasia Plate. Through deciphering multi-channel seismic data, these flexural features are analyzed in the offshore Changhua coastal area. The flexure normal faults are important features to realize structural activities in the western Taiwan Foreland Basin. It should be a significant issue to decipher whether these faults are still active. In this study, we analyze all the available seismic reflections profiles in the central part of the Taiwan Strait, and have observed many pre-Pliocene normal faults that are mainly distributed in the middle of the Taiwan Strait to Changyun Rise. We tentatively suggest that the formation of these faults may be associated with the formation of the foreland basal unconformity. So, we idenify the faults from multi-channel seismic profiles, and try to recognize their continuity. For getting the dip angles of the faults, we convert the seismic profiles from time domain into depth domain. We can provide important parameters to sandbox experiment to evaluate the seafloor stability of this area. As our government plans to establish offshore wind power generaters in this area, I hope this research could contribute to that green energy project. | en |
dc.description.provenance | Made available in DSpace on 2021-06-17T04:25:38Z (GMT). No. of bitstreams: 1 ntu-107-R04241409-1.pdf: 9541971 bytes, checksum: 903d1b8652ee7b33e0dc8eee3ef311fb (MD5) Previous issue date: 2018 | en |
dc.description.tableofcontents | 目錄
致謝 I 中文摘要 Ⅲ Abstract Ⅳ 目錄 V 圖目錄 VII 第一章 前言 1 1-1前言 1 1-2研究目的與方法 2 1-3本論文架構 3 第二章 區域背景 6 2-1臺灣新生代地體構造 6 2-2前陸盆地系統 7 第三章 研究方法 11 3-1資料處理流程 11 3-2 震測資料處理 11 3-3資料分析 16 第四章 研究結果 24 4-1研究區域的構造特徵 24 4-2前陸基底不整合面之地層等厚圖 25 4-3區域構造圖以及其應用 26 第五章 結果討論 38 5-1區域內正斷層的屬性 38 5-2 區域內斷層走向的轉換機制 38 5-3區域穩定性之探討 39 第六章 結論 44 參考文獻 45 | |
dc.language.iso | zh-TW | |
dc.title | 晚中新世以來
臺灣海峽東部前陸盆地之斷層構造 | zh_TW |
dc.title | Fault Structures of Foreland Basin
in the Eastern Taiwan Strait since Late Miocene | en |
dc.type | Thesis | |
dc.date.schoolyear | 106-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 蘇志杰(Chih-Chieh SU),許鶴瀚(Ho-Han Hsu),楊耿明(Kenn-Ming Yang) | |
dc.subject.keyword | 臺灣海峽,前陸盆地,反射震測,斷層構造,撓區型正斷層, | zh_TW |
dc.subject.keyword | Taiwan Strait,Foreland basin,Multichannel seismic reflection profile,fault structures,flexural normal fault, | en |
dc.relation.page | 51 | |
dc.identifier.doi | 10.6342/NTU201803436 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2018-08-15 | |
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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