請用此 Handle URI 來引用此文件:
http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/27039
完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 陳于高 | |
dc.contributor.author | Po-Nong Li | en |
dc.contributor.author | 李珀儂 | zh_TW |
dc.date.accessioned | 2021-06-12T17:54:19Z | - |
dc.date.available | 2008-02-18 | |
dc.date.copyright | 2008-02-18 | |
dc.date.issued | 2008 | |
dc.date.submitted | 2008-02-04 | |
dc.identifier.citation | 一、中文部份
六角兵吉和牧山鶴彥, 1934. 高雄洲恆春油田調查報告. 台灣總督府殖產局出版, 第660號. 石崎和彥, 1942. 西恆春台地附近地質學的觀察. 台灣地學記事, 第13卷(第2-3號): 第46-64頁. 石再添、鄧國雄、張瑞津和楊貴三, 1985. 恆春地區的活斷層與地形面. 國立台灣師範大學地理教育, 第11期: 第1-12頁. 石再添, 蔡文彩, 許民陽, 目崎茂和和木庭元晴, 1989. 墾丁國家公園地區的珊瑚礁定年及地形研究. 內政部營建署墾丁國家公園管理處, 保育研究報告第57號: 共58頁. 宋國城, 1991. 臺灣地質圖幅及說明書,圖幅第六九、七十、七二號,恆春半島. 經濟部中央地質調查所: 共77頁. 吳樂群和陳華玟, 1990. 台灣南部恆春西台地北段晚更新世地層之沉積層序. 經濟部中央地質調查所彙刊, 第6號: 第13-50頁. 周佳毅, 2003. 鵝鸞鼻岬近岸海床地貌研究. 國立台灣大學海洋研究所碩士論文: 共122頁. 莊惠如, 2006. 台灣西南海域泥貫入體分佈與構造活動之關係. 國立台灣大學海洋研究所碩士論文: 共113頁. 林朝棨, 1957. 台灣地形. 台灣省文獻委員會: 共424頁. 林久芳, 1989. 台灣恆春半島及東部海岸全新世隆起珊瑚礁之鈾系定年研究. 國立台灣大學地質研究所碩士論文: 共119頁. 張敏, 1985. 台灣南部恆春半島新第三系之生物地層. 國立台灣大學地質研究所碩士論文: 共65頁. 張成華, 1993. 台灣西南部海域之泥貫入體研究. 國立台灣大學海洋研究所碩士論文: 共71頁. 徐鐵良, 1984. 地質與工程. 中國工程師學會: 第55-102頁. 許中民, 1986. 台灣南端恆春半島第四紀後期構造運動之研究. 國立台灣大學地質研究所博士論文: 共135頁. 許民陽, 1988. 台灣海階之地形學研究. 私立中國文化大學地學研究所博士論文: 共178頁. 陳文山, 1985. 台灣南部恆春半島之地質. 國立台灣大學地質研究所碩士論文: 106頁. 陳文山, 黃奇瑜和鄭穎敏, 1985. 台灣恆春半島中新世地層之生痕化石. 地質, 第6卷(第2期): 第21-38頁. 陳文山和李偉彰, 1990. 西恆春台地地層之檢討. 地質, 第10期(第2卷): 第127-140頁. 陳文山, 1992. 恆春半島墾丁層層位及時代的檢討. 經濟部中央地質調查所特刊, 第6期: 第135-142頁. 陳文山, 黃能偉, 顏一勤, 楊志成和楊小青, 2004. 地震地質調查及活動斷層資料庫建置計畫槽溝開挖與股地震研究計畫(3/5)--三、恆春斷層條帶地質圖說明書. 經濟部中央地質調查所報告第93-6號: 共39頁,附兩張恆春斷層條帶地質圖. 陳文山, 李偉彰, 黃能偉, 顏一勤, 楊志成, 楊小青, 陳勇全和宋時驊, 2005. 恆春半島增積岩體的構造與地層特性:全新世恆春斷層的活動性. 西太平洋地質科學, 第5卷: 第129-154頁. 馮立中, 2006. 台灣南部海域增積岩體的構造特徵. 國立台灣大學海洋研究所, 碩士論文: 共68頁. 傅式齊, 1997. 台灣南部陸上及海域弧陸斜向碰撞及隱沒構造之演化. 國立台灣大學理學院海洋研究所碩士論文: 共99頁. 黃衍騮, 1993. 台灣西南部海域之地質構造分析. 國立台灣大學地質科學研究所碩士論文: 共64頁. 黃偉倫, 1995. 台灣西南海域泥貫入體之分布與陸上諸背斜之關係及其對沉積環境之影響. 國立台灣大學海洋研究所碩士論文: 共68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. 詹新甫, 1974. 恆春半島之地層與構造並申論中新世傾瀉層. 台灣省地質調查所彙刊, 第24號: 第99-108頁. 二、英文部分 Biq, C.C., 1972. Dual-trench structure in the Taiwan-Luzon region. Proceedings of the Geological Society of China, 15: 65-75. Biq, C.C., 1977. The Kenting Melange and the Manlia Trench. Proceedings of the Geological Society of China, 20: 119-122. Byrne, T., 1995. Deformation partitioning and tectonic exhumation in the pre-collision zone of the Taiwan orogenic belt. EOS Transactions, Amer. Geophys. Union, 76(46): F635. Chemenda, A.I., Yang, R.K., Hsieh, C.H. and Groholsky, A.L., 1997. Evolutionary model for the Taiwan collision based on physical modelling. Tectonophysics, 274: 253-274. Chemenda, A.I., Yang, R.K., Stephan, J.F., Konstantinovskaya, E.A. and Ivanov, G.M., 2001. New results from physical modelling of arc-continent collision in Taiwan: evolutionary model. Tectonophysics, 333: 159-178. Chen, Y.G. and Liu, T.K., 1993. Holocene Radiocarbon Dates in Hengchun Peninsula and Their Neotectonic Implications. Journal of the Geological Society of China, 36(4): 457-479. Cheng, Y.M. and Haung, C.Y., 1975. Biostratigraphic study in the west Hengchun Hill. . ACTA Geologica Taiwanica, 18: 49-59. Cheng, W.B., Wang, C.S. and Shyu, C.T., 1998. A three-dimensional Vp model of the southeastern Taiwan area and its tectonic implications. TAO, 9(3): 425-452. Chi, W.S. et al., 2003. Tectonic wedging along the rear of the offshore Taiwan accretionary prism. Tectonophysics, 374: 199-217. Claudio, V.F. and Lin, J.C., 2005. Neotectonics and seismic hazard assessment in Hengchun Peninsula, southern Taiwan. C.R. Geoscience, 337: 1194-1199. Grando, G. and McClay, K., 2007. Morphotectonics domains and structural styles in the Makran accretionary prism, offshore Iran. Sedimentary Geology, 196: 157-179. Ho, C.S., 1986. A synthesis of the geologic evolution of Taiwan. Tectonophysics, 125: 1-16. Ho, C.S., 1988. An introduction to the geology of Taiwan, explanatory text of the geological map of Taiwan. Central Geological Survey, Minisitry of Economic Affairs, Taipei: 192pp. Huang, C.Y., Shyu, C.T., Lin, S.B., Lee, T.Q. and Sheu, D.D., 1992. Marine geology in the arc-ccontinent collision aone off southeastern Taiwan: Implications for Late Neogene evolution of the Coastal Range. Marine Geology, 107: 183-212. Huang, C.Y., Yuan, P.B., Lin, C.B. and Wang, T.K., 2000. Geodynamic processes of Taiwan arc-continent collision and comparison with analogs in Timor, Papua New Guinea, Urals and Corsica. Tectonophysics, 325: 1-21. Huang, C.Y., Yuan, P.B. and Tsao, S.J., 2006. Temporal and spatial records of active arc-continent collision of Taiwan: A synthesis. GSA Bulletin, 118(3/4): 274-288. Kao, H., Huang, G.C. and Liu, C.S., 2000. Transition from oblique subduction to collision in the northern Luzon arc-Taiwan region: Constraints from bathymetry and seismic observations. J. Geophys. Res., 105(B2): 3059-3080. Kimura, G., Kitamura, Y., Hashimoto, Y., Yamaguchi, A., Shibata, T., Ujiie, K. and Okamoto, S. 2007. Transition of accretionary wedge structures around the up-dip limit of the seismogenic subduction zone. Earth and Planetary Science Letters, 255: 471-484. Liew, P.M. and Lin, C.F., 1987. Holocene activity of the Hengchun Peninsula as evidenced by the deformation of marine terraces. Mem. Geol. Soc. China, 9: 241-259. Liu, C.S., Huang, I.L. and Teng, L.S., 1997. Structural features of southwestern Taiwan. Marine Geology, 137: 305-319. Liu, C.S., Liu, S.Y., Lallemand, S.E., Lundberg, N. and Reed, D.L., 1998. Digital elevation model offshore Taiwan and its tectonic implications. TAO, 9(4): 705-738 Lu, C.Y. and Hsu, K.J., 1992. Tectonic evolution of the Taiwan mountain belt. Petroleum Geology of Taiwan, 27: 21-46. Lundberg, N., Reed, D.L., Liu, C.S. and J. Lieske, J., 1992. Structural controls on orogenic sedimentation, submarine Taiwan accretionary collision. Acta Geologica Taiwanica, 30: 131-140. Lundberg, N., Reed, D.L., Liu, C.S. and J. Lieske, J., 1997. Forearc-basin closure and arc accretion in the submarine suture zone south of Taiwan. Tectonophysics, 274: 5-23. Malavieille, J., Lallemand, S.E., Dominguez, S., Deschamps, A., Lu, C.Y., Liu, C.S. and Schnurle, P. 2002. Arc-continent collision in Taiwan: New marine observations and tectonic evolution. Geological Society of America, Special Paper(358): 187-211. McIntosh, K. et al., 2005. Crustal-scale seismic profiles across Taiwan and the western Philippine Sea. Tectonophysics, 401: 23-54. Nakamura, Y., McIntosh, K. and Chen, A.T., 1998. Preliminary results of a large offset seismic survey west of Hengchun Peninsula, Southern Taiwan. TAO, 9(3): 395-408. Pan, Y.S., 1968. Interpretation and seismic coordination of the Bouguer gravity anomalies obtained in southwestern Taiwan. Mem, Geol. Soc. China, 6: 197-208. Pelletier, B. and Stephan, J.F., 1986. Middle Miocene obduction an late Miocene beginning of collision registered in the Hengchun Peninsula: Geodynamic implications for evolution of Taiwan. Tectonophysics, 125: 133-160. Pelletier, B., Stephan, J.F., Blanchet, R., Muller, C. and Hu, H.N., 1984. Geology of the Hengchun Peninsula, Southern Taiwan: argument for a moddle obduction and for an arc-continental collision since Upper Miocene(Abs). Sino-French Seminar on Geodynamics of the Eurassian-Philippine Sea Plate Boundary, Taipei,April 20-30: 64-65. Peng, T.H., Li, Y.H. and Wu, F.T., 1977. Tectonic uplift rates of the Taiwan island since the early Holocene. Mem. Geol. Soc. China, 2: 57-70. Reed, D.L., Lundberg, N., Liu, C.S. and Kuo, B.Y., 1992. Structural relations along the margin of the offshore Taiwan accretionary wedge: implications for accretion and crustal kinematics. Acta Geologica Taiwanica, 30: 105-122. Schluter, H.U. et al., 2002. The Makran accretionary wedge:sediment thickness and ages and the origin of mud volcanoes. Marine Geology, 185: 219-232. Shih, T.T., Teng, K.H., Chang, J.C. and Yang, G.S., 1985. The active faults and geomorphic surfaces of Hengchun Area in Taiwan (in Chinese with English abstract). Geogr. Educ., 11: 1-14. Shyu, J.B.H., Sieh, K. and Chen, Y.G., 2005a. Tandem suturing and disarticulation of the Taiwan orogen revealed by its neotectonic elements. Earth and Planetary Science Letters, 233: 167-177. Shyu, J.B.H., Sieh, K., Chen, Y.G. and Liu, C.S., 2005b. Neotectonic architecture of Taiwan and its implications for future large earthquakes. Journal of Geophysical Research, 110,B08402: doi:10.1029/2004JB003251. Sung, Q.C. and Wang, Y., 1986. Sedimentary environment of the Miocene sediments in the Hengchun Peninsula and their tectonic implication. Mem, Geol. Soc. China, 7: 325-340. Suppe, J., 1984. Kinematics of arc-continent collision, flipping of subduction, and back-arc spreading near Tiawan. Mem. Geol. Soc. China, 6: 21-33. Tang, J.C., Chemenda, A.I., Chery, J., Lallemand, S. and Hassani, R., 2002. Compressional subduction regime and initial arc-continental collisin: Numerical modelling. Geol. Soc. Am. Special paper, 358: 177-186. Wang, T.K., Chen, M.K., Lee, C.S. and Xia, K., 2006. Seismic imaging of the transiotional crust across the northeastern margin of the South China Sea. Tectonophysics, 412: 237-254. Wu, F.T., 1978. Recent tectonics of Taiwan. Jour. Phys. Earth, 26(Suppl.): 265-299. Yu, H.S. and Chiang, C.S., 1995. Morphology and origin of the Hongtsai submarine canyon west of the Hengchun Peninsula, Taiwan. Journal of the Geological Society of Taiwan, 38(1): 81-93. | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/27039 | - |
dc.description.abstract | 本研究區域位於台灣南端,包含陸上之恆春半島與一部份海裡之恆春海脊。鑒於本研究區域過往之前人研究,鮮少同時討論對陸上與海中之地質、地形與構造之關係。本研究冀望藉由地理資訊系統(GIS)、數值地型模型、航空照片、野外調查、反射震測資料與多音束測深系統(MBS)等工具,對於本研究區域之地形進行重新檢視,進而判斷近期活動構造之運動行為,最後整合各項資訊,對恆春區域之新期構造運動作整體性之了解。
陸上之調查結果將恆春半島上之海階地形面由老至年輕劃分為一到八期,整體恆春半島皆有第八期之海階分布,表示恆春半島近期來處於一個整體隆升之構造階段。西恆春台地上由五至七期之海階分布,愈老之海階紀錄愈多地形東傾之行為,表示西恆春台地近期來一直處於構造傾動之階段。鵝鑾鼻半島上由一到六期之海階分布,海階之變形顯示鵝鸞鼻半島整體為一背斜構造。恆春斷層沿線之構造地形,呈現恆春斷層為一左移走向分量大於逆衝分量之斷層,並在湖內以南,分為三條分支斷層,應該與恆春斷層之走向於湖內發生轉折有關。 海中之地形顯示恆春區域大體上可視為一背斜構造,其主要特徵為背斜之頂部寬廣,兩翼呈現陡峭之地形,本研究稱此一背斜為恆春背斜。恆春背斜乃由東邊的南縱海槽斷層,與西邊的西恆春斷層所組成之一上衝構造所造成。其中由震測剖面之解釋並配合海底地形的分析,可以得知西恆春台地因為座落於西恆春背斜之東翼,而造成其地形上東傾與海階面變形之結果。另外由震測與地形資料之分析,發現恆春斷層出海後,走向轉為北偏西30度,便一路往南延伸與南縱海槽斷層相接。海深資料顯示本研究區分布有眾多之正斷層,多為因應大地應力而生。 整合上述之種種資料,本研究區域之新期構造運動以南縱海槽斷層與西恆春斷層所組成之上衝構造為主,其中恆春斷層以左移之運動方式斜切而過。 | zh_TW |
dc.description.abstract | The study area including onshore Hengchun Peninsula and part of offshore Hengchun Ridge is located at southern Taiwan and called Hengchun Area. Because the previous studies about Hengchun Area rarely tie the onshore and offshore geological, geomorphological and structural information together to have a further discussion. This study would like to re-examine the geomorphology of Hengchun Area by using tools such as Geographic Information System (GIS), Digital Elevation Model (DEM), aerial photos, reflection seismic data, and Multibeam Echo Sounding System (MBS). By compiling all the information that we acquire from both this study and previous studies, this study feels like achieving the objective of comprehension of the neotectonics of Hengchun Area.
Marine terraces is divided into eight stages on Hengchun Peninsula, from marine1 (oldest) to marine 8 (youngest). Holocene terraces, marine 8, are widely distributed over Hengchun Peninsula, indicating recently tectonic uplifting of Hengchun Peninsula. On the east-tilting Western Hengchun Tableland, there are marine 5 to marine 7 covering on the surface. The phenomenon of older terraces showing greater slope elucidates the continuously tilting of Western Hengchun Tableland. The deformation of marine terraces on Oluanpi Peninsula shows that the Oluanpi Peninsula itself is an antiform structure. The tectonic-related landforms along Hengchun Fault trace indicate that the left-lateral slip of Hengchun Fault is greater than dip slip and the Hengchun Fault separates into three branchces south of Hunei as the result of fault-strike change. Offshore bathymetric data shows that Hengchun Area is a huge antiform shape with broad top and steep limbs. This antiform is called Hengchun Antiform and is made up by a pop-up structure. The pop-up structure is composed of South Longitudinal Trough Fault to the east limb and Western Hengchun Fault to the west limb. Based on interpretations from seismic and bathymetry data, this study relates the east-tilting and deformation of marine terraces on Western Hengchun Tableland to the fact that Western Hengchun Tableland itself is the east limb of Western Hengchun Antiform. The strike of Hengchun Fault turns to N30oW when it extends southward offshore and then connects with South Longitudinal Trough Fault. The pervasive normal faulting in Hengchun Area is probably in response to regional tectonic stress. In summary, nectectonics of Hengchun Area is characterized by a pop-up structure and Hengchun Fault which obliquely cuts through the Hengchun Area with larger sinistral displacement than vertical displacement. | en |
dc.description.provenance | Made available in DSpace on 2021-06-12T17:54:19Z (GMT). No. of bitstreams: 1 ntu-97-R94224111-1.pdf: 12447023 bytes, checksum: 5f25e4839d0faad1e318c9f02e9e9bba (MD5) Previous issue date: 2008 | en |
dc.description.tableofcontents | 口試委員審定書………………………………………………………I
致謝…………………………………………………………………...II 中文摘要……………………………………………………………..III 英文摘要……………………………………………………………..IV 第一章 緒論...…………………………………………………….….1 1.1研究動機……………………………………………………....1 1.2研究目的………………………………………………….…...4 1.3研究方法………………………………………………….…...4 1.3.1航空照片與數位高程模型…………………………..….4 1.3.2野外考察…………………………………………….…..6 1.3.3海底地形資料………………………...............................7 1.3.4反射震測資料……………………………………….…..7 第二章 前人研究……………...……………………….....................10 2.1 大地構造架構……………………………………………......10 2.2 區域地質…………………………………………………......11 2.2.1 恆春海脊—增積岩體的骨幹……………………...…..11 2.2.2 恆春半島—陸上的增積岩體………………………….12 2.3 海底相關研究………………………………………………..15 2.4 陸上相關研究…………………………………………..........17 2.4.1 西恆春台地相關研究………………………………….17 2.4.2 恆春斷層相關研究…………………………………….17 2.4.3 活動構造與其他相關研究…………………………….19 第三章 陸上地形分析與野外調查結………………………………21 3.1 地形面分析………………………………………………..…21 3.1.1海階面分布與對比.…………………………………..…22 3.1.2 其他地形面分析……………………………………..…22 3.2 構造地形判釋……………………………..……………...…24 3.2.1 恆春斷層沿線…………………………………….…….24 3.2.2 恆春斷層沿線野外調查結果…………………………..38 3.2.3 西恆春台地……………………………………………..44 3.2.4 西恆春台地野外調查結果……….…………………….51 3.2.5 鵝鸞鼻半島……………………………………………..52 第四章 海底地形分析與震測資料解釋.…………..……………….55 4.1 海底地形分析……………………………………………….55 4.2 恆春背斜………………………………………………….…56 4.3 楓港外海構造地形分析與震測資料解釋………………….59 4.4 西恆春台地外海構造地形分析與震測資料解釋………….62 4.5 南灣—鵝鑾鼻外海構造地形分析與震測資料解釋……….73 4.6 三角陷落帶構造地形分析………………………………….73 第五章 討論...……………………………………………………….76 5.1 恆春斷層之運動特性……………………………………….76 5.2 恆春斷層之海陸連結……………………………………….76 5.3 活動構造之成因…………………………………………….78 5.3.1恆春斷層之成因…………….…………………………..78 5.3.2西恆春背斜之成因………….…………………………..81 5.3.3本研究區域恆春背斜之成因………………….………..82 5.3.4西恆春斷層之成因…………………………….………..82 5.3.5三角陷落帶之成因…………………………….………..83 5.3.6張裂性正斷層系統之成因…………………….………..83 5.4 恆春區域之新期構造運動特性…………………………….84 5.5 近期構造活動性…………………………………………….85 第六章 結論…………...…………………………………………….87 參考文獻…………...………………………………………………...88 | |
dc.language.iso | zh-TW | |
dc.title | 南台灣恆春區域新期構造運動之研究 | zh_TW |
dc.title | Neotectonics of Hengchun Area, Southern Taiwan | en |
dc.type | Thesis | |
dc.date.schoolyear | 96-1 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 劉家瑄,朱傚祖,李建成,宋國士 | |
dc.subject.keyword | 恆春半島,恆春斷層,西恆春斷層,西恆春背斜,西恆春台地,上衝構造, | zh_TW |
dc.subject.keyword | Hengchun Fault,Hengchun Peninsula,Western Hengchun Tableland,Western Hengchun Fault,Western Hengchun Antiform,Pop-up structure, | en |
dc.relation.page | 92 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2008-02-04 | |
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-97-1.pdf 目前未授權公開取用 | 12.16 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。