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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 | Chia-Hua Lin | en |
dc.contributor.author | 林珈樺 | zh_TW |
dc.date.accessioned | 2021-05-13T08:37:03Z | - |
dc.date.available | 2017-08-24 | |
dc.date.available | 2021-05-13T08:37:03Z | - |
dc.date.copyright | 2016-08-24 | |
dc.date.issued | 2016 | |
dc.date.submitted | 2016-08-02 | |
dc.identifier.citation | Abe, K. (1981). Magnitudes of large shallow earthquakes from 1904 to 1980. Phys. Earth Planet. Inter., 27(1), 72-92.
Aki, K. (1967). Scaling law of seismic spectrum. J. Geophys. Res., 72(4), 1217-1231. Andrews, D. J. (1980). A stochastic fault model, 1, Static case. J. Geophys. Res., 85, 3867–3877, 1980a. Andrews, D. J. (1981). A stochastic fault model: 2. Time‐dependent case. J. Geophys. Res.: Solid Earth, 86(B11), 10821-10834. Angelier, J., Lee, J. C., Chu, H. T., Hu, J. C., Lu, C. Y., Chan, Y. C., Lin, T. J., Font, Y., Deffontaines, B., & Yi-Ben, T. (2001). Le séisme de Chichi (1999) et sa place dans l'orogène de Taiwan. Comptes Rendus de l'Académie des Sciences-Series IIA-Earth Planet. Sci., 333(1), 5-21. Bonilla, M. G. (1977). Summary of Quaternary faulting and elevation changes in Taiwan. Mem. Geol. Soc. China, 2, 43-55. Chaljub, E., Capdeville, Y., & Vilotte, J. P. (2003). Solving elastodynamics in a fluid–solid heterogeneous sphere: a parallel spectral element approximation on non-conforming grids. J. Comput. Phys., 187(2), 457-491. Cheng, S. N., Yeh, Y. T., & Yu, M. S. (1996). The 1951 Taitung earthquake in Taiwan. J. Geol. Soc. China Taiwan, 39, 267-286. Chung, L. H., Chen, Y. G., Wu, Y. M., Shyu, J. B. H., Kuo, Y. T., & Lin, Y. N. N. (2008). Seismogenic faults along the major suture of the plate boundary deduced by dislocation modeling of coseismic displacements of the 1951 M7. 3 Hualien–Taitung earthquake sequence in eastern Taiwan. Earth Planet. Sci. Lett., 269(3), 416-426. Frankel, A. (1991). High-frequency spectral falloff of earthquakes, fractal dimension of complex rupture, b value, and the scaling of strength on faults. J. Geophys. Res, 96, 6291-6302. Geist, E. L. (2002). Complex earthquake rupture and local tsunamis. J. Geophys. Res.: Solid Earth, 107(B5). doi:10.1029/2000JB000139 Gutenberg, B. and Richter, C. F. (1954). Magnitude and energy of earthquakes. Annali di Geofisica, 9, 1-15. Hanks, T. C. (1979). b values and ω− γ seismic source models: Implications for tectonic stress variations along active crustal fault zones and the estimation of high‐ frequency strong ground motion. J. Geophys. Res.: Solid Earth, 84(B5), 2235-2242. Hanks, T. C. and Kanamori, H. (1979). A moment magnitude scale, J. Geophys. Res. 84, 2348- 2350. Hartzell, S. H., & Heaton, T. H. (1983). Inversion of strong ground motion and teleseismic waveform data for the fault rupture history of the 1979 Imperial Valley, California, earthquake. Bulletin of the Seismological Society of America, 73(6A), 1553-1583. Herrero, A., & Bernard, P. (1994). A kinematic self-similar rupture process for earthquakes. Bull. Seismol. Soc. Am., 84(4), 1216-1228. Hsu, T. L. (1956). Geology of the Coastal Range, eastern Taiwan. Bull. Geol. Surv. Taiwan, 8, 39-63. Hsu, T. L. (1962). Recent faulting in the Longitudinal Valley of eastern Taiwan. Geol. Soc. China Mem. 1, 95-102. Hsu, T. L., & Chang, H. C. (1979). Quaternary faulting in Taiwan. Mem. Geol. Soc. China, 3(1), 979. Hu, J. C., Cheng, L. W., Chen, H. Y., Wu, Y. M., Lee, J. C., Chen, Y. G., Lin, K. C., Rau, R. J., Kuochen, H., Yu, S. B., & Angelier, J. (2007). Coseismic deformation revealed by inversion of strong motion and GPS data: the 2003 Chengkung earthquake in eastern Taiwan. Geophys. J. Int., 169(2), 667-674. Huang, H. H., Wu, Y. M., Song, X., Chang, C. H., Lee, S. J., Chang, T. M., & Hsieh, H. H. (2014). Joint Vp and Vs tomography of Taiwan: Implications for subduction-collision orogeny. Earth Planet. Sci. Lett., 392, 177-191. doi:10.1016/j.epsl.2014.02.026 Kanamori, H. (1977). The energy release in great earthquakes. J. Geophys. Res., 82(20), 2981-2987. Komatitsch, D., & Tromp, J. (2002a). Spectral-element simulations of global seismic wave propagation—I. Validation. Geophys. J. Int., 149(2), 390-412. doi:10.1046/j.1365-246X.2002.01653.x Komatitsch, D., & Tromp, J. (2002b). Spectral-element simulations of global seismic wave propagation—II. Three-dimensional models, oceans, rotation and self-gravitation. Geophys. J. Int., 150(1), 303-318. doi:10.1046/j.1365-246X.2002.01716.x Komatitsch, D., Liu, Q., Tromp, J., Süss, P., Stidham, C., & Shaw, J. H. (2004). Simulations of ground motion in the Los Angeles basin based upon the spectral-element method. Bull. Seismol. Soc. Amer., 94(1), 187-206. Kuochen, H., Wen, K. L., Hsieh, H. H., Lin, C. M., Chang, T. M., & Kuo, K. W. (2012). Site classification and Vs30 estimation of free-field TSMIP stations using the logging data of EGDT. Eng. Geol., 129, 68-75. Lavallée, D., & Archuleta, R. J. (2003). Stochastic modeling of slip spatial complexities for the 1979 Imperial Valley, California, earthquake. Geophys. Res. Lett., 30(5). Lavallée, D., & Archuleta, R. J. (2005). Coupling of the random properties of the source and the ground motion for the 1999 Chi Chi earthquake. Geophys. Res. Lett., 32(8). Lavallée, D., Liu, P., & Archuleta, R. J. (2006). Stochastic model of heterogeneity in earthquake slip spatial distributions. Geophys. J. Int., 165(2), 622-640. Lee, W. H. K., Wu, F. T., & Wang, S. C. (1978). A catalog of instrumentally determined earthquakes in China (magnitude≧ 6) compiled from various sources. Bull. Seismol. Soc. Amer., 68(2), 383-398. Lee, S. J., Chen, H. W., Liu, Q., Komatitsch, D., Huang, B. S., & Tromp, J. (2008). Three-dimensional simulations of seismic-wave propagation in the Taipei basin with realistic topography based upon the spectral-element method. Bull. Seismol. Soc. Amer., 98(1), 253-264. Lee, S. J., Chan, Y. C., Komatitsch, D., Huang, B. S., & Tromp, J. (2009). Effects of realistic surface topography on seismic ground motion in the Yangminshan region of Taiwan based upon the spectral-element method and LiDAR DTM. Bull. Seismol. Soc. Amer., 99(2A), 681-693. Lee, Y. H., Chen, G. T., Rau, R. J., & Ching, K. E. (2008). Coseismic displacement and tectonic implication of 1951 Longitudinal Valley earthquake sequence, eastern Taiwan. J. Geophys. Res.: Solid Earth, 113(B4). Lin, P. S., Hsie, P. S., Lee, Y. R., Cheng, C. T., & Shao, K. S. (2012). The research of probabilistic seismic hazard analysis and geological survey of nuclear power plant: construction of ground motion prediction equation for response spectra: commission report of the Institute of Nuclear Energy Research, Atomic Energy Council, Executive Yuan (in Chinese). Mandelbrot, B. B., & Van Ness, J. W. (1968). Fractional Brownian motions, fractional noises and applications. SIAM review, 10(4), 422-437. Mandelbrot, B. B. (1977). Fractals, form and chance, and dimension. (p. 365). San Francisco: WH Freeman. Mandelbrot, B. B. (1982). The Fractal Geometry of Nature, Freeman, New York. Okada, Y. (1985). Surface deformation due to shear and tensile faults in a half-space. Bull. Seismol. Soc. Amer., 75(4), 1135-1154. Okada, Y. (1992). Internal deformation due to shear and tensile faults in a half-space. Bull. Seismol. Soc. Amer., 82(2), 1018-1040. Peitgen, H. O., & Saupe, D. (1988). The Science of Fractal Images, 1988. Peitgen, H. O. (1992). H. J urgens, and D. Saupe. Fractals for the Classroom. Part One. Introduction to Fractals and Chaos. Sato, R., & Matsu'ura, M. (1974). Strains and tilts on the surface of a semi-infinite medium. J. Phys. Earth, 22(2), 213-221. Shyu, J. B. H., Sieh, K., Chen, Y. G., & Liu, C. S. (2005). Neotectonic architecture of Taiwan and its implications for future large earthquakes. J. Geophys. Res.: Solid Earth, 110(B8). doi:10.1029/2004JB003251 Shyu, J. B. H., Sieh, K., Avouac, J. P., Chen, W. S., & Chen, Y. G. (2006). Millennial slip rate of the Longitudinal Valley fault from river terraces: Implications for convergence across the active suture of eastern Taiwan. J. Geophys. Res.: Solid Earth, 111(B8). doi:10.1029/2005JB003971 Shyu, J. B. H., Chung, L. H., Chen, Y. G., Lee, J. C., & Sieh, K. (2007). Re-evaluation of the surface ruptures of the November 1951 earthquake series in eastern Taiwan, and its neotectonic implications. J. Asian Earth Sci., 31(3), 317-331. Shyu, J. B. H., Chuang, Y. R., Chen, Y. L., & Cheng, C. T. (2016). A new on-land seismogenic structure source database by the Taiwan earthquake model (TEM) project for seismic hazard analysis of Taiwan. Terr. Atmos. Ocean. Sci. (accepted). doi:10.3319/TAO.2015.11.27.02(TEM) Steketee, J. A. (1958). On Volterra's dislocations in a semi-infinite elastic medium. Canadian Journal of Physics, 36(2), 192-205. Tsai, C. C. (1997). Slip, stress drop and ground motion of earthquakes: A view from the perspective of fractional Brownian motion. Pure Appl. Geophys., 149(4), 689-706. Wells, D. L., & Coppersmith, K. J. (1994). New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement. Bull. Seismol. Soc. Amer., 84(4), 974-1002. 內政部(1980)中華民國台灣地區三角點成果表。 台灣省三角點成果表(1970)。 台灣省氣象所(1952)中華民國四十年-地震報告。台北,83頁。 石再添、張瑞津、黃朝恩、石慶得、楊貴三、孫林耀明(1983)台灣北部及東部活斷層的地形學研究。國立台灣師範大學地理學研究報告,第九期,21-72頁。 朱傚祖、游明聖(1997) 台東縱谷地震與斷層關係之研究。行政院國家科學委員會專題研究計劃成果報告。NSC-86-2116-M-047-002,133 頁。 何邦碩(1974)花蓮近海海域地球物理初步測勘。海洋彙刊,第12期,第39-47頁。 林啟文、張徽正、盧詩丁、石同生、黃文正(2000)台灣活動斷層概論,第二版,經 濟部中央地質調查所特刊,第十三號,122頁。 姜介中(2009)利用驗潮紀錄估計臺灣沿岸地表垂直運動。國立台灣大學海洋研究所碩博士班碩士論文,共88頁。 孫郁勝(2015)應用隨機滑移模型於台灣地區之機率式海嘯為害度分析,國立中央大學地球科學學系碩博班碩士論文,共121頁。 徐明同(1980)台灣地震目錄(自公元1644年至1979年)。國立台灣大學地震工程研究中心,77頁。 張徽正、林啟文、陳勉銘、盧詩丁(1998)台灣活動斷層概論。經濟部中央地質調查所特刊,第十號。 陳文山、林益正、顏一勤、楊志成、紀權窅、黃能偉、林啟文、林偉雄、劉彥求、林燕慧、石同生、盧詩丁(2008)從古地震研究與 GPS 資料探討縱谷斷層的分段意義。經濟部中央地質調查所特刊, (20), 165-191。 陳文山、俞何興、俞震甫、鍾孫霖、林正洪、林啟文、游能悌、吳逸民、王國龍(2016)台灣地質概論。社團法人中華民國地質學會出版,共204頁。 陳培源(2006)台灣地質。台灣省應用地質技師公會出版,共484頁。 楊貴三(1986)台灣活斷層的地形學研究-特論活斷層與地形面的關係。私立中國文 化大學地學研究所博士論文,共178頁。 楊蔭清(1953)四十一年來之花蓮地震。花蓮文獻,創刊號,第67-71頁。 溫國樑、吳子修、陳俊德、黃雋彥(2012)臺灣地區地震潛勢評估之研究(II),交通部中央氣象局委託研究計畫期末成果報告,6-10頁。 鄭世楠、余騰鐸、葉永田、張建興(1997)1951年花蓮-台東地震系列之重定位。紀念台灣地區氣象測報一百年-天氣分析與預報研討會海象與地震論文彙編,690-699頁。 鄭世楠、王子賓、林祖慰、江嘉豪(2011)台灣地區地震目錄的建置(II)。中央氣象局地震技術報告彙編,第57卷,483-501。 | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/3813 | - |
dc.description.abstract | 台灣東部花東縱谷被視為歐亞板塊與菲律賓海板塊的縫合帶,而花東縱谷斷層系統由北到南貫穿整個花東縱谷,屬於台灣地區活躍的斷層系統。在1951年10月到12月的期間,四個規模大於6.9的地震陸續發生在花蓮外海及花東縱谷斷層沿線,且記錄到數千個餘震,餘震震源隨時間由北往南傳遞,此地震事件被稱為「花東縱谷地震序列」,當時在縱谷沿線觀察到總共約90公里的同震地表破裂。本研究針對此的震序列做進一步的探討,以期了解縱谷斷層的滑移特性。本文主要分為兩大部份,第一部分藉由同震地表變形量以非負最小平方法(Non-Negative Least Square, NNLS)對三個不同斷層模型進行反演,求得斷層面上之滑移分布(slip pattern),再透過譜元素法(Spectral Element Method, SEM)計算縱谷斷層分段破裂之地震波傳遞情形,並以模擬之地動分布圖(ShakeMap)和瞬時速度波場(snapshot)之結果,討論其波傳特性;第二部分則以台灣地震模型(Taiwan Earthquake Model)的縱谷斷層幾何作為基礎,考慮地震發生時,斷層滑移分布的不確定與隨機性,透過隨機滑移分布模型(stochastic slip model)建立出十個隨機滑移分布,並模擬縱谷斷層全段破裂在不同震源破裂情境下的地震波傳情形,最後統計不同破裂起始點的平均地動分布與地動極值分布。數值模擬的統計結果顯示,當縱谷斷層發生破裂,花東縱谷地區在各種震源破裂模型中,受到影響最為顯著,地表加速度值大多超過250 cm/s2。若破裂起始點在縱谷斷層中段,全台的地表加速度量值皆會大於80 cm/s2,而儘管距離縱谷斷層較遠的台北盆地、宜蘭平原、台灣南部地區,因受到破裂方向性與場址效應的影響,在特定的破裂分布情形下,會產生超過預期的地表加速度量值。藉由逆推而得的同震滑移分布與隨機滑移分布模型所建立之震源破裂模型的波傳模擬結果,我們可以了解當縱谷斷層發生破裂時,對台灣的影響範圍,並以統計的方式降低斷層面的滑移不確定性對地動分布的影響,期望更接近未來可能的地震情境,作為未來地震防災的參考依據。 | zh_TW |
dc.description.abstract | The Longitudinal Valley (LV) in the eastern Taiwan is considered as the suture zone between the Eurasia Plate and the Philippine Sea Plate. Thousands of earthquakes are occur in this area every year. The Longitudinal Valley Fault (LVF) is a seismically active structure, which is located along the LV. During the time period from October to December in 1951, lots of large earthquakes occurred between Hualien and Taitung area, including four major earthquakes (M > 6.9) and thousands of aftershocks. This earthquake series is known as the Longitudinal Valley Earthquake sequence. Coseismic surface rupture with a total length of approximate 90 km were observed along LV. In order to understand the characteristics of source rupture and resultant strong ground motion, this study is comprised of two different parts. In first part, we reconstructed the source model and strong ground motion time history of this earthquake sequence. Inversion of the coseismic displacement data was first conducted. Based on the inverted slip distribution, we performed 3D forward simulation using the Spectral Element Method. Therefore, the second part of the thesis focuses on ground motion prediction for scenario earthquakes. We performed wave propagation simulation with ten stochastic rupture scenarios and examined the results collectively. The numerical simulation results showed that the PGA larger than 250 cm/s2 distributed along LV in eastern Taiwan in all cases. If the rupture started in the middle of LVF, PGA larger than 80 cm/s2 could be detected in the entire island. In the particular stochastic source rupture models, the PGA might be larger than expected in some places far from LVF due to source radiation and directivity effect, such as Taipei basin, Ilan and southern part of Taiwan. The models we presented in this thesis for both historical and scenario events can serve as reference for future in-depth seismotectonic studies and hazard assessment. | en |
dc.description.provenance | Made available in DSpace on 2021-05-13T08:37:03Z (GMT). No. of bitstreams: 1 ntu-105-R02224105-1.pdf: 4448878 bytes, checksum: 23e83659d38b115ba7309928f91e46ae (MD5) Previous issue date: 2016 | en |
dc.description.tableofcontents | 口試委員會審定書 I
致謝 II 中文摘要 III Abstract V 目錄 VII 圖目錄 IX 表目錄 XI 第一章 緒論 1 1.1 研究動機與目的 1 1.2 研究背景 2 1.2.1 地質背景 2 1.2.2 1951年花東縱谷地震序列 3 1.3 前人研究 4 1.4 內容概述 5 第二章 研究方法 17 2.1 引言 17 2.2 同震位移資料與縱谷斷層模型 18 2.2.1 同震位移資料 18 2.2.2 縱谷斷層模型 19 2.3 震源模型逆推 20 2.3.1 彈性錯位理論(dislocation model) 20 2.3.2 非負最小平方逆推法(Non-Negative Least Square, NNLS) 22 2.4 三維波傳模擬 23 2.4.1 譜元素法(Spectral Element Method, SEM) 23 2.4.2 網格模型之建立 23 2.4.3 地震波傳模擬 24 第三章 重建1951年花東縱谷地震序列震源破裂特性 33 3.1 引言 33 3.2 1951年震源破裂模型逆推與討論 33 3.2.1 同震滑移分布結果 33 3.2.2 震源破裂模型與歷史地震之關聯 35 3.3 1951年地震波傳模擬結果與討論 36 3.3.1 最大地表加速度分布 37 3.3.2 瞬時速度波場 39 第四章 情境地震模擬 52 4.1 引言 52 4.2 縱谷斷層全段破裂之情境 52 4.3 隨機滑移模型與模擬結果統計 53 4.3.1 隨機滑移分布模型 54 4.3.2 地震波傳模擬結果與討論 55 第五章 綜合討論 64 5.1 引言 64 5.2 重建1951年縱谷地震序列 64 5.2.1 地震波傳模擬結果與歷史等震度圖之比較 64 5.2.2 強地動衰減式 66 5.3 縱谷斷層不同破裂情境之討論 67 5.3.1 縱谷斷層分段破裂與全段破裂之比較 68 5.3.2 逆推結果與隨機滑移分布模型模擬結果之比較 68 第六章 結論 77 參考文獻 79 附錄A三角測量資料 86 附錄B 棋盤測試及19個測站與143個測站逆推結果比較 91 附錄C 模型A與模型B地震波傳模擬之瞬時速度波場 96 附錄D 縱谷斷層全段破裂模擬之最大地表加速度分布圖 105 | |
dc.language.iso | zh-TW | |
dc.title | 重建1951年花東縱谷地震序列震源破裂特性與縱谷斷層情境地震模擬之研究 | zh_TW |
dc.title | Source rupture and ground motion simulations of 1951 Longitudinal Valley Earthquake Sequences and future earthquake scenario | en |
dc.type | Thesis | |
dc.date.schoolyear | 104-2 | |
dc.description.degree | 碩士 | |
dc.contributor.coadvisor | 李憲忠 | |
dc.contributor.oralexamcommittee | 許雅儒,鄭世楠,鍾令和 | |
dc.subject.keyword | 1951年花東縱谷地震序列,縱谷斷層,震源逆推,隨機滑移分布模型,三維地震波傳模擬, | zh_TW |
dc.subject.keyword | 1951 Longitudinal Valley earthquake sequence,Longitudinal Valley Fault,source rupture model,stochastic slip model,3D wave propagation simulation, | en |
dc.relation.page | 108 | |
dc.identifier.doi | 10.6342/NTU201601658 | |
dc.rights.note | 同意授權(全球公開) | |
dc.date.accepted | 2016-08-03 | |
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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