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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 徐澔德(J Bruce H Shyu) | |
| dc.contributor.author | Ping-Kuan Hsieh | en |
| dc.contributor.author | 謝品寬 | zh_TW |
| dc.date.accessioned | 2022-11-24T03:09:15Z | - |
| dc.date.available | 2021-11-04 | |
| dc.date.available | 2022-11-24T03:09:15Z | - |
| dc.date.copyright | 2021-11-04 | |
| dc.date.issued | 2021 | |
| dc.date.submitted | 2021-10-26 | |
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/80555 | - |
| dc.description.abstract | 菲律賓位於歐亞板塊與菲律賓海板塊互相聚合形成的複雜地體構造區域，孕育了許多活動構造及地震。而薄荷島位於菲律賓中部，在西北東南向壓縮的構造環境下發育了許多褶皺與逆斷層。2013年菲律賓薄荷島發生了一場規模7.2的地震，造成了當地嚴重的生命財產損失，進一步認識該地區的活動構造特性便顯得十分重要。雖然薄荷島過去的地震紀錄顯示此區域具有構造活動，然而地質學家對本區域的活動構造仍知之甚少。在菲律賓中部的薄荷島南部海岸發育了一系列海階，這些海階是本區域受到構造抬升的地形證據。前人曾經針對本區域附近的邦勞島與帕米拉坎島上的海階進行研究，發現抬升速率具有空間分布上的差異，然而造成抬升，以及其速率差異的機制仍尚未明瞭。為增進對薄荷島構造活動的瞭解，本研究選定薄荷島南部海岸前人尚未探討過且廣泛分布的海階為研究對象。 本研究利用數值地形模型描繪階面及階崖分布，發現在薄荷島南部Loboc河東西兩側分別存在三階及五階海階；野外工作發現此區域海階主要由珊瑚礁石灰岩所構成，而由海階所採到的珊瑚樣本鈾釷定年結果可以對應到不同的海洋同位素階(MIS)。藉由建立地形剖面標定海階的海岸線角作為古海水面指標，本研究在分別討論海階形成年代後計算了本區域的長期抬升速率。 本研究所計算出的抬升速率顯示Loboc河口的東側抬升較西側快，而同一期海階階面側向高度變化亦顯示相同趨勢。由於前人所繪之East Bohol Fault並未切穿Loboc河河口，而該斷層於切穿薄荷島南部海岸處並未造成MIS 5e海階階面明顯的高低落差，本研究推測前人所繪之該斷層可能為一自13萬年以來較不活躍的分支，而該斷層西北側可能存在另一切穿Loboc河河口，且近期較活躍的分支斷層，其斷層活動造成Loboc河口東側的上盤抬升速率較Loboc河西側的下盤高。而由於抬升速率顯示薄荷島南部海岸整體而言均處在抬升狀態，本研究推測薄荷島南部外海的變形前緣可能為一呈東北東－西南西走向、向西北傾的逆斷層，此斷層的活動使薄荷島南部海岸抬升形成廣泛分布的海階。而薄荷島上一系列東北－西南走向的斷層及褶皺系統可能即是此逆斷層上盤的褶皺逆衝帶。由於此外海逆斷層仍可能為薄荷島南部帶來地震以及海嘯的威脅，本研究建議應進一步探討其活動特性及回歸週期，以作為訂定該地區防災政策的參考。 | zh_TW |
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| dc.description.tableofcontents | 口試委員審定書........................................................I 誌謝.................................................................II 摘要.................................................................III Abstract.............................................................V 目錄.................................................................VII 圖目錄...............................................................X 表目錄...............................................................XIII 第一章 前言.........................................................1 1.1 研究動機........................................................1 1.2 研究目的........................................................4 1.3 研究區域地理位置...............................................6 1.4 地體構造與地質概況.............................................6 第二章 前人研究.......................................................9 2.1 歷史地震......................................................9 2.1.1 1990年薄荷島地震...............................................9 2.1.2 2013年薄荷島地震...............................................10 2.2 活動構造.......................................................12 2.3 海階地形與活動構造的關聯........................................14 2.4 Panglao島的古海水面及抬升速率研究...............................16 第三章 研究方法.......................................................19 3.1 地形分析......................................................19 3.1.1 數值高程模型...................................................19 3.1.2 Google Earth衛星影像及街景服務..................................22 3.2 野外工作.......................................................22 3.3 放射性鈾釷同位素定年法..........................................24 3.3.1 鈾釷定年原理概述................................................24 3.3.2 鈾釷定年的限制..................................................27 3.3.3 珊瑚樣本前處理及鈾釷定年步驟.....................................27 3.4 海階地形剖面分析................................................28 3.4.1 海階地形剖面概述................................................28 3.4.2 利用海岸線角作為古海水面指標.....................................30 3.4.3 海階長期抬升速率計算.............................................32 第四章 研究結果........................................................34 4.1 海階地形分析結果.................................................34 4.1.1 Loboc河西側海階.................................................37 4.1.2 Loboc河東側海階.................................................40 4.2 野外工作結果....................................................42 4.2.1 Loboc河西岸.....................................................43 4.2.2 Loboc河東岸.....................................................48 4.2.3 Pamilacan島.....................................................54 4.2.4 小結............................................................56 4.3 放射性鈾釷分析結果...............................................58 4.4 海階地形剖面.....................................................63 4.4.1 A-A’剖面........................................................63 4.4.2 B-B’剖面........................................................66 4.4.3 C-C’剖面........................................................68 4.4.4 D-D’剖面........................................................70 4.4.5 E-E’剖面........................................................72 4.4.6 F-F’剖面........................................................74 4.4.7 G-G’剖面........................................................77 4.4.8 海階側向地形剖面（L-L’剖面）......................................79 第五章 討論............................................................81 5.1 海階抬升速率計算.................................................81 5.2 薄荷島海階分階及形成機制討論......................................84 5.2.1 A-A’剖面........................................................84 5.2.2 B-B’、C-C’剖面..................................................84 5.2.3 D-D’剖面........................................................86 5.2.4 E-E’剖面........................................................86 5.2.5 F-F’剖面........................................................87 5.2.6 G-G’剖面........................................................87 5.2.7 小結............................................................88 5.3 活動構造........................................................90 5.3.1 造成Loboc河東西側抬升速率差異的活動構造............................90 5.3.2 薄荷島南部外海可能存在的活動構造...................................93 第六章 結論............................................................96 參考文獻................................................................98 | |
| dc.language.iso | zh-TW | |
| dc.subject | 鈾釷定年 | zh_TW |
| dc.subject | 海階 | zh_TW |
| dc.subject | 菲律賓薄荷島 | zh_TW |
| dc.subject | 活動構造 | zh_TW |
| dc.subject | 抬升速率 | zh_TW |
| dc.subject | marine terraces | en |
| dc.subject | uplift rate | en |
| dc.subject | Bohol | en |
| dc.subject | U-Th dating | en |
| dc.subject | active tectonics | en |
| dc.title | 菲律賓薄荷島南部之第四紀海階及其構造意義 | zh_TW |
| dc.title | "Quaternary marine terraces in southern Bohol, Philippines and their tectonic implications" | en |
| dc.date.schoolyear | 109-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.advisor-orcid | 徐澔德(0000-0002-2564-3702) | |
| dc.contributor.oralexamcommittee | 李建成(Hsin-Tsai Liu),宮守業(Chih-Yang Tseng),王昱,姜宏偉 | |
| dc.subject.keyword | 菲律賓薄荷島,海階,活動構造,抬升速率,鈾釷定年, | zh_TW |
| dc.subject.keyword | Bohol,marine terraces,active tectonics,uplift rate,U-Th dating, | en |
| dc.relation.page | 106 | |
| dc.identifier.doi | 10.6342/NTU202104164 | |
| dc.rights.note | 同意授權(限校園內公開) | |
| dc.date.accepted | 2021-10-27 | |
| 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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