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http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/99311完整後設資料紀錄
| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 徐澔德 | zh_TW |
| dc.contributor.advisor | J Bruce H. Shyu | en |
| dc.contributor.author | 陳承鴻 | zh_TW |
| dc.contributor.author | Cheng-Hung Chen | en |
| dc.date.accessioned | 2025-08-22T16:08:00Z | - |
| dc.date.available | 2025-08-23 | - |
| dc.date.copyright | 2025-08-22 | - |
| dc.date.issued | 2025 | - |
| dc.date.submitted | 2025-08-06 | - |
| dc.identifier.citation | 第一章之參考資料
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/99311 | - |
| dc.description.abstract | 臺灣屬於活躍的造山帶，擁有眾多孕震構造與頻繁的地震活動。在此地質背景下，臺灣地震模型（Taiwan Earthquake Model）計畫已辨識出45條陸域孕震構造，並廣泛應用於災害評估與防災。然而，儘管臺灣近海曾報導具有多個活動構造與豐富的歷史地震紀錄，目前仍缺乏系統性的海域孕震構造資料庫供防災使用。
本研究整合臺灣周邊海域的地質與地球物理資料，藉由反射震測剖面中不連續反射訊號所指出的斷層是否延伸至海床，以及海底地形圖中構造線形的側向延續性，共辨識出54條近海孕震構造的位置與地下幾何形態。本研究更進一步推估其孕震參數，包含可能的地震規模、長期滑移速率與地震再現週期。根據三種斷層幾何與地震規模關係式，並考慮海陸構造聯合破裂的情況下，所有海域構造皆有能力產生規模6.5以上的地震。由於在隱沒帶中，因物質特性使得構造的部分應力可能以無震潛移方式釋放，故本研究引用隱沒帶的耦合率資料調整滑移速率，重新估計各斷層的有效應變累積量。結果顯示，滑移速率較高（約10–20 mm/yr）的構造主要分布於琉球與馬尼拉隱沒帶的上盤區域，對應的地震再現週期小於1000年；而滑移速率較低（約0.1–2.0 mm/yr）的構造則位於臺灣東北外海的後造山區，再現週期多數大於6000年。 由於震測剖面資料品質與地形解析度的限制，構造參數仍存有相當大的不確定性，需進一步優化。本研究建立了第一版適用於地震危害度分析的海域斷層資料庫，預期能提升臺灣地區的地震危險度評估，並促進臺灣的地震科學研究朝向海洋發展。本研究所提出構造長期滑移速率的估計方法，也期望能夠應用於其他缺乏定年資訊的海域構造研究中。 | zh_TW |
| dc.description.abstract | Taiwan is an active orogenic belt characterized by numerous seismogenic structures and frequent earthquakes. In this dynamic setting, the Taiwan Earthquake Model (TEM) project has identified 45 on-land seismogenic structures, widely used for disaster assessment and preparedness; however, despite reports of active structures and many historical earthquakes offshore Taiwan, a comprehensive offshore seismogenic structure database is still lacking for seismic hazard analysis.
This study integrates geological and geophysical data to determine the locations and subsurface geometries of offshore structures. Based on two criteria, namely the seabed disturbance by faulting in seismic reflection profiles and the lateral continuity of seafloor structural lineaments, 54 structures offshore Taiwan were identified and mapped. This study further estimated their structural parameters, such as capable earthquake magnitude, long-term slip rate, and the mean earthquake recurrence interval. By employing three fault geometry–earthquake magnitude scaling relationships and considering possible multi-fault rupture scenarios between on-land and offshore faults, this study finds that all identified offshore structures are capable of generating earthquakes of Mw ≥ 6.5. In subduction zones, some tectonic stress may be released aseismically due to material properties. To account for this, published coupling ratio data were applied to adjust slip rates, refining estimates of effective strain accumulation on fault planes. Our results show that the area with fast-slipping (~10–20 mm/yr) structures is located on the hanging wall side of the Ryukyu and Manila subduction systems, corresponding to recurrence intervals of less than 1,000 years, whereas structures with lower slip rates (~0.1–2.0 mm/yr) are located in the post-collision zone off northeast Taiwan, with most recurrence intervals more than 6,000 years. Due to limitations in seismic-profile quality and bathymetric resolution, these parameters still have large uncertainties and require further refinement. However, by establishing this first version offshore database, it is expected to enable not only improved assessments of earthquake hazards in Taiwan but also to promote marine-focused seismic research. Moreover, the proposed method for estimating long-term slip rates offers applicability to offshore seismogenic structures in other regions lacking geochronological constraints. | en |
| dc.description.provenance | Submitted by admin ntu (admin@lib.ntu.edu.tw) on 2025-08-22T16:08:00Z No. of bitstreams: 0 | en |
| dc.description.provenance | Made available in DSpace on 2025-08-22T16:08:00Z (GMT). No. of bitstreams: 0 | en |
| dc.description.tableofcontents | 目次
誌謝 I 口試委員會審定書 IV 摘要 V Abstract VI 目次 VIII 圖次 XIII 表次 XVI 第一章、緒論 1 1.1 前言 1 1.2 論文章節架構 8 1.3 第一章之參考資料 9 第二章、 臺灣地震模型（TEM）之決定臺灣海域孕震構造的位置與發震潛能 11 第二章摘要 11 2.1 前言 12 2.2 研究區域與地質背景 13 2.3 研究方法 13 2.3.1 決定海域孕震構造的位置 14 2.3.1.1 標準一、震測剖面中孕震構造須切穿或擾動近海床地層 19 2.3.1.2 標準二、海底地形圖顯示之孕震構造具有側向延伸的海床線形 19 2.3.2 判斷構造的運動方式 21 2.3.3 決定構造的地下幾何 21 2.3.4 決定構造的發震規模與單一地震事件錯移量 22 2.4 臺灣海域孕震構造之位置與地下幾何 25 2.4.1 Domain A：臺灣北部外海地質區（位於沖繩海槽之北部，#1–#11） 25 2.4.1.1 臺灣北部外海地質區的地質背景 25 2.4.1.2 臺灣北部外海地質區的構造個論 27 2.4.1.3 臺灣北部外海地質區的構造地下幾何 29 2.4.2 Domain B：沖繩海槽南段地質區（#12–#17） 29 2.4.2.1 沖繩海槽南段地質區的地質背景 29 2.4.2.2 沖繩海槽南段地質區的構造個論 30 2.4.2.3 沖繩海槽南段地質區的構造地下幾何 31 2.4.3 Domain C：琉球隱沒系統上盤地質區（#18–#21） 32 2.4.3.1 琉球隱沒系統上盤地質區的地質背景 32 2.4.3.2 琉球隱沒系統上盤地質區的構造個論 34 2.4.3.3 琉球隱沒系統上盤地質區的構造地下幾何 35 2.4.4 Domain D：臺灣東部外海地質區（#22–#28） 36 2.4.4.1 臺灣東部外海地質區的地質背景 36 2.4.4.2 臺灣東部外海地質區的構造個論 37 2.4.4.3 臺灣東部外海地質區的構造地下幾何 42 2.4.5 Domain E：臺灣西南外海地質區（#29–#50） 44 2.4.5.1 臺灣西南外海地質區的地質背景 44 2.4.5.2 臺灣西南外海地質區的構造個論 46 2.4.5.3 臺灣西南外海地質區的構造地下幾何 47 2.4.6 Domain F：臺灣西部外海地質區（#51–#54） 48 2.4.6.1 臺灣西部外海地質區的地質背景 48 2.4.6.2 臺灣西部外海地質區的構造個論 54 2.4.6.3 臺灣西部外海地質區的構造地下幾何 55 2.5 討論 58 2.5.1 本研究孕震構造的定義限制 58 2.5.1.1 前人研究的資料品質與數量 58 2.5.1.2 海床侵蝕與堆積作用的影響 58 2.5.1.3 無法判釋出深處的構造 59 2.5.1.4 不易決定構造的水平運動分量 60 2.5.2 估計孕震構造的發震規模 60 2.5.2.1 單一構造破裂模型 60 2.5.2.2 斷層分段破裂與聯合破裂模型 68 2.5.3 海域孕震構造的歷史地震 70 2.5.4 海陸域孕震構造位置的應用性與未來研究展望 72 2.6 結論 74 2.7 第二章之參考資料 75 第三章、 臺灣地震模型（TEM）之決定臺灣海域孕震構造的長期滑移速率 97 第三章摘要 97 3.1 前言 98 3.2 臺灣海域的地質背景與新構造分區 99 3.3 研究區域與方法 99 3.3.1海域構造滑移速率估計方法 100 3.3.2 海底地形的分析與測量 103 3.3.3 震測剖面的分析與測量 103 3.4 臺灣海域孕震構造的滑移速率估計 104 3.4.1 Domain A：東北外海構造（#1–#11） 104 3.4.2 Domain B：沖繩海槽南段地質區（#12–#17） 109 3.4.3 Domain C：琉球隱沒系統上盤地質區（#18–#21） 113 3.4.4 Domain D：臺灣東部外海地質區（#22–#28） 119 3.4.5 Domain E：臺灣西南外海地質區（#29–#50） 131 3.4.6 Domain F：臺灣西部外海地質區（#51–#54） 138 3.5 討論 150 3.5.1 外海構造長期滑移速率值的空間分布 150 3.5.1.1 臺灣東部外海的構造滑移速率分布 151 3.5.1.2 臺灣北部外海的構造滑移速率分布 154 3.5.1.3 沖繩海槽擴張速率與海槽內孕震構造的活動性討論 154 3.5.1.4 臺灣南部外海的構造滑移速率分布 156 3.5.2 孕震構造的地震再現週期 158 3.5.3 海域構造之活動紀錄與歷史文獻記載比對 167 3.5.4 海域孕震構造參數的敏感度分析 167 3.5.5 海域孕震構造的長期滑移速率值之優化 168 3.5.6 海域孕震構造資料庫之應用與展望 171 3.6 結論 172 3.7 第三章之參考資料 173 第四章、海域孕震構造資料庫的綜合討論 185 4.1 研究成果比較 185 4.1.1 成果與臺灣地震模型之陸域孕震構造資料庫比較 185 4.1.2 成果與其他臺灣的活動斷層圖比較 186 4.2 海域孕震構造資料庫之應用方向 187 4.2.1 陸域地震危害度計算 187 4.2.2 海域建設與資源開發 188 4.2.3 地震的發震構造解釋與海嘯潛勢 189 4.2.4 短時間尺度構造研究——構造監測 189 4.2.5 長時間尺度的構造研究——大地構造解釋與構造滑移速率的分布 190 4.2.6 科學資料整合與促進國際間的合作 191 4.3 海域孕震構造資料庫的不確定性與可能優化方向 191 4.3.1 海域構造之幾何優化 191 4.3.1.1 海床上位置與長度精度提升 191 4.3.1.2 構造地下幾何重建與優化 193 4.3.1.3 地形起伏影響構造的幾何估計 196 4.3.1.4 震測剖面之時深轉換優化 196 4.3.2 海域構造之滑移速率優化 198 4.3.2.1 滑移速率計算過程給予固定誤差之合理性 199 4.3.2.2 評估各種計算方式的最大值與最小值 199 4.3.2.3 討論速率計算方式所代表的時間尺度 199 4.3.2.4 討論斜移運動的可能性與對滑移速率的影響 201 4.3.2.5 滑移速率隨斷層不同段的空間變化與其代表性 201 4.3.2.6 評估海域構造的無震潛移運動 202 4.3.2.7 滑移速率隨時間的改變對計算結果的影響 204 4.4 海域孕震構造資料庫的其他科學研究議題 205 4.4.1 參數之間的相關性討論 205 4.4.2 探討構造活動所伴隨的地形與地層紀錄 206 4.4.3 構造之海床上方水體對構造活動性的影響 207 4.4.4 延伸討論不同海域的沉積速率空間分布 208 4.4.5 不同地質區的地質討論與未來研究方向 209 4.4.5.1 Domain A可以延伸討論的議題 209 4.4.5.2 Domain B可以延伸討論的議題 210 4.4.5.3 Domain C可以延伸討論的議題 210 4.4.5.4 Domain D可以延伸討論的議題 211 4.4.5.5 Domain E可以延伸討論的議題 213 4.4.5.6 Domain F可以延伸討論的議題 214 4.5 第四章之參考資料 215 第五章、結論 225 附錄 227 附錄一、海域孕震構造資料庫之完整參數總表 227 附錄二、臺灣海域海底地形圖與地形名稱 240 | - |
| dc.language.iso | zh_TW | - |
| dc.subject | 地震災害 | zh_TW |
| dc.subject | 海域孕震構造 | zh_TW |
| dc.subject | 地震再現週期 | zh_TW |
| dc.subject | 長期滑移速率 | zh_TW |
| dc.subject | 地震規模 | zh_TW |
| dc.subject | Earthquake magnitude | en |
| dc.subject | Long-term slip rate | en |
| dc.subject | Earthquake recurrence interval | en |
| dc.subject | Seismic hazard | en |
| dc.subject | Offshore seismogenic structures | en |
| dc.title | 臺灣海域孕震構造資料庫 | zh_TW |
| dc.title | Offshore seismogenic structure database in Taiwan | en |
| dc.type | Thesis | - |
| dc.date.schoolyear | 113-2 | - |
| dc.description.degree | 博士 | - |
| dc.contributor.oralexamcommittee | 李建成;王昱;鄧屬予;劉家瑄;馬國鳳;詹忠翰;許雅儒 | zh_TW |
| dc.contributor.oralexamcommittee | Jian-Cheng Lee;Yu Wang;Louis Suh-Yui Teng;Char-Shine Liu;Kuo-Fong Ma;Chung-Han Chan;Ya-Ju Hsu | en |
| dc.subject.keyword | 海域孕震構造,地震災害,地震規模,長期滑移速率,地震再現週期, | zh_TW |
| dc.subject.keyword | Offshore seismogenic structures,Seismic hazard,Earthquake magnitude,Long-term slip rate,Earthquake recurrence interval, | en |
| dc.relation.page | 242 | - |
| dc.identifier.doi | 10.6342/NTU202502461 | - |
| dc.rights.note | 同意授權(全球公開) | - |
| dc.date.accepted | 2025-08-11 | - |
| dc.contributor.author-college | 理學院 | - |
| dc.contributor.author-dept | 地質科學系 | - |
| dc.date.embargo-lift | 2025-08-23 | - |
| 顯示於系所單位： | 地質科學系 | |
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