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http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/18952完整後設資料紀錄
| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 郭安妮(On-Lei Annie Kwok) | |
| dc.contributor.author | PO-KAI CHEN | en |
| dc.contributor.author | 陳柏凱 | zh_TW |
| dc.date.accessioned | 2021-06-08T01:40:36Z | - |
| dc.date.copyright | 2016-08-26 | |
| dc.date.issued | 2016 | |
| dc.date.submitted | 2016-08-19 | |
| dc.identifier.citation | [1] Abrahamson, N. A., Gregor, N., and Addo, K., 2016. BC hydro ground motion prediction equations for subduction earthquakes, Earthquake Spectra 32. 23-44.
[2] BC Hydro (2012). Probabilistic Seismic Hazard Analysis (PSHA) Model, vols. 1 – 4, BC Hydro Engineering Report E658,Vancouver. [3] Boore, D.M. (2010). Orientation-independent, nongeometric-mean measures of seismic intensity from two horizontal components of motion, Bulletin of the Seismological Society of America, Vol. 100, No. 4, pp 1830-1835 [4] Chen, Y. L. (1995). Three dimensional velocity structure and kinematic analysis in Taiwan area. Master’s Thesis, National Central University, Taiwan, 172 p (in Chinese). [5] Chiou, B. S.-J., and R. R. Youngs (2008). An NGA model for the average horizontal component of peak ground motion and response spectra. Earthquake Spectra 24. 173-215. [6] Kao, H., Chen, W.P. (2000). The Chi-Chi earthquake sequence: active out-of-sequence thrust faulting in Taiwan. Science 288, 2346–2349. [7] Lee, C. T., C. T. Cheng, C. W. Liao, and Y. B. Tsai (2001). Site classification of Taiwan free-field strong-motion stations, Bull. Seismol. Soc. Am. 91, 1283 – 1297. [8] Lin, P. S., and C. T. Lee (2008). Ground-motion attenuation relationships for subduction-zone earthquakes in Northeastern Taiwan. Bulletin of the Seismological Society of America 98, 220–240. [9] Lin, P. S., C. T. Lee, C. T. Cheng, and C. H. Sung (2011). Response spectral attenuation relations for shallow crustal earthquakes in Taiwan. Engineering Geology 121. 150–164. [10] Liu, K. S., and Y. B. Tsai (2005). Attenuation relationships of peak ground acceleration and velocity for crustal earthquake in Taiwan, Bull. Seismol. Soc. Am. 95, 1045 – 1058. [11] Liu, K. S., Y. B. Tsai, and B. S. Lin (2013). A study on fault type and site effect (Vs30) parameters in the attenuation relationships of peak ground acceleration and velocity in Ilan, Taiwan, Bull. Seismol. Soc. Am. 103, 1823 – 1845. [12] Liu, K. S., Y. B.Tsai, C. H. Chang, and P. S. Lin (2014). A study of site effects in Ilan, Taiwan, based on attenuation relationships of spectral acceleration. Bull. Seismol. Soc. Am. 104, 2467-2490. [13] Shen, S. S. (1996). Characteristics of subduction and collision structures in northeastern Taiwan from earthquake mechanisms determined by body waveform inversion. Master’s Thesis, National Central University, Taiwan, 177 pp (in Chinese). [14] Tichelaar, B. W., and L. J. Ruff (1993). Depth of seismic coupling along subduction zones, J. Geophys. Res. 98, 2017 – 2037. [15] Walling, M., Silva, W., and Abrahamson, N., 2008. Nonlinear site amplification factors for constraining the NGA models. Earthquake Spectra 24, 243 – 255 [16] Youngs, R. R., S. J. Chiou, W. J. Silva, and J. R. Humphrey (1997). Strong ground motion attenuation relationships for subduction zone earthquakes, Seism. Res. Lett. 68, 58 – 73. [17] Yu, S. B., H. Y. Chen, and L. C. Kuo (1997). Velocity field of GPS stations in the Taiwan area, Tectonophysics 274, 41 – 59. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/18952 | - |
| dc.description.abstract | 台灣落在菲律賓海板塊與歐亞大陸板塊的交界處，兩板塊以每年約8公分的速度聚合。在台灣的南方，歐亞大陸板塊隱沒到菲律賓海板塊之下；到了台灣北方，則是菲律賓海板塊隱沒到歐亞大陸板塊之下。而在這兩個板塊間相互不斷的擠壓摩擦下，台灣平均每年發生2000次的地震，其震源深度可以從很淺到幾百公里左右的深度。
利用過去的地震紀錄得出的經驗模型我們可以得到強地動預估式(GMPEs)，藉此估計一個測站受到不同地震時的地動強度。而強地動預估式考慮的因素通常有震源(source)、距離(distance)以及場址(site)的效應。本研究利用林柏伸和李錫堤教授在2008提出的強地動預估式，以及Abrahamson等人在2016所提出的強地動預估式做為模型，比較兩者在台灣隱沒帶地震時的偏差關係並進行評估。 | zh_TW |
| dc.description.abstract | Taiwan is located at the boundary of Philippine Sea plate and Eurasian plate. These two plates converge at a rate of 8 centimeters per year (Yu et al., 1997). To the south of Taiwan, Eurasian plate is subducting below the Philippine Sea plate; while to the, northeast, the Philippine Sea plate is subducting below the Eurasian plate. Collision of these two plates leads to significant compression and friction accumulated in the region along the boundary. On average, there are more than 2000 earthquakes annually in Taiwan. The focal depths of these earthquakes can be shallow or occurring at a depth of several hundreds of kilometers.
Ground motion prediction equations (GMPEs), which are empirical models derived from past earthquake recordings, are often used to estimate ground motion intensity level at a site for an earthquake of particular magnitude. GMPEs consist of parameters that would describe the source, path and site effects. In this study, the GMPE models developed by Lin and Lee (2008) and Abrahamson et al. (2016) are reviewed. By using the subduction earthquakes from Taiwan, applicability and biases associated with these models are evaluated. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-08T01:40:36Z (GMT). No. of bitstreams: 1 ntu-105-R03521127-1.pdf: 4940692 bytes, checksum: b3ef6b3e4903f315889d638fc8c38210 (MD5) Previous issue date: 2016 | en |
| dc.description.tableofcontents | 口試委員會審定書 #
誌謝 i 中文摘要 ii ABSTRACT iii CONTENTS iv LIST OF FIGURES vi LIST OF TABLES xi Chapter 1 Introduction 1 1.1 Motivation and Objective of Study 1 1.2 Thesis Organization 2 Chapter 2 Literature Review 3 2.1 Tectonic Environment of Taiwan 3 2.2 Ground Motion Prediction Equations (GMPEs) Model 4 2.2.1 Early Ground Motion Attenuation Model or GMPEs 4 2.3 Review of Strong Motion Prediction Equations for Taiwan 7 Chapter 3 Ground Motion Data of Subduction Earthquakes in Taiwan 16 3.1 Data collection 16 3.1.1 Information on Ground Motion Station 16 3.1.2 Strong Motion Records 16 3.2 GMPE models used in this Study 24 Chapter 4 Residual Analysis Results 30 4.1 Evaluation of Residuals 30 4.2 Analysis of Residuals from GMPE by Lin and Lee (2008) 30 4.2.1 Residuals from all earthquake events 30 4.2.2 Residuals from interface events 30 4.2.3 Residuals from intraslab events 31 4.3 Analysis of Residuals from GMPE by Abrahamson et at. (2016) 41 4.3.1 Residuals from all earthquake events 41 4.3.2 Residuals from interface events 41 4.3.3 Residual from intraslab events 41 4.4 Residual statistics 49 4.4.1 Distribution of Residuals 49 4.4.2 Residuals by Earthquake Event 49 Chapter 5 Conclusion and Recommendation 67 5.1 Conclusion 67 5.2 Recommendation for future studies 67 REFERENCE 69 APPENDIX 73 | |
| dc.language.iso | en | |
| dc.subject | 反應譜 | zh_TW |
| dc.subject | 隱沒帶 | zh_TW |
| dc.subject | 強地動預估式 | zh_TW |
| dc.subject | subduction zone | en |
| dc.subject | ground motion prediction equation | en |
| dc.subject | response spectra | en |
| dc.title | 台灣隱沒帶地震的強地動衰減式之偏差評估 | zh_TW |
| dc.title | Evaluation of Biases in Ground Motion Prediction Equations for Subduction Earthquakes in Taiwan | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 104-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 葛宇甯(Yu-Ning Ge),邱俊翔(Jiunn-Shyang Chiou) | |
| dc.subject.keyword | 隱沒帶,強地動預估式,反應譜, | zh_TW |
| dc.subject.keyword | subduction zone,ground motion prediction equation,response spectra, | en |
| dc.relation.page | 79 | |
| dc.identifier.doi | 10.6342/NTU201603435 | |
| dc.rights.note | 未授權 | |
| dc.date.accepted | 2016-08-21 | |
| dc.contributor.author-college | 工學院 | zh_TW |
| dc.contributor.author-dept | 土木工程學研究所 | zh_TW |
| 顯示於系所單位： | 土木工程學系 | |
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