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http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/91442完整後設資料紀錄
| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 莊昀叡 | zh_TW |
| dc.contributor.advisor | Yun-Ruei Chuang | en |
| dc.contributor.author | 蔣友維 | zh_TW |
| dc.contributor.author | You-Wei Jiang | en |
| dc.date.accessioned | 2024-01-26T16:31:37Z | - |
| dc.date.available | 2024-01-27 | - |
| dc.date.copyright | 2024-01-26 | - |
| dc.date.issued | 2024 | - |
| dc.date.submitted | 2024-01-22 | - |
| dc.identifier.citation | 1067 公厘軌距軌道橋隧檢查養護規範（2003）。交通部，民國 92 年。
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Present-day crustal motion along the Longitudinal Valley Fault, eastern Taiwan. Tectonophysics, 333(1-2), 199-217. | - |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/91442 | - |
| dc.description.abstract | 台灣造山帶位於弧陸碰撞帶，由菲律賓海板塊的呂宋島弧向西以及歐亞板塊向東斜向碰撞在此造成褶皺逆衝帶，形成一系列南北走向的活動斷層。台灣西南部位於褶皺逆衝帶的前緣位置，並且在 2016 年受到美濃地震的影響，使得此區域的斷層活動變得更加不穩定。台灣西南部境內包含台南與高雄都會區，有台灣高鐵公司（以下稱「高鐵」）鐵路、台灣鐵路管理局（以下稱「台鐵」）鐵道以及國道高速公路通過。近年來也陸續設立了多個產業園區以及數條預計建設的交通設施。而先前的研究透過 GNSS 等測地資料發現，在台灣西南部跨斷層兩側有明顯速度落差，支持現今的地表斷層潛移的現象，跨越活動斷層的交通設施與產業園區就可能受到跨斷層速度差受到影響甚至是破壞。因此為了要獲取台灣西南部的速度場，本研究使用歐洲太空總署（European Space Agency, ESA）的 Sentinel-1A 的SAR 影像，在升軌方向使用 146 幅影像，觀測時間從 2016 年 3 月到 2021 年 11月；在降軌方向使用 130 張影像，觀測時間從 2016 年 5 月到 2022 年 2 月。我們使用永久散射體雷達干涉（Persistent Scatterer InSAR, PSInSAR）的 StaMPS/MTI(Stanford Method for Persistent Scatterers/ Multi-Temporal InSAR)演算法，針對目標區域的活動斷層造成的地表變形以及關鍵基礎設施的變形製作時間序列觀測資料。本研究結果顯示在中央地質調查所的後甲里斷層兩側的速度落差在垂直方向上約為 3~6 毫米/年，呈現由北向南遞增的情形；在車瓜林斷層兩側的速度落差在東西方向上約為 4~8 毫米/年；而在台灣地震模型（Taiwan Earthquake Model, TEM）右昌斷層兩側的速度落差在東西方向上約為 5 毫米/年。並在斷層兩側的位移在時間序列上也可以明顯見到相反的變形趨勢，足見這些斷層可能存在斷層潛移的情形。針對關鍵基礎設施高鐵沿線以及台鐵沿線，在部分跨越活動斷層路段兩側也同樣取得時間序列變形趨勢。在高鐵沿線變形最大處即跨越地調所車瓜林斷層處，達到橫向水平位移的容許規範約為 7 年；而台鐵沿線變形最大處即跨越右昌斷層處，達到縱向水平位移的容許規範約為 10 年；國道 7 號等規劃路線，其沿線跨越斷層處的變形量也將在 10 年內達到 H 等級。產業園區類的基礎設施，雖然不像交通系統容易受到地表變形立即的危害，但部分園區接近有潛移活動的活動斷層敏感區，亦需要更多的觀測來留意。本研究比對前人針對斷層特性的研究，在斷層處的變形趨勢皆符合，並且也與前人利用測地技術測得之可能存在斷層潛移之結果符合。因此，本研究建議未來在台灣西南部地區活動斷層附近設置之關鍵基礎設施能更加留意活動斷層活動性帶來的影響。 | zh_TW |
| dc.description.abstract | The Taiwan mountain belt features many active faults resulting from the oblique collision between the two tectonics (Suppe, 1984). Geodetic observations in previous studies show that sharp velocity gradients across active faults in SW Taiwan, suggesting the presence of surface fault creep. Synthetic Aperture Radar (SAR), which is an active system that transmits microwaves to surface targets and receives backscatters from them, has a lot of benefits such as cloudy-free, day-and-night monitoring, and all-weather detection. In this study, SAR images derived from the ESA’s Sentinel-1A satellite were used. 166 SAR images from March 9, 2016, to November 14, 2021, in the ascending direction (ASC) and 133 SAR images from May 10, 2016, to February 8, 2022, in the descending direction (DES), which cover the whole study area are used to detect surface deformation. I use the PSInSAR algorithm of StaMPS/MTI to create time series data of surface deformation and target deformation of the critical infrastructure. At the maximum deformation place along the Taiwan High Speed Rail Corporation (THSR) railroad, which crosses the Chekualin fault, will reach the allowable level for lateral horizontal displacement within 7 years. Along the Taiwan Railway Administration MOTC. (TR) railroad, at the maximum deformation place, which crosses the Youchang fault, will reach the allowable level for longitudinal horizontal displacement within 10 years. For planned routes like National Highway No. 7, the deformation at locations where active fault crosses is expected to reach Class H within 10 years. Although infrastructure in industrial parks is not affected by surface deformations immediately, some parks are close to sensitive areas with potential active fault creep, requiring more monitoring. This study's findings are consistent with previous research on fault characteristics and are in line with the results obtained through geodetic techniques indicating potential fault creep. Therefore, it is recommended that future critical infrastructure near active fault zones in southwestern Taiwan should pay more attention to the impact of fault creep. | en |
| dc.description.provenance | Submitted by admin ntu (admin@lib.ntu.edu.tw) on 2024-01-26T16:31:37Z No. of bitstreams: 0 | en |
| dc.description.provenance | Made available in DSpace on 2024-01-26T16:31:37Z (GMT). No. of bitstreams: 0 | en |
| dc.description.tableofcontents | 口試委員審定書 i
誌謝 ii 摘要 iii Abstracts v List of tables x List of Figures xi Chapter 1 Introduction 1 1.1 Motivations 1 1.2 Purposes 4 1.3 Study area 5 Chapter 2 Literature review 11 2.1 Geology setting 11 2.1.1 Stratigraphy of SW Taiwan 13 2.1.2 Active faults 16 2.2 Region surface deformation in SW Taiwan 21 2.3 Critical infrastructure monitoring in Taiwan 23 Chapter 3 Method 28 3.1 Radar (RAdio Detection And Ranging) 28 3.2 Side-Looking Airborne Radar (SLAR) and Synthetic Aperture Radar (SAR) 29 3.2.1 SLAR 29 3.2.2 SAR 30 3.3 InSAR and DInSAR 31 3.4 Persistent Scatterers Interferometry (PSInSAR) 32 3.4.1 Produce interferogram 33 3.4.2 Phase stability analysis 33 3.5 Data collection 39 Chapter 4 Result 43 4.1 PS velocity fields in LOS direction 43 4.2 Correct PSInSAR by GNSS velocity 47 4.3 Decomposition 53 4.4 Comparison PS and leveling 56 Chapter 5 Discussion 60 5.1 Active fault motion 60 5.2 Infrastructure deformation 68 5.2.1 Transportation systems 68 5.2.2 Industrial parks 88 Chapter 6 Conclusions 95 Reference 96 Supplementary 1: Interferograms 104 | - |
| dc.language.iso | en | - |
| dc.title | 利用 PSInSAR 監測臺灣西南部關鍵基礎設施相關之地表變形 | zh_TW |
| dc.title | Using PSInSAR to monitor the surface deformation of critical infrastructure in SW Taiwan | en |
| dc.type | Thesis | - |
| dc.date.schoolyear | 112-1 | - |
| dc.description.degree | 碩士 | - |
| dc.contributor.oralexamcommittee | 景國恩;張午龍;陳松春;曾國欣 | zh_TW |
| dc.contributor.oralexamcommittee | Kuo-En Ching;Wu-Lung Chang;Song-Chuen Chen;Kuo-Hsin Tseng | en |
| dc.subject.keyword | 永久散射體差分干涉技術,關鍵基礎設施,台灣西南部,活動斷層, | zh_TW |
| dc.subject.keyword | PSInSAR,Critical infrastructures,SW Taiwan,Active faults, | en |
| dc.relation.page | 119 | - |
| dc.identifier.doi | 10.6342/NTU202400130 | - |
| dc.rights.note | 同意授權(全球公開) | - |
| dc.date.accepted | 2024-01-23 | - |
| 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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