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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 莊昀叡 | zh_TW |
| dc.contributor.advisor | Ray Y. Chuang | en |
| dc.contributor.author | 廖冠至 | zh_TW |
| dc.contributor.author | Guan-Zh Liao | en |
| dc.date.accessioned | 2024-08-16T17:12:31Z | - |
| dc.date.available | 2024-12-27 | - |
| dc.date.copyright | 2024-08-16 | - |
| dc.date.issued | 2024 | - |
| dc.date.submitted | 2024-08-12 | - |
| dc.identifier.citation | 大江二郎 (1939)。台中州南投油田調查報告。臺灣總督府殖產局，866。
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Three‐dimensional elastic dislocation modeling of the postseismic response to the 1964 Alaska earthquake. Journal of Geophysical Research: Solid Earth, 107(B4), ECV-1 | - |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/94632 | - |
| dc.description.abstract | 造山帶是地球上地質活動最劇烈和危險的區域之一，其特點是劇烈的構造活動和褶皺逆衝。造山帶的變形前緣作為一個標誌，指示了活動構造運動和非活動構造運動之間的邊界。一般來說，變形前緣也是造山帶最活躍的構造區域，因此迫切需要對該區域進行深入了解和持續監測。
臺灣的造山帶是世界上最活躍的造山帶之一。在臺灣中部，造山帶的前緣構造是彰化斷層。據信彰化斷層最近一次引發的地震發生在1848年，距今已近180年。車籠埔地震的發生使得彰化斷層及臺灣中部造山帶的變形前緣更值得進一步調查。因此，本研究集中於彰化斷層的應變積累和地震潛勢。研究目標是整合各種大地測量數據，包括GNSS、水準測量和InSAR，分析地表速度，並利用地表速度的數據建立模型，以確定斷層的滑移虧損速率。 本研究發現，儘管造山活動向西推進，且彰化斷層處於最前緣，但彰化斷層並未顯示出最高的滑移虧損速率，反而是車籠埔斷層顯示出最高的滑移虧損速率。然而，車籠埔斷層剛剛進入新的地震週期，而彰化斷層已在其當前週期中持續了近180年。一旦彰化斷層引發地震，將對超過300萬人構成重大風險。因此，不能忽視彰化斷層相關的潛在危害。 | zh_TW |
| dc.description.abstract | The orogenic belt is one of the most geologically dynamic and hazardous areas on Earth, characterized by intense tectonic activity and fold-and-thrust belts. The deformation front of the orogenic belts serves as a marker, indicating the boundary between active and inactive tectonic movements. Generally, the deformation front is also the most active structure of orogenic belts, and there is an urgent need for a thorough understanding and continuous monitoring of this region.
The orogenic belt in Taiwan, which is one of the most active orogenic belts in the world. In the central Taiwan, the frontal structure of the orogenic belt is the Changhua fault. The most recent earthquake triggered by the Changhua fault is believed in 1848, nearly 180 years ago. The out-of-sequence Chi-Chi earthquake makes the Changhua fault and the deformation front of the Taiwan central orogenic belt even more worthy of investigation. Therefore, this study focuses on the fault strain accumulation and seismic potential of the Changhua fault. This research aims to integrate varied geodetic data including GNSS, leveling, and InSAR to analyze surface velocities, and conducting a model with geodetic data to determine the slip deficit rates. It is found that despite the westward propagation of orogenic activity and the Changhua fault being at the forefront, the Changhua fault does not show the highest slip deficit rate. Instead, the Chelungpu fault shows the highest slip deficit rate. However, the Chelungpu fault has just started a new seismic cycle, whereas the Changhua fault has been in its current cycle for 176 years, posing a significant risk to over 3,000,000 people in the event of an earthquake triggered by the Changhua fault. Therefore, the potential hazards associated with the Changhua fault should not be ignored. | en |
| dc.description.provenance | Submitted by admin ntu (admin@lib.ntu.edu.tw) on 2024-08-16T17:12:31Z No. of bitstreams: 0 | en |
| dc.description.provenance | Made available in DSpace on 2024-08-16T17:12:31Z (GMT). No. of bitstreams: 0 | en |
| dc.description.tableofcontents | 論文口試委員審定書 i
誌謝 ii 摘要 iii Abstract iv Table of Contents vi List of Figures ix List of Tables xii Chapter 1 Research motivation and purpose 1 1.1 Research motivation 1 1.2 Research purposes 5 Chapter 2 Literature review 6 2.1 The orogenic belt and deformation front in the world 6 2.2 The orogenic belt and deformation front in Taiwan 10 2.2.1 The tectonic process in Taiwan 10 2.2.2 The tectonic process and geological setting in the central Taiwan 11 2.3 Synthetic aperture radar 12 2.4 Numeric model 16 2.5.1 Two-dimensional model 17 2.5.2 Three-dimensional model 19 Chapter 3 Study area 22 3.1 Study area 22 3.2 The faults in the central Taiwan 24 3.2.1 Changhua fault 24 3.2.2 Chelungpu fault 30 3.2.3 Tamaopu-Shuangtung fault 32 3.2.4 Sanyi fault 32 3.2.5 Tuntzuchiao fault 34 3.2.6 Chushiang fault 35 3.3 Geodetic slip deficit rates of faults in the central Taiwan 37 3.4 The geometry of faults 39 Chapter 4 Data and methods 43 4.1 Study data 43 4.1.1 GNSS 43 4.1.2 Leveling 44 4.1.3 SAR 44 4.2 Methods 45 4.2.1 Research workflow 45 4.2.2 Process GNSS and leveling data 47 4.2.3 InSAR time series and velocity 54 4.2.4 Modelling the faults in the central Taiwan 59 4.2.5 The assessment of the moment magnitude of the faults 68 Chapter 5 Results 69 5.1 Two-dimensional dislocation model 69 5.1.1 Testing the lower and upper detachment 69 5.1.2 The southern profile of 2-D model 74 5.1.3 The northern profile of 2-D model 75 5.2 Three-dimensional dislocation model 80 5.2.1 The results of 3-D model 80 5.2.2 3-D model testing 88 5.3 The moment magnitude of the faults 96 Chapter 6 Discussions 99 6.1 Comparison with results of other studies 99 6.1.1 The slip deficit rates from the 3-D model results 99 6.1.2 The moment magnitude of the faults 100 6.2 Comprehensive assessment of slip deficit rates in three scenarios 101 6.3 The impact of the Changhua fault’s slip deficit rate 105 6.3.1 The impact to faults structures 105 6.3.2 The impact to earthquake hazards 106 Chapter 7 Conclusions 108 Reference 111 Appendix 132 Appendix A: Velocity of GNSS stations in horizontal direction 132 Appendix B: Velocity of GNSS and leveling in vertical direction 145 Appendix C: Velocity of InSAR in line-of-sight direction 162 Appendix D: Fitting result of GNSS and leveling data 181 Appendix D1: Continuous-mode GNSS 181 Appendix D2: Campaign-mode GNSS 206 Appendix D3: Leveling 234 Appendix E: Posterior distribution of 2-D model results 254 Appendix F: The 3-D model results 257 | - |
| dc.language.iso | en | - |
| dc.title | 臺灣造山帶西部前緣在震間期的變形與應變累積 | zh_TW |
| dc.title | Interseismic Deformation and Strain Accumulation Along Western Front of Taiwan Orogen | en |
| dc.type | Thesis | - |
| dc.date.schoolyear | 112-2 | - |
| dc.description.degree | 碩士 | - |
| dc.contributor.oralexamcommittee | 景國恩;黃文正;郭昱廷;鐘令和 | zh_TW |
| dc.contributor.oralexamcommittee | Kuo-En Ching;Wen-Jeng Huang;Yu-Ting Kuo;Ling-Ho Chung | en |
| dc.subject.keyword | 彰化斷層,造山帶變形前緣,數值模型,震間期變形,地震潛勢, | zh_TW |
| dc.subject.keyword | The Changhua fault,Deformation front,Numeric model,Interseismic deformation,Seismic Potential, | en |
| dc.relation.page | 264 | - |
| dc.identifier.doi | 10.6342/NTU202403926 | - |
| dc.rights.note | 同意授權(全球公開) | - |
| dc.date.accepted | 2024-08-13 | - |
| dc.contributor.author-college | 理學院 | - |
| dc.contributor.author-dept | 地理環境資源學系 | - |
| 顯示於系所單位： | 地理環境資源學系 | |
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