請用此 Handle URI 來引用此文件：
http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/30012完整後設資料紀錄
| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 吳逸民(Yih-Min Wu) | |
| dc.contributor.author | Hsin-Hua Huang | en |
| dc.contributor.author | 黃信樺 | zh_TW |
| dc.date.accessioned | 2021-06-13T01:30:32Z | - |
| dc.date.available | 2007-07-25 | |
| dc.date.copyright | 2007-07-25 | |
| dc.date.issued | 2007 | |
| dc.date.submitted | 2007-07-17 | |
| dc.identifier.citation | Angelier, J. (1984). Tectonic analysis of fault slip data sets. J. Geophys. Res., 89, 5835-5848.
Biq, C. (1981), Collision, Taiwan-style. Mem. Geol. Soc. China, 4, 91-102. Blanchet, R., J.-F. Stephan, C. Rangin, P. Cabezas, D. Baladad, P. Bouysse, P.-P. Chen, P. Chotin, J.-Y. Collot, J. Daniel, J.-M. Drouhot, B. Marsset, B. Pelletier, M. Richard, and M. Tardy (1988). The Western end of the Ryukyu active margin against the Taiwan collision zone: POP 2 cruise results. Presented at the Geodynamic Evolution of Rastern Eurasian Margin International Symposium. Chang, C.-P., J. Angelier, and C.-Y. Huang (2000). Origin and evolution of a melange: the active plate boundary and suture zone of the Longitudinal Valley, Taiwan. Tectonophysics, 355, 43-62. Chen, K.-C., and J.-H. Wang (1988). A study on aftershocks and focal mechanisms of two 1986 earthquakes in Hualien, Taiwan. Proc. Geol. Soc. China, 31, 65-72. Chen, K.-J., Y.-H. Yeh, H.-Y. Yen, and C.-H. Lin (1995). Seismological studies in the Chinshan fault area. J. Geol. Soc. China, 38, 335-353. Chiao, L.-Y., H. Kao, S. Lallemand, and C.-S. Liu (2001). An alternative interpretation for slip vector residuals of subduction interface earthquakes: a case study in the westernmost Ryukyu slab. Tectonophysics, 333, 123-134. Chou, H.-C., B.-Y. Kuo, S.-H. Hung, L.-Y. Chiao, D. Zhao, and Y.-M. Wu (2006). The Taiwan-Ryukyu subduction-collision complex: Folding of a viscoelastic slab and the double seismic zone. J. Geophys. Res., 111, B04410, doi: 10.1029/2005JB003822. Ellsworth, W.-L. and X. Zhonghuai (1980). Determination of the stress tensor from focal mechanism data, abstract. Eos Trans. AGU, 61, 1117. Ellsworth, W.-L. (1982). A general theory for determining state of stress in the earth from fault slip measurements. Terrea Congnita, 2, 170-171. Geiger, L. (1912). Probability method for the determination of earthquake epicenters from the arrival time only, (translated from Geiger’s 1910 German article), Bulletin of St. Louis University, 8, 56-71. Gephart, J.-W., and D.-W. Forsyth (1984). An improved method for determining the regional stress tensor using earthquake focal mechanism data: application to the San Fernando earthquake sequence. J. Geophys. Res., 100, 22197-22213. Gephart, J.-W. (1990a). FMSI - A Fortran program for invering fault/slickenside and earthquake focal mechanism data to obtain the regional stress tensor. Comput. And Geosci., 16, 953-989. Gephart, J.-W. (1990b). Stress and the direction of slip on fault planes. Tectonics, 9, 845-858. Hu, J.-C., S.-B. Yu, H.-T. Chu, and J. Angelier (2002). Transition tectonics of northern Taiwan induced by convergence and trench retreat. Geological Society of America Special Paper, 358, 149-162. Huang, C.-Y., P.-B. Yuan, C.-W. Wang, and C.-P. Chang (2000). Geodynamic processes of Taiwan arc-continent collision and comparison with analogs in Timor, Papua New Guinea, Urals and Corsica. Tectonophysics, 325, 1-21. Hsu, M.-T. (1971). Seismicity of Taiwan and some related problems. Bull. Intl. Inst. Seismol. Earthquake Eng., 8, 41-160. Hsu, V., C. Wang, Z.-S. Liaw, C.-T. Shyu, and F.-K. Duennebier (1987). Aftershocks monitered by a joint array of land stations and ocean bottom seismometers east of Taiwan. Geophys. Res. Lett., 14, 591-594. Kao, H., S. S. J. Shen, and K.-F. Ma (1998). Transition from oblique subduction to collision: Earthquakes in the southernmost Ryukyu arc-Taiwan region. J. Geophys. Res., 103, 7211-7229. Kim, K.-H., J.-M. Chiu, J. Pujol, and K.-C. Chen (2006). Polarity reversal of active plate boundary and elevated oceanic upper mantle beneath the collision suture in central eastern Taiwan. Bull. Seismol. Soc. Am., 96, 796–806. Kissling, E., W.-L. Ellsworth, D. Eberhart-Phillips, and U. Kradolfer (1994). Initial reference models in local earthquake tomography. J. Geophys. Res., 99, 19635-19646. Kuochen, Hao, Y.-M. Wu, C.-H. Chang, J.-C. Hu, and W.-S. Chen (2004). Relocation of the Eastern Taiwan Earthquakes and Its Tectonic Implications. Terre. Atmos. Oceanic Sci., 15, 647-666. Kuochen, Hao, Y.-M. Wu, Y.-G. Chen, and R.-Y. Chen (2007). 2003 Mw6.8 Chengkung Earthquake and its Related Seismogenic Structures. J. Asian Earth Sci., doi: 10.1016/j.jseaes.2006.07.028. Lallemand, S., C.-S. Liu, S. Dominguez, P. Schnurle, J. Malavieille, and the ACT scientific crew (1999). Trench-parallel stretching and folding of forearc basins and lateral migration of the accretionary wedge in the southern Ryukyus: a case of strain partition caused by oblique convergence. Tectonics, 18, 231-247. Lee, C.-N. (1962). Distribution of earthquake foci in the Taiwan region and its tectonic significance. Proc. Geol. Soc. China, 5, 109-118. Lee, C.-S., G.-G. Shor, L.-D. Bibee, R,-S. Lu, and T. Hilde (1980). Okinawa Trough: Origin of a back-arc basin. Mar. Geol., 35, 219-241. Lee, C.-T. and Y. Wang (1988). Quaternary stress changes in northern Taiwan and their tectonic implication. Proc. Geol. Soc. China, 31(1), 154-168. Lee, C.-S., S.-L. Chung, and SPOT Members (1998). Southernmost part of the Okinawa Trough (SPOT): An active extension/ collision/ subduction area. EOS, Trans. Am. Geophys. Union, 79, W109. Liang, W. T., J. C. Lee, and B. Y. Kuo (2005). Left-lateral strike-slip faulting in Ilan: Lateral extrusion at the transition betewwn Taiwan mountain range and the Okinawa Trough. GEEA, 104-108. Liu, C.-S., S.-Y. Liu, S.-E. Lallemand, N. Lundberg, and D. Reed (1998). Digital elevation model offshore Taiwan and its tectonic implication. Terre. Atmos. Oceanic Sci., 9, 705-738. Lu, C.-Y., J. Malavieille (1994). Oblique convergence, indentation and rotation tectonics in the Taiwan Mountain Belt: Insights from experimental modelling. Earth Planet. Sci. Lett., 121, 477-494. Lu, C.-Y., J. Angelier, H.-T. Chu, and J.-C. Lee (1995). Contractional, transcurrent, rotational and extensional tectonics: Examples from Northern Taiwan. Tectonophysics, vol. 125, 129–146. Ma, K.-F., and M. Kikuchi (1994). Initial investigation of the May 24, 1994 Hualien and June, 1994 Nanao earthquakes. Terr. Atmos. Oceanic Sci., 9 345-362. McKenzie, D.-P. (1969). The relation between fault plane solutions and the directions of the principal stress. Bull. Seismol. Soc. Am., 59, 591-601. Michael, A.-J. (1984). Determination of stress from slip data: faults and fold. J. Geophys. Res., 89, 11517-11526. Michael, A.-J. (1987). Use of focal mechanisms to determine stress: a control study. J. Geophys. Res., 92, 357-368. Rau, R.-J. and Francis T. Wu (1995). Tomographic imaging of lithospheric structures under Taiwan. Earth Planet. Sci. Lett., 133, 517-532. Reid, H.-F. (1911). The elastic-rebound theory of earthquakes. Univ. Calif. Publ. Bull. Dept. of Geol., 6, 413-444. Shyu, J. B. H., K. Sieh, Y.-G. Chen, and C.-S. Liu (2005a). Neotectonic architecture of Taiwan and its implications for future large earthquakes. J. Geophys. Res., 110, B08402, doi:10.1029/2004JB003251. Shyu, J. B. H., K. Dieh, Y.-G. Chen (2005b). Tandem suturing and disarticulation of the Taiwan orogen revealed by its neotectonic elements. Earth Planet. Sci. Lett., 233, 167-177. Sibuet, J.-C., J. Letouzey, F. Barrier, J. Charvet, J. P. Foucher, T. W. C. Hilde, M. Kimura, L.-Y. Chiao, B. Marsset, C. Muller, and J.-F. Stephan (1987). Back arc extention in the Okinawa trough. J. Geophys. Res., 92, 14041-14063. Sibuet, J.-C., B. Deffontaines, S.-K. Hsu, N. Thareau, J.-P. Le Formal, C.-S. Liu, and the ACT party (1998). Okinawa Trough backarc basin: Early tectonic and magmatic evolution. J. Geophys. Res., 103, 30245-30267. Suppe, J. (1984). Kinematics of arc-continental collision, flipping of subduction, and back-arc spreading near Taiwan. Mem. Geol. Soc. China, 4, 67-89. Teng, L.-S. (1990). Geotectonic evolution of late Cenozoic arc-continent collision in Taiwan. Tectonophysics, 183, 57-76. Teng, L.-S, (1996). Extensional collapse of the northern Taiwan mountain belt. Geology, 24, 949-952. Tsai, Y.-B., C.-C. Feng, J.-M. Chiu, and H.-B. Liaw (1975). Correlation between microearthquakes and geological faults in the Hsintien-Ilan area. Petrol. Geol. Taiwan, 12, 149-167. Tsai, Y.-B., T. Teng, J.-M. Chiu, and H.-L. Liu (1977). Tectonic implications of the seismicity in the Taiwan region. Mem. Geol. Soc. China, 2, 13-41. Thurber, C. and D. Eberhart-Phillips (1999). Local earthquake tomography with flexible gridding. Comput. Geosci., 25, 809-818. Um, J. and C.-H. Thurber (1987). A fast algorithm for two-point seismic ray tracing. Bull. Seismol. Soc. Am., 77, 972-986. Wang, T.-K. and C.-H. Chiang (1998). Imaging of arc-arc collision in the Ryukyu Forearc region offshore Hualien from TAICRUST OBS Line 16. Terre. Atmos. Oceanic Sci., 9, 329-344. Wu, F.-T. (1978). Recent tectonics of Taiwan. J. Phys. Earth, 26(suppl.), S265-S299. Wu, Y.-M., C.-H. Chang, N.-C. Hsiao, and F.-T. Wu (2003). Relocation of the 1998 Rueyli, Taiwan, earthquake sequence using three-dimensions velocity structure with stations corrections. Terre. Atmos. Oceanic Sci., 14, 421-430. Wu, Y.-M., C.-H. Chang, L. Zhao, J. B. H. Shyu, Y.-G. Chen, K. Sieh, and J.-P. Avouac (2007). Seismic tomography of Taiwan: Improved constraints from a dense network of strong-motion stations. J. Geophys. Res. in press. Yeh, Y.-H., C.-H. Lin, and S.-W. Roecker (1989). A study of upper crustal structures beneath northeastern Taiwan : possible evidence of the western extension of Okinawa Trough. Proc. Geol. Soc. China, 32(2), 139-156. Yeh, Y.-H., Eric Barrier, C.-H. Lin, and J. Angelier (1991). Stress tensor analysis in the Taiwan area from focal mechanisms of earthquakes. Tectonophysics, 200, 267-280. Yu, S.-B. and Tsai Y.-B. (1981). A study of microseismicity and crustal deformation of the Kuangfu-Fili area in eastern Taiwan. Bull. Inst. Earth Sci., Academia Sinica, 2, 1-18. Yu, S.-B., and L.-C. Kuo (2001). Present-day crustal motion along the Longitudinal Valley Fault, eastern Taiwan. Tectonophysics, 333, 199-217. 王鑫，1990，台灣地形景觀，渡假出版社，共250頁。 江新春，1976，宜蘭平原之震測，礦業技術第14卷，第6期，第215-221頁。 李錫堤、鄭錦桐、廖啟雯、張原賓，1998，台灣活斷層圖，中央大學應用地質研究所，工程及地質防災科技研究室。 李瓊武、余水倍，1987，台灣東部水平變動之研究，第六屆測量學術及研討會論文集，第127-134頁。 李建成，1988，台灣北部的新構造運動：斷層與古應力的分析研究，國立台灣大學碩士論文，共128頁。 何春蓀，1982，台灣地質概論－台灣地質圖說明書，經濟部中央地質調查所出版，共164頁。 林哲民、張道明、溫國樑，2003，利用接收函數法推估蘭陽平原淺層速度構造，第十屆台灣地區地球物理研討會論文集，第351-353頁。 林啟文、林偉雄、高銘健，1993，五萬分之一台灣地質圖圖幅第二十二號，經濟部中央地質調查所。 林啟文、高銘健，1997，五萬分之一台灣地質圖圖幅第十六號，經濟部中央地質調查所。 陳文山、王源，1996，台灣東部海岸山脈地質，經濟部中央地質調查所編印，共101頁。 陳穆申，2004，狹長造山帶的擠壓－伸張轉換過程：以台灣東部中央山脈的地震活動為例，國立成功大學碩士論文，共115頁。 許雅儒，1998，由GPS的觀測資料探討宜蘭平原的伸張變形，國立中央大學碩士論文，共108頁。 黃鑑水、何信昌，1989，五萬分之一台灣地質圖圖幅第十號，經濟部中央地質調查所。 葉恩肇，1998，台灣東北部蘇澳至東澳地區蓬萊造山運動之韌性剪切變形及其構造演化，國立台灣大學碩士論文，共186頁。 蔡義本，1976，宜蘭地區之地震研究，礦業技術第14卷，第5期，第156-165頁。 鄭世楠，1995，台灣及其鄰近地區大地應力分佈的研究，國立中央大學博士論文，共215頁。 賴慈華、謝孟龍，2003，台灣各沖積平原兩萬年來地塊垂直運動速率，中國地質學會九十二年年會暨學術研討會摘要，第119頁。 | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/30012 | - |
| dc.description.abstract | 台灣東北地區（121.0-123.0°E，23.5-25.5°N）受到隱沒帶（琉球弧溝系統）、弧後張裂（沖繩海槽），與弧陸碰撞（呂宋島弧）三者的共同影響，長久以來，一直是一個地震活躍、地質構造複雜，且地表調查不易的區域。在前人的研究中，多半將此區的宜蘭平原與縱谷地區分開討論，認為宜蘭平原受最新期海槽張裂活動的影響正處於伸張環境，地震多為正斷層；縱谷地區則因尚在弧陸碰撞的範圍，斷層機制以帶有右移分量的逆斷層為主，但對宜蘭平原與縱谷地區之間卻少有著墨。
因此，為探討台灣東北地區由碰撞末期轉變為隱沒拉張之構造特性。本研究收集中央氣象局地震觀測網（Central Weather Bureau Seismic Network, CWBSN）1994年1月至2005年12月發生在台灣東北地區，且條件為（1）同時有8個以上的測站清晰收到訊號、（2）芮氏規模（ML）大於3、（3）震源深度小於50公里之地震資料共12030筆，使用三維速度模型與測站修正法重新定位；並結合強地動觀測網（Taiwan Strong Motion Instrumentation Program, TSMIP）在此區密集的P波初動資料，求取高品質的震源機制初動解共169組，用以解析更精細的淺層地震構造。 資料分析結果顯示，斷層型態由北而南呈現正斷層（蘭陽溪以北）、走向斷層（蘭陽溪以南）、逆斷層（縱谷北段）的轉變。在弧陸碰撞轉變為弧後拉張之間，轉換帶是以有系統地走向斷層在運動，且在南澳走向滑移運動密集發生的地方，在重新定位後可區分出兩組不同走向的地震序列：一組是東西向的左移序列；另一組則位於東方外海，走向呈N50°W，有部分右移機制的出現，可能反應了沖繩海槽正向南擴張的現象。此外，在震源空間位置之時序分析中我們也發現在24.3-24.5ºN與24.8-24.9ºN有兩個高地震活動帶，分別對應到宜蘭平原最北的正斷層序列與南澳的走向斷層序列，前者可能受到沖繩海槽淺部張裂性地震活動向西南延伸的影響；後者則意味著此處為一正在活動的地質弱帶。且在南北向剖面中，觀察到一平行班氏帶的地震帶自縱谷北緣向北漸深，可能是海岸山脈已隨菲律賓海板塊隱沒的證據。 綜合上述研究結果，並佐以近年GPS測量與地球物理方面的資料，此走向斷層帶的成因，我們認為台灣東北地區正受到沖繩海槽西南延伸的影響，以宜蘭平原北緣之正斷層向南伸張，造成地層在彎折時發生層間的左移滑動，此一構造行為即沿著南澳一帶的地質弱帶發生，形成一系列的左移斷層系統。而海岸山脈碰撞之效應，因為隨板塊隱沒之故對此區淺部構造之影響已相對不再顯著。 | zh_TW |
| dc.description.abstract | Northeastern Taiwan (121.0-123.0°E，23.5-25.5°N) is a tectonically complex area acted by combined effects of slab subduction, backarc opening, and continental-arc collision. According to the previous studies, this area is usually divided into two tectonic entities, the Ilan basin and its sourthern collision zone. The Ilan basin related to Okinawa Trough is a extension environment dominated by normal faults and the collision zone is still a compressive environment because of the arc-continental collision. But the detail structure of the transition area between them has not been studied.
Therefore, this study tried to explore the tectonic characteristics of the transition area from waning collision, to subduction and then post-collisional extension. A total of 12030 earquakes recorded by Central Weather Bureau Seismic Network（CWBSN） from January 1994 to July 2005 were relocated and studied in this study. These events were relocated by using three-dimensional velocity model. By combination the first motion polarities from Taiwan Strong Motion Instrumentation Program（TSMIP）and CWBSN, totally 169 focal mechanism solutions were determined for tectonic analysis. Base on the results of the relocated seismicity and focal mechanisms, in the study region, the spatial distribution of the focal mechanisms sequentially switches from thrust, strike-slip, and normal fault northward. It is obvious that the transition area between back-arc extension and continental-arc collision is dominated by left lateral strike-slip fault systematically. Furthermore, based on the seismicity profiles, right-lateral focal mechanisms were determined in Nanao earthquake sequence and a concentrated seismicity zone parallel to the subduction zone. It is possible that Coastal Range（CR）has already subducted along with Phillipine Sea Plate and the transition area is affected by Okinawa Trough more than CR. In addition, two active seismicity zones found in latitude 24.3-24.5ºN and 24.8-24.9ºN are corresponding to the normal and left-lateral strike-slip zone, respectively. It might imply that these two zones were located at the tectonic weak zone and thus with high seismicity. In conclusion, the southward opening of the Okinawa trough is a main driving force in northeastern Taiwan and bending the north Taiwan mountain belt. The left-lateral fault system appears at transition area was caused by the bedding-slip motion for considering the results from relocated seismicity, focal mechanisms and geological settings. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-13T01:30:32Z (GMT). No. of bitstreams: 1 ntu-96-R94224211-1.pdf: 9274813 bytes, checksum: a35cf497939c3c23faea7480dce636b2 (MD5) Previous issue date: 2007 | en |
| dc.description.tableofcontents | 中文摘要 I
英文摘要 III 誌謝 V 目 錄 VI 圖目錄 VIII 表目錄 X 第一章 緒論 1 1.1 研究內容簡介 1 1.2 研究動機與目的 3 第二章 研究區域背景 5 2.1 區域概況 5 2.1.1 地形與地質 5 2.1.2 地體構造 7 2.2 前人研究 11 2.2.1 南沖繩海槽的地形與構造演化 11 2.2.2 宜蘭平原下方之構造地質與盆地形貌 12 2.2.3 宜蘭平原之塌陷與沖繩海槽的關連性 12 2.2.4 菲律賓海板塊的隱沒與扭曲 16 2.2.5 琉球海溝西緣與花東縱谷北端的界線 16 2.2.6 海岸山脈的去向 16 2.2.7 花東縱谷北段的特性 17 2.2.8 碰撞-隱沒帶之構造特性 21 第三章 研究方法 24 3.1 資料來源、選取與分析流程 24 3.1.1 最小完整地震規模（Mc）之時序分析 25 3.1.2 強地動觀測網（TSMIP）的優勢 26 3.2 地震重新定位 28 3.2.1 三維速度構造與測站修正 30 3.2.2 一維與三維速度模型 33 3.2.3 三維速度層析影像 34 3.3 震源機制解 35 3.3.1 以初動法求解 36 3.3.2 地震網外的涵蓋問題 39 3.3.3 初動法與波形逆推法之歧異 39 3.3.4 應力反演的代表性 40 第四章 研究成果 43 4.1 地震重新定位結果 43 4.2 震源位置在經度、緯度及深度之時序分析 51 4.3 震源機制解結果 55 4.3.1 區域應力反演結果 55 4.3.2 地震構造與三維速度層析影像的套疊 60 第五章 討論 74 5.1 宜蘭地區的淺層地震構造 74 5.2 花東縱谷北段的淺層地震構造 77 5.3 海岸山脈的隱沒 80 5.4 轉換帶走向斷層系統之運動機制推演 81 5.4.1 GPS向量場之比對 82 5.4.2 古應力資料的時序探討 86 第六章 結論 88 參考文獻 89 附錄A 地震震源機制解參數表 96 附錄B 地震震源機制解圖錄 101 附錄C 2006地質年會得獎海報（優勝） 109 附錄D 2007 TGA台灣地球科學聯合學術研討會得獎海報（佳作） 110 | |
| dc.language.iso | zh-TW | |
| dc.title | 台灣東北地區的地震構造：由碰撞末期轉變為隱沒拉張之構造特性 | zh_TW |
| dc.title | Seismotectonics of northeastern Taiwan: Structural characteristics of a transitional area from waning collision to subduction and post-collisional extension | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 95-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 陳于高(Yue-Gau Chen),張建興(Chien-Hsin Chang),黃柏壽(Bor-Shouh Huang) | |
| dc.subject.keyword | 地震構造,地震重定位,震源機制解, | zh_TW |
| dc.subject.keyword | seismotectonics,earthquake relocation,focal mechanism, | en |
| dc.relation.page | 110 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2007-07-17 | |
| 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 | |
文件中的檔案：
| 檔案 | 大小 | 格式 | |
|---|---|---|---|
| ntu-96-1.pdf 目前未授權公開取用 | 9.06 MB | Adobe PDF |
系統中的文件，除了特別指名其著作權條款之外，均受到著作權保護，並且保留所有的權利。