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| ???org.dspace.app.webui.jsptag.ItemTag.dcfield??? | Value | Language |
|---|---|---|
| dc.contributor.advisor | 王昱 | zh_TW |
| dc.contributor.advisor | Yu Wang | en |
| dc.contributor.author | 程卉珊 | zh_TW |
| dc.contributor.author | Wai San Cheng | en |
| dc.date.accessioned | 2023-09-22T17:37:37Z | - |
| dc.date.available | 2023-11-09 | - |
| dc.date.copyright | 2023-09-22 | - |
| dc.date.issued | 2023 | - |
| dc.date.submitted | 2023-08-12 | - |
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(1996). 神奈川の活断層. 神奈川県温泉地学研究所報告, 27(1), 23-63, 図巻末 24 枚. | - |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/90150 | - |
| dc.description.abstract | 多重斷層破裂為兩條或以上斷層同時破裂的情境，造成比區域裡所有斷層單一破裂更大的地震規模。儘管歷史地震紀錄中早有多重斷層破裂的出現，過去對於其發生的控制條件仍未有完整的討論，且現有多數的地震危害度評估模型裡亦未充分考慮此破裂情境。為改善臺灣地震模型裡對於多重斷層破裂的地震危害度分析，本研究聚焦於分析斷層間的空間關係，透過收集世界各地的多重斷層破裂地震事件資料，從已知的地震事件中找出多重斷層破裂的可能行為模式，並將其應用到臺灣地震模型裡的孕震構造，以找出臺灣本島可能產生的多重斷層破裂情境，從而估算它們的規模以及再現週期。
本研究收集的資料顯示多重斷層的同震破裂會受控於斷層的滑移類型、三維斷層面間的距離以及其相對排列關係。從收集的資料可發現斷層同震破裂能跳躍至五公里以外的斷層後繼續其破裂行為，且逆斷層可以影響的距離比走滑斷層為大，此現象可能歸因於逆斷層傾角較走滑斷層緩。此外，結果顯示走滑斷層間和逆斷層間只有在走向差異介於0-40度與80-90度之間才能發生多重斷層破裂。 依上述的條件，本研究基於臺灣地震模型裡現有的孕震構造資料庫列出臺灣可能出現的多重斷層破裂情境，並在考慮多重斷層破裂情境後，計算臺灣本島孕震構造的發震地震規模與頻率之間的關係。本研究結果顯示多重斷層破裂可能會對長時間尺度的地震危害度評估造成一定的影響，此類型破裂除了會造成比只考慮單一斷層破裂更大規模的地震外，孕震構造的破裂再現週期也可能在考慮多重斷層破裂情境後變長。因此在未來的地震危害度分析中，應考量斷層面間的距離以及其相對排列關係對模型所產生的影響。 | zh_TW |
| dc.description.abstract | Multi-fault rupture earthquake is an event which involves near-simultaneous or cascading rupture on two or more faults in one single earthquake, and results in a larger magnitude that exceeds the capable magnitude of any single seismogenic fault involved in the earthquake. Although the unexpected earthquake magnitude may have high impact on the seismic hazard assessment, most seismic hazard models include only single-fault rupture scenarios, and the geological condition to promote multi-fault rupture in single earthquake is yet well-studied. Hence, we collected worldwide multi-fault rupture cases and built up a database focusing on spatial relationships between contributing faults and their physical characteristics (e.g., fault types, geometries), in order to find out the possible multi-fault rupture scenario in Taiwan.
In terms of the structural discontinuities that may arrest the coseismic ruptures, our data suggest the “5-km” surface fault separation may not act as the termini to stop all the coseismic ruptures. For reverse faulting cases, the coseismic ruptures could jump further on the surface, compared to strike-slip faulting cases. This difference is likely resulted from the three-dimensional geometries between the adjacent faults since reverse faults tend to have gentler geometries at depth than the strike-slip faults. Moreover, the fault alignment also affects the jumping behaviour. For both strike-slip faults and reverse faults, jumps would not occur within the strike variation between 40-80°. We provide possible multi-fault rupture sets from the empirical observations, their corresponding capable magnitude and recurrence interval, and present a magnitude-frequency relationship under the architecture of the seismogenic structures in the Taiwan Earthquake Model. Since the multi-fault rupture would result in larger magnitude events with lower frequency than the ordinary fault ruptures, we suggest the future analysis need to consider its impact on the seismic hazard assessment. | en |
| dc.description.provenance | Submitted by admin ntu (admin@lib.ntu.edu.tw) on 2023-09-22T17:37:37Z No. of bitstreams: 0 | en |
| dc.description.provenance | Made available in DSpace on 2023-09-22T17:37:37Z (GMT). No. of bitstreams: 0 | en |
| dc.description.tableofcontents | 口試委員審定書 i
誌謝 ii 中文摘要 iii Abstract iv Table of contents vi List of Figures ix List of Tables xv Chapter 1 Introduction 1 Chapter 2 Methods 7 2.1 Data collection 7 2.2 Magnitude estimation 12 2.3 Spatial relation analysis 15 2.4 Application to Taiwan Earthquake Model 16 Chapter 3 Review of previous studies 20 3.1 Magnitude 20 3.1.1 Observed magnitude estimated by seismic moment 20 3.1.2 Empirical relationships 22 3.2 Spatial relations between faults 25 Chapter 4 Global multi-fault rupture scenarios 33 4.1 Case study of multi-fault ruptures 39 4.1.1 Worldwide multi-fault rupture cases 39 4.1.2 Observations from the previous database 70 4.1.3 Multi-fault ruptures in Taiwan 71 4.2 Magnitude 75 4.3 Fault types 76 4.4 Spatial relations 77 4.4.1 Alignment 77 4.4.2 Spacing 78 4.4.3 Summary of spatial relations 80 Chapter 5 Application to Taiwan Earthquake Model 82 5.1 Fault alignment 82 5.2 Fault spacing 83 5.3 Multi-fault rupture sets 84 5.3.1 Pairs 84 5.3.2 Combinations 86 5.4 The recurrence interval of the rupture sets 90 5.5 Magnitude-frequency relations 93 Chapter 6 Discussion 96 6.1 Limitations 96 6.1.1 Spatial relations 96 6.1.2 Magnitude estimation 96 6.1.3 Secondary fault and sympathetic ruptures 97 6.2 Compare to other models including multi-fault rupture 97 6.2.1 The United States 97 6.2.2 New Zealand 99 6.2.3 Taiwan 102 6.3 Magnitude 110 6.3.1 Segmentation 110 6.3.2 Long-tail residual 111 6.4 Frequency 112 6.4.1 Recurrence interval estimation 112 6.4.2 Magnitude-frequency distribution 114 6.4.3 Time-dependent 114 6.5 1935-like earthquake 116 6.5.1 Regional fault 116 6.5.2 Multi-fault rupture frequency 118 6.6 Extreme multi-fault rupture scenario 119 6.6.1 Possibility of extreme scenario 119 6.6.2 Recurrence interval 120 6.7 Impacts on hazard level assessment 121 Chapter 7 Conclusions 122 References 123 Appendix 138 | - |
| dc.language.iso | en | - |
| dc.subject | 臺灣地震模型 | zh_TW |
| dc.subject | 地震危害度 | zh_TW |
| dc.subject | 地震情境 | zh_TW |
| dc.subject | 多重斷層破裂 | zh_TW |
| dc.subject | Multi-fault rupture | en |
| dc.subject | earthquake scenario | en |
| dc.subject | seismic hazard assessment | en |
| dc.subject | Taiwan Earthquake Model (TEM) | en |
| dc.title | 臺灣多重斷層破裂情境初探 | zh_TW |
| dc.title | Applying multi-fault rupture scenario to Taiwan Earthquake Model | en |
| dc.type | Thesis | - |
| dc.date.schoolyear | 111-2 | - |
| dc.description.degree | 碩士 | - |
| dc.contributor.oralexamcommittee | 李錫堤;馬國鳳;徐澔德;高嘉謙 | zh_TW |
| dc.contributor.oralexamcommittee | Chyi-Tyi Li;Kuo-Fong Ma;J Bruce H Shyu;Jia-Cian Gao | en |
| dc.subject.keyword | 多重斷層破裂,地震情境,地震危害度,臺灣地震模型, | zh_TW |
| dc.subject.keyword | Multi-fault rupture,earthquake scenario,seismic hazard assessment,Taiwan Earthquake Model (TEM), | en |
| dc.relation.page | 150 | - |
| dc.identifier.doi | 10.6342/NTU202302553 | - |
| dc.rights.note | 同意授權(限校園內公開) | - |
| dc.date.accepted | 2023-08-13 | - |
| dc.contributor.author-college | 理學院 | - |
| dc.contributor.author-dept | 地質科學系 | - |
| dc.date.embargo-lift | 2024-08-15 | - |
| Appears in Collections: | 地質科學系 | |
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| ntu-111-2.pdf Access limited in NTU ip range | 32.87 MB | Adobe PDF |
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