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完整後設資料紀錄
DC 欄位 | 值 | 語言 |
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dc.contributor.advisor | 胡植慶 | |
dc.contributor.author | Wei Pneg | en |
dc.contributor.author | 彭葦 | zh_TW |
dc.date.accessioned | 2021-06-15T04:01:47Z | - |
dc.date.available | 2011-03-10 | |
dc.date.copyright | 2010-03-10 | |
dc.date.issued | 2010 | |
dc.date.submitted | 2010-02-22 | |
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dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/45026 | - |
dc.description.abstract | Coulomb stress changes had been discussed broadly for understanding the earthquake interaction. Most successful studies were focused on the strike-slip fault system, such as San Andreas fault and north Anatolian fault. Comparing to the strike-slip fault, the complexity of thrust fault system is that the coulomb stress transfer varies with the depth and leads more uncertainty of subsurface structures to calculate the stress transfer. In this study we focused on a creeping Chihshang fault with the creeping rate of about 2-3 cm/yr, which ruptured on December 12, 2003 by Mw 6.5 Chenkung earthquake in eastern Taiwan. We calculated the coulomb stress change with different type of reciver fault in order to figure out how the background seismicity rate along the locked and crreping zone does influence the coulomb stress change. Futhermore, we want to discuss the fault interaction where April 1, 2006 Mw 6.4 Taitung earthquake which stress increasement probably imparted by the 2003 Chenkung earthquake. | en |
dc.description.provenance | Made available in DSpace on 2021-06-15T04:01:47Z (GMT). No. of bitstreams: 1 ntu-99-R96224113-1.pdf: 15796102 bytes, checksum: 0bc01d1027d685fc8947857842d597cd (MD5) Previous issue date: 2010 | en |
dc.description.tableofcontents | Chapter I Motivation
1.1 Introduction …………………………………………………………………1 1.2 RoadMap ……………………………………………………………………3 Chapter II Seismicity Observation 2.1 Seismicity on the LVF ………………………………………………………..6 2.1.2 Fault segmentation …………….................................................................8 2.1.2.1 Mc estimate ………………………………………………………..9 2.1.2.2 Background seismicity rate ………………………………………..9 2.1.2.3 Aftershock duration ……………………………………...……....9 2.2 Change of seismicity rate associated with 2003 event ………………………10 2.2.1 Seismicity in eastern Taiwan ……………………………………......10 2.2.2 Seismicity in the Chihshang area …………………………………...12 Chapter III Coulomb stress transfer model 3.1 Coulomb stress changes ……………………………………………………..30 3.2 Rupture model …………………………………………………………….....30 3.3 Coulomb stress induced by Chengkung earthquake …………………….......31 3.3.1 Results of Coulomb stress change …………………………………..31 Chapter IV rate/state friction model 4.1 rate/state friction model ……………………………………………………...43 4.2 Results of expected seismicity rate …………………………………….........44 Chapter V Discussions 5.1 Earthquake triggering among segments of LVF ………………………….....49 5.2 Triggering order among segments of LVF …………………………………..50 Chapter VI Conclusions 6.1 Conclusions …………………………………………………………….……….54 References ..................................……………………………………………..55 | |
dc.language.iso | en | |
dc.title | 2003年台東成功地震對於縱谷斷層地震活動度之影響 | zh_TW |
dc.title | Influence of seismicity rate change due to Chengkung earthquake along the Longitudinal Valley fault | en |
dc.type | Thesis | |
dc.date.schoolyear | 98-1 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 陳卉瑄,盧佳遇,葉恩肇,戚務正 | |
dc.subject.keyword | 成功地震,庫倫應力,斷層觸發, | zh_TW |
dc.subject.keyword | rate/state model,coulomb stress change,earthquake triggering,Chengkung earthquake, | en |
dc.relation.page | 59 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2010-02-22 | |
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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