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完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 詹瑜璋 | zh_TW |
dc.contributor.advisor | Yu-Chang Chan | en |
dc.contributor.author | 白庭瑜 | zh_TW |
dc.contributor.author | Ting-Yu Pai | en |
dc.date.accessioned | 2023-05-18T16:12:33Z | - |
dc.date.available | 2023-11-09 | - |
dc.date.copyright | 2023-05-10 | - |
dc.date.issued | 2023 | - |
dc.date.submitted | 2023-02-10 | - |
dc.identifier.citation | 王源與陳文山(1993)十萬分之一海岸山脈地質圖幅。經濟部中央地質調查所。
王意華(2017)高解析度數值高程模型地形參數之網格式製圖分析。航測及遙測學刊。第22卷,第2期,第77-92頁。 石再添、鄧國雄、許民揚與楊貴三(1988)臺灣花東海岸海階的地形學研究。師大地理研究報告,第14期,第1-50頁。 宋國城(1991)利吉層中富岡砂岩之沈積機制研究。中國地質學會會刊,第34卷,第3期,第173-197頁。 宋聖榮(1990)臺灣東部海岸山脈中段火山岩研究兼論北呂宋火山島弧的演變。 臺灣大學地質科學研究所博士論文,共251 頁。 宋聖榮與羅煥記(1990)臺灣東部海岸山脈火山岩及相關岩石之層序。經濟部中央地質調查所特刊,第4號,第 261-270 頁。 李民(1984)臺灣東部海岸山脈南段瑞源地區的地質。國立臺灣大學地質科學研究所碩士論文,共54.頁。 李德貴與紀文榮 (1990)海岸山脈沈積岩地層的古地磁年代。經濟部中央地質調查所特刊,第4號,第 271-294 頁。 林泗濱(1986)台東縣海岸山脈黏土之礦床。地質,第7卷,第2期,第35-53頁。 林益正(1993) 台灣東部利吉層中基質泥及沙岩岩塊之構造分析與其構造環境之意義,國立台灣大學地理學研究所碩士論文,124頁 林偉雄、林啟文、劉彥求與陳柏村(2008)五萬分之一臺灣地質圖及說明書-臺東、知本圖幅。經濟部中央地質調查所,共58頁。 邱家宏(2018)應用高精度數值地形精進臺北地區褶皺逆衝帶地質圖。國立臺灣大學地質科學研究所碩士論文,共135頁,doi: 10.6342/NTU201801939。 邵文佑(2015)利用鋯石鈾鉛定年與鉿同位素組成探討台灣東部火成岩之岩石成因。國立臺灣大學地質科學研究所碩士論文,共287頁。doi:10.6342/NTU.2015.01013。 施乃慈(2018)在三維環境中繪製高解析度地質圖:以臺灣北部雙溪地質圖幅為例。國立臺灣大學地質科學研究所碩士論文,共145頁,doi: 10.6342/NTU201802944。 姚宗茂、田沛霖與王執明(1989)臺灣東部泰源盆地之地層與沉積環境。地質,第9卷,第1期,第95-112頁。 孫正瑋(2019)應用高解析度數值地形模型精進輕度變質岩區地質圖-以頭城地質圖幅為例。國立臺灣大學地質科學研究所碩士論文,共112頁,doi: 10.6342/NTU201901740。 徐鐵良(1954)臺灣東部海岸山脈地形與近期上升運動。臺灣省地質調查所彙刊,第7號,第9-18頁。 徐鐵良(1956)臺灣東部海岸山脈地質。臺灣省地質調查所彙刊,第8號,第15-41頁。 侯進雄、費立沅、邱禎龍、陳宏仁、謝有忠、胡植慶與林慶偉(2014)空載光達數值地形產製與地質災害的應用。航測及遙測學刊,第18號,第2期, 93-108 唐懷昱(2018)海岸山脈南段泰源盆地凝灰岩之初步研究。國立臺灣大學地質科學研究所碩士論文,共87頁。 袁彼得(2009)海岸山脈南段東河石灰岩中白雲岩的成因及機制。行政院國家科學委員會專題研究計畫成果報告(精簡版),共13頁。 陳文山(1988)臺灣海岸山脈沉積盆地之演化及其在地體構造上之意義。國立臺灣大學地質學研究所博士論文,共 344 頁。 陳文山(1991)台灣東部海岸山脈利吉層的成因。經濟部中央地質調查所特刊,第5號,第257-266頁。 陳文山(2009)海岸山脈火山島弧與碰撞盆地的地層架構與年代。西太平洋地質科學,第9卷,第67-98頁。 陳文山(2016)臺灣地質概論。臺北市:中華民國地質學會。 陳文山與王源(1996)臺灣東部海岸山脈地質。經濟部中央地質調查所,共101頁。 陳思婷(2018)晚更新世以來花東海岸南段的階地演化。國立台灣大學地質科學研究所碩士論文,共163頁。 詹瑜璋(2009)大台北地區特殊地質災害調查與監測第二期-空載雷射掃描數值地形地質構造分析(2/4)(計畫編號:98-5226904000-03-03)。新北市:經濟部中央地質調查所。 詹瑜璋(2010)大台北地區特殊地質災害調查與監測第二期-空載雷射掃描數值地形地質構造分析(3/4)(第三年度)(計畫編號:99-5226904000-03-03)。新北市:經濟部中央地質調查所。 詹瑜璋 (2012)空載光達技術完美刻畫大屯火山群地形。地質,第31卷,第1期,第 32-35 頁。 詹瑜璋、張國楨與陳柔妃(2012)空載光達精準判釋海岸山脈中段構造地形。地質,第31卷,第2期,第42-43頁。 趙柏濂(2021)應用空載光達數值地形精進火成岩與沉積岩混合區地質圖:以海岸山脈玉里地質圖幅為例。國立臺灣大學地質科學研究所碩士論文,共128頁doi: 10.6342/NTU202101583。 劉彥求(1997)海岸山脈南段及綠島之構造地質研究。國立成功大學地球科學系碩士論文,共 87 頁。 賴序衡(2015) 海岸山脈南段泰源盆地之地層架構及沉積歷史。國立臺灣大學地質科學研究所碩士論文,共103頁。 賴序衡與鄧屬予(2015)縱橫泰源 台23線地質旅遊。地質,第34卷,第2期,第44-51頁。 賴序衡與鄧屬予(2016)海岸山脈南段泰源盆地的地層與構造。經濟部中央地質調查所彙刊,第29號,第45-76頁。 賴序衡、吳天偉與鄧屬予(2018)東台灣海岸山脈南段八里灣層中凝灰岩層及礫質岩層之對比。經濟部中央地質調查所彙刊,第31號,第1-32頁。 賴昱銘(2012)北呂宋島弧的火山岩漿與演化。國立臺灣大學地質科學研究所博士論文,共216頁。 簡至暐(2003)台灣東部海岸山脈利吉混同岩體成因之研究:微體古生物證據。國立台灣大學地質科學研究所碩士論文,共211頁。 羅煥記(1993)東台灣海岸山脈成廣澳山東坡區安山岩之地質與地球化學。(計畫編號:NSC 81-0202-M-002-10)。台北市:行政院國家科學委員會。 羅煥記、陳文山與宋聖榮(1993)五萬分之一臺灣地質圖及說明書-成功、東河圖幅,經濟部中央地質調查所。 龐麒修(2019)台灣海岸山脈最南端利吉混同層構造演化。國立中央大學地球科學學系碩士論文,共122頁。 Barrier, E. and Muller, C.(1984)New observations and discussion on the origin and age of the Lichi Mélange. Mem.Geol. Soc.China, 6, 303-26 Chang, C. P., Angelier, J. and Huang, C. Y.(2000) Origin and evolution of a mélange: the active plate boundary and suture zone of the Longitudinal Valley, Taiwan. Tectonophysics, 325, 1-2, 43-62. Chang, C. P., Angelier, J., Huang, C. Y. and Liu, C. S.(2001)Structural evolution and significance of a mélange in a collision belt: the Lichi Mélange and the Taiwan arc–continent collision. Geol. Mag. 138 (6), 633-651, doi: 10.1017/S0016756801005970 Chang, L.S. (1967) A biostratigraphic study of the Tertiary in the Coastal Range, eastern Taiwan, based on smaller foraminifera (I: Southern part). Proc. Geol. Soc. of China ,10, 64-76. Chang, L.S. (1968) A biostratigraphic study of the Tertiary in the Coastal Range, eastern Taiwan, based on smaller foraminifera (II: Northern part). Proc. Geol. Soc. of China ,11, 19-33. Chang, L. S. (1969) A biostratigraphic study of the Tertiary in the Coastal Range, eastern Taiwan, based on smaller foraminifera (Ⅲ: Middle Part). Proc. Geol. Soc. of China, 10, 89-101. Chen, R. F., Lin, C. W., Chen, Y. H., He, T. C. and Fei, L. Y.(2015) Detecting and characterizing active thrust fault and deep-seated landslides in dense forest areas of southern taiwan using airborne LiDAR DEM. Remote Sens. 7(11):15443-15466, doi:10.3390/rs71115443. Chen, W. H., Huang, C. Y., Lin, Y. J., Zhao, Q. H., Yan, Y., Chen, D. F., Zhang, X. C., Lan, Q., and Yu, M. M. (2015) Depleted deep South China Sea δ13C paleoceanographic events in response to tectonic evolution in Taiwan–Luzon Strait since Middle Miocene. Deep Sea Research Part II: Topical Studies in Oceanography, 122, 195-225, doi: 10.1016/j.dsr2.2015.02.005. Chen, W. H., Huang, C. Y., Yan, Y., Dilek, Y., Chen, D., Wang, M. H., Zhang, X., Lan, Q. and Yu, M.(2017)Stratigraphy and provenance of forearc sequences in the Lichi Mélange, Coastal Range: Geological records of the active Taiwan arc-continent collision. J. Geophys. Res. Solid Earth, 122, 7408–7436, doi: 10.1002/2017JB014378. Chen, W. S. (1988) Development of Deep-Sea Fan Systems in Coastal Range Basin, Eastern Taiwan: Science Reports of the National Taiwan University, ACTA Geologica Taiwanica, 26, 37-56 Chen, W. S. (1997a) Lithofacies analyses of the arc-related sequence in the Coastal Range, eastern Taiwan. J. Geol. Soc. China, 40, 313–338. Chen, W. S. (1997b) Mesoscopic structures developed in the Lichi Mélange during the arc-continent collision in the Taiwan region. J. Geol. Soc. China,40, 415-434. Chen, W. S., Yang, C. Y., Chen, S. T. and Huang, Y. C. (2020) New insights into Holocene marine terrace development caused by seismic and aseismic faulting in the Coastal Range, eastern Taiwan. Quat. Sci. Rev., 240, 106369. doi: 10.1016/j.quascirev.2020.106369. Chi, W. C., Chen, L., Liu, C. S. and Brookfield, M. (2014). Development of arc–continent collision mélanges: linking onshore geological and offshore geophysical observations of the Pliocene Lichi Mélange, southern Taiwan and northern Luzon arc, western Pacific. Tectonophysics, 636, 70–82, doi: 10.1016/j.tecto.2014.08.009. Horng, C. S. and Shea, K. S. (1996) Dating of the Plio-Pleistocene rapidly deposited sequence based on integrated magneto-biostratigraphy: a case study of the Madagida-Chi section, Coastal Range, eastern Taiwan. J. Geol. Soc. China, 39, 31-58. Horng, C. S. and Shea, K. S. (1997) Magnetobiostratigraphy of the MAWU-CHI section, Southern Coastal Range, eastern Taiwan. J. Geol. Soc. China, 40, 2, 339-362. Hsieh, M. L., Hogg. A., Song S. R., Kang S. C. and Chou C.Y. (2017) A mass-wasting dominated Quaternary mountain range, the Coastal Range in eastern Taiwan. Quat. Sci. Rev., 177, 276-298, doi: 10.1016/j.quascirev.2017.10.019. Hsu, T. L. (1976). The Lichi mélange in the Coastal Range framework. Bull. Geol. Surv. Taiwan, 25, 87-95. Huang, C. Y. (2010) Mechanism and consequence of forearc back-thrusting in formation of Lichi Melange in Coastal Range, eastern Taiwan. GSA, Tectonic Crossroads: Evolving Orogens of Eurasia-Africa-Arabia, Ankara, Turkey 2010, Abstract with Program, 85. Huang, C. Y., and Yuan, P. B. (1994) Stratigraphy of the Kangkou Limestone in the Coastal Range, Eastern Taiwan, J. Geol. Soc. China, 37(4), 585-605. Huang, C. Y., Chien, C. W., Yao, B. and Chang, C. P.(2008)The Lichi Mélange: a collision mélange formation along early arcward backthrusts during forearc basin closure, Taiwan arc-continent collision. In: Draut, A.E., Clift, P.D., Scholl, D.W. (Eds.), Formation and Applications of the Sedimentary Record in Arc Continent Collision Zone. Geol. Soc. Amer. Spec. Paper 436, 127–154. doi: 10.1130/ 2008.2436(06). Huang, C. Y., Yuan, P. B., Song, S. R., Lin, C. W., Wang, C. S., Chen, M. T., Shyu, C. T., and Karp, B. (1995) Tectonics of short-lived intra-arc basins in the arc-continent collision terrane of the Coastal Range, eastern Taiwan. Tectonics, 14(1), 19-38. Huang, C. Y., Chen, W. H., Wang, M. H., Lin, C. T., Yang, S., Li, X., Yu, M., Zhao, X., Yang, K. M., Liu, C. S., Hsieh, Y. H., Harrish, R.(2018) Juxtaposed sequence stratigraphy, temporal-spatial variations of sedimentation and development of modern-forming forearc Lichi Mélange in North Luzon Trough forearc basin onshore and offshore eastern Taiwan: An overview. Earth Sci. Rev. 182, 102–140, doi: 10.1016/j.earscirev.2018.01.015. Huang, C. Y., Yuan, P.B. and Tsao, S.J. (2012) Temporal and spatial records of active arc-continent collision in Taiwan. A synthesis. Geol. Soc. Am. Bull., 118(3-4), 274-288, doi:10.1130/B25527.1 Iwahashi, J. and Pike, R. J. (2007) Automated classifications of topography from DEMs by an unsupervised nested-means algorithm and a three-part geometric signature. Geomorphology, 86, 409-440. Lai, L. S. H, Dorsey, R. J., Horng, C. S., Chi, W. R., Shea, K. S. and Yen, J. Y. (2021) Polygenetic mélange in the retrowedge foredeep of an active arc-continent collision, Coastal Range of eastern Taiwan. Sedi. Geol., 418,105901 Lai, Y. M. and Song, S. R. (2013) The volcanoes of an oceanic arc from origin to destruction: a case from the northern Luzon Arc. J. Asian Earth Sci., 74, 0, 97-112. Lin, C. W., Liu, Y. C., Lai, W. C. and Cheng, W. H. (1999) Fault tectonics of the coastal range, eastern Taiwan. J. Geol. Soc. China., 42(3), 429-446. Lin, C. W., Lin, C. W., Tseng, C. M., Tseng, Y. H., Fei, L. Y., Hsieh, Y. C. and Tarolli, P. (2013) Recognition of large scale deep-seated landslides in forest areas of Taiwan using high resolution topography. J. Asian Earth Sci., 62, 389–400. Lo, P. C., Lo, W., Wang, T. T. and Hsieh, Y. C. (2021) Application of Geological Mapping Using Airborne-Based LiDAR DEM to Tunnel Engineering: Example of Dongao Tunnel in Northeastern Taiwan. Appl. Sci., 11(10), 4404. https://doi.org/10.3390/app1110440 Ooe, G. (1939) Geologic Map of Taiwan: Taito sheet. Government General of Taiwan, 861. Page, B. M. and Suppe, J. (1981) The pliocene Lichi Mélange of Taiwan: its plate-tectonic and olistostromal origin. Am. J. Sci. 281, 193–227. Prima, O. D. A., Echigo, A., Yokoyama, R. and Yoshida, T. (2006) Supervised landform classification of Northeast Honshu from DEM-derived thematic maps. Geomorphology, 78, 373-386. Raymond, L. A.(1984) Classification of mélanges. In: Raymond, L.A. (Ed.), Mélanges: Their Nature and Significance. Geol. Soc. Am., Special Paper 198, 7–20. Richard, M., Bellon, H., Maury, R. C., Barrier, E. and Juang, W. S. (1986) Miocene to recent calc-alkaline volcanism in eastern Taiwan: K-Ar ages and petrography. Tectonophysics, 125, 87-102. Song, S. R. and Lo, H. J., (2002) Litohfacies of volcanic rocks in the central Costal Range, eastern Taiwan: implications for island arc evolution. J. Asian Earth Sci., 21(1), 23-38, doi:10.1016 /S1367-9120(02)00003-2 Teng, L. S. (1979) Petrographical Study of the Neogene Sandstones of the Coastal Range, Eastern Taiwan (I. Northern Part)Science Reports of the National Taiwan University ACTA Geologica Taiwanica, 20, 129-156. Thomas, M. Y., Avouac, J. P., Gratier, J. P., and Lee, J. C. (2014). Lithological control on the deformation mechanism and the mode of fault slip on the Longitudinal Valley Fault, Taiwan. Tectonophysics, 632, 48-63, doi: 10.1016/j.tecto.2014.05.038. Ventura, G., Vilardo, G., Terranova, V. and Bellucci, S. E. (2011) Tracking and evolution of complex active landslides by multi-temporal airborne LiDAR data: The Montaguto landslide (Southern Italy). Remote Sens. Environ. 115 (12), doi:10.1016/j.rse.2011.07.007. Wang, C. S. (1976) The Lichi Formation of the Coastal Range and arc-continent collision in Eastern Taiwan., Bull. Geol. Surv. Taiwan, 25, 73-86. Wang, Y. (1966) Some geologic observations in the Coastal Range, eastern Taiwan, J. Geol. Soc. China., 9, 86-93. Yeh, C. H, Chan, Y. C., Chang, K. J., Lin, M. L. and Hsieh, Y. C. (2014) Derivation of strike and dip in sedimentary terrain using 3D image interpretation based on airbone LiDAR data. Terr. Atmos. Ocean. Sci., 25(6), 775-790, doi:10.3319/TAO.2014.07.02.01(TT) Yeh, C. H., Lin, M. L., Chan, Y. C., Chang, K. J. and Hsieh, Y. C. (2017) Dip-slope mapping of sedimentary terrain using polygon auto-tracing and airborne LiDAR topographic data. Eng. Geol., 222, 236-249, doi: 10.1016/j.enggeo.2017.04.009. Yen, T. P. (1969) The late Neogene formations of the Coastal Range, eastern Taiwan. Proc. Geol. Soc. China, 12, 81-87. | - |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/87179 | - |
dc.description.abstract | 海岸山脈是菲律賓海板塊與歐亞板塊弧陸碰撞作用下的產物,記錄了島弧火山從出生到死亡的歷史。其主要由火成岩及沉積岩組成,火成岩區地勢高聳、植被分佈茂密且野外觀察不易,前人的野外位態資料相較沉積岩區來得稀缺,進而對地質構造抱持不同見解。由此可見,海岸山脈火成岩區地質構造尚待後人釐清。此外,新一代地質圖製圖帶有不確定性,如何說明製圖的不確定性亦為本文欲解決的問題。本文研究區域為玉里地質圖幅以南的海岸山脈地質區,旨在利用空載光達產製的2米解析度數值地形解析研究區域內地質架構及歷史:將數值地形輸入ArcGIS Pro後,於三維環境藉由視角轉換繪製數值地形之構造線型,同時將地形根據層理地形特徵強弱分為四類。接著計算迴歸平面位態、實際至野外以UAV輔助查核,並輔以前人文獻,釐清研究範圍內地質架構的同時,補足都鑾山層位態資料。最終產製新一代海岸山脈南段五萬分之一地質圖及層理地形分級圖。繪製成果顯示,運用高解析度的數值地形進行三維判釋有助使火成岩與沉積岩的地層邊界更加精確。找出都鑾山層中斷層構造(如:成廣澳斷層、七里斷層、小馬斷層以及石厝溝斷層)的同時,使花東山斷層分佈的位置更加明確。並發現前人未曾報導過的羅山剪切帶、萬人山正斷層系統以及泰源盆地南端的大規模山崩。本研究以三維地形製圖解析海岸山脈南段地質構造,精進五萬分之一地質圖,提高製圖解析度;並將層理地形特徵根據強弱進行分級,初步說明了地形製圖的不確定性;而UAV輔助查核則獲取地勢高聳及遙遠處露頭資訊,使海岸山脈南段野外露頭資訊更為完整。研究成果將可作為未來地質研究及工程施作參考。 | zh_TW |
dc.description.abstract | The Coastal Range of Taiwan is a product of the arc continent collision between the Philippine Sea Plate and the Eurasian Plate, which records the history of island arc volcanoes from birth to death. Coastal Range is mainly composed of igneous rocks and sedimentary rocks. The igneous rock area has a high terrain, dense vegetation distribution, and field observation is not easy. Compared with the sedimentary rock area, field data within the igneous rock area is scarce, which lead to different views on the geologic structure. Geologic structures of igneous rock area in the Coastal Range have yet to be clarified. In addition, there are uncertainties of the new generation geological mapping, how the uncertainties to be explained is also a problem to be solved by this study. The research area of this study is the southern part of Coastal Range. This study aims to use the 2-meter resolution airborne LiDAR derived DEM to study the geologic structure and the history of the area. After inputting the DEM into ArcGIS Pro, this study delineated the structure lineament in the 3D environment through different perspectives, at the same time, ranking the terrain into four types according to the strength of the bedding topographic features. Calculaing the attitude data of the bedding regression plane then go to field to verify the delineated results. Supplemented by previous study, this study clarifies the geological structure within the research area, and to supplement the attitude data in the Tuluanshan Formation. Finally, a new generation of 1/50,000 geological map and bedding characteristic ranking map of the southern Coastal Range were produced. The mapping results show that using high-resolution DEM for 3D interpretation makes the stratigraphic boundaries between igneous and sedimentary rocks more precise. While finding out the fault structure in the Tuluanshan Formation (such as: Chengguang'ao fault, Qili fault, Xiaoma fault and Shicuogou fault), the location of the Huatungshan Fault distribution become clear. This study also discovered the Loshan shear zone, the Mt. Wanren normal fault system, and the large-scale landslide at the southern part of the Taiyuan Basin, which have not been reported before. In this study, 3D topographic mapping is used to analyze the geologic structure of the southern Coastal Range, and the 1/50,000 geologic map is refined to improve the mapping resolution, and the bedding topographic characteristics are ranked according to their strength, which preliminarily explains the uncertainty of topographic mapping. The UAV-assisted verification obtains information on high-lying terrain and outcrops in distant places, making the information on outcrops of the southern Coastal Range more complete. The research results can be used as a reference for future geologic research and civil engineering. | en |
dc.description.provenance | Submitted by admin ntu (admin@lib.ntu.edu.tw) on 2023-05-18T16:12:33Z No. of bitstreams: 0 | en |
dc.description.provenance | Made available in DSpace on 2023-05-18T16:12:33Z (GMT). No. of bitstreams: 0 | en |
dc.description.tableofcontents | 口試委員審定書 i
誌謝 ii 中文摘要 iii Abstract iv 目錄 vi 圖目錄 xii 表目錄 xviii 第一章、 緒論 1 1.1 研究動機及目的 1 第二章、 研究區域及文獻回顧 4 2.1 研究區域 4 2.2 地層 2 2.3 構造 8 2.4 高解析度數值高程模型 11 2.5 新一代地質圖 13 2.6 層理地形分級 14 第三章、 研究方法 16 3.1 使用軟體 17 3.2 數值高程模型 18 3.3 相關圖層計算及套色 20 3.3.1 層理地形分級 23 3.4 構造線型判釋及繪製 25 3.4.1 打點系統 26 3.4.2 火成岩區岩層線繪製 27 3.4.3 沉積岩區岩層線繪製 29 3.4.4 斷層線型 31 3.4.5 沉積岩褶皺軸 32 3.4.6 地層邊界線 33 3.4.7 沖積層及階地堆積層邊界 34 3.4.8 外來岩塊圈繪 35 3.5 構造線型位態計算 36 3.6 野外查核 36 3.6.1 UAV任務規劃 38 3.6.2 室內成果核對 38 3.7 地質圖繪製 40 3.7.1 剖面繪製 42 3.7.2 位態數值放置工具箱設計 43 第四章、 研究成果 46 4.1 海岸山脈南段地質圖 48 4.2 地層地形特徵 54 4.2.1 都鑾山層 54 4.2.2 港口石灰岩 54 4.2.3 蕃薯寮層與八里灣層 54 4.2.4 利吉層 55 4.2.5 平緩坡度條帶(Gentle Slope Belt) 56 4.3 地層分段 58 4.3.1 成功盆地八里灣層地層分段 59 4.3.2 泰源盆地地層分段 61 4.3.3 台東盆地八里灣層地層分段 65 4.3.4 東河地區八里灣層 66 4.3.5 樂合盆地八里灣層 67 4.3.6 成功地區都鑾山層地層分段 69 4.3.7 都蘭地區都鑾山層地層分段 71 4.3.8 富里地區都鑾山層 73 4.3.9 東河地區都鑾山層 76 4.3.10 德高地區都鑾山層 77 4.3.11 富里地區蕃薯寮層 78 4.3.12 鸞山地區蕃薯寮層 79 4.4 構造特徵描述 81 4.4.1 泰源向斜 82 4.4.2 都鑾山背斜 83 4.4.3 石厝溝斷層 84 4.4.4 九芎嶺斷層 84 4.4.5 成廣澳斷層 85 4.4.6 長濱斷層 86 4.4.7 都蘭斷層 87 4.4.8 都鑾山斷層 88 4.4.9 花東山斷層 89 4.4.10 萬人山正斷層系統 91 4.4.11 永豐斷層 91 4.4.12 大馬斷層 92 4.4.13 七里斷層 93 4.4.14 松林斷層 93 4.4.15 卑南山斷層與利吉斷層 97 4.4.16 杉原斷層 98 4.4.17 羅山剪切帶 98 4.4.18 小馬斷層 98 4.4.19 加只來斷層 102 4.4.20 吳江村斷層 103 4.4.21 烏心石斷層 104 4.5 層理地形分級 105 4.5.1 第一類層理地形特徵 105 4.5.2 第二類層理地形特徵 106 4.5.3 第三類層理地形特徵 107 4.5.4 第四類 107 4.6 野外查核 108 4.6.1 成功地區 109 4.6.2 泰源地區 110 4.6.3 東河地區 114 4.6.4 都蘭地區 115 4.6.5 富里地區 116 4.6.6 關山地區 117 第五章、 討論 118 5.1 製圖技術與限制 118 5.1.1 利於製圖及展示之軟體及套件 118 5.1.2 地形分級成果處理方式 119 5.1.3 倒懸地形的影響 120 5.1.4 與層理面接近的坡面(順向坡) 122 5.1.5 階地堆積層與人為開發地 123 5.1.6 地形特徵相似的地層 126 5.1.7 UAV輔助野外查核 127 5.1.8 海岸山脈濁流岩vs西部麓山帶沉積岩 128 5.1.9 坡度平緩處的繪製及圈繪方式 130 5.2 海岸山脈南段地質構造 132 5.2.1 樂合盆地構造 132 5.2.2 都鑾山層傾向急遽變化處的斷層作用 135 5.2.3 泰源向斜兩翼厚度差異 137 5.2.4 大莊越山倒轉岩層 137 5.2.5 萬人山正斷層系統 137 5.2.6 花東山斷層分佈 139 5.2.7 羅山剪切帶 141 5.2.8 加只來山節理系統 144 5.2.9 長濱斷層、都蘭斷層與九芎嶺斷層 148 5.2.10 海岸山脈南端利吉層與八里灣層接觸關係 151 5.3 地層與地形特徵 154 5.3.1 火成岩岩層線意義 154 5.3.2 成廣澳火山近火山口相 155 5.3.3 地層邊界修正 157 5.3.4 崩移的地層 159 5.3.5 利吉層中的外來岩塊 160 5.3.6 泰源盆地南端地層 163 5.3.7 木坑溪部分受剪的岩層 166 5.3.8 多組方向性強的線型 168 5.3.9 山崩與深層重力變形 170 5.3.10 萬人山可能的形成機制 172 5.4 建議補充調查區域 173 第六章、 結論 175 參考文獻 176 附錄一、野外查核地點及照片 187 附錄二、前人地質圖圖例 239 | - |
dc.language.iso | zh_TW | - |
dc.title | 應用空載光達數值地形解析海岸山脈南段地質構造 | zh_TW |
dc.title | Using airborne LiDAR DEM for interpreting geologic structures in the southern Coastal Range | en |
dc.type | Thesis | - |
dc.date.schoolyear | 111-1 | - |
dc.description.degree | 碩士 | - |
dc.contributor.coadvisor | 胡植慶 | zh_TW |
dc.contributor.coadvisor | Jyr-Ching Hu | en |
dc.contributor.oralexamcommittee | 王泰典;陳致同;葉恩肇 | zh_TW |
dc.contributor.oralexamcommittee | Tai-Tien Wang;Chih-Tung Chen;En-Chao Yeh | en |
dc.subject.keyword | 海岸山脈南段,五萬分之一地質圖,數值高程模型,光達,三維製圖, | zh_TW |
dc.subject.keyword | southern Coastal Range,1/50000 geologic map,DEM,LiDAR,3D geologic mapping, | en |
dc.relation.page | 241 | - |
dc.identifier.doi | 10.6342/NTU202300392 | - |
dc.rights.note | 同意授權(限校園內公開) | - |
dc.date.accepted | 2023-02-13 | - |
dc.contributor.author-college | 理學院 | - |
dc.contributor.author-dept | 地質科學系 | - |
顯示於系所單位: | 地質科學系 |
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