位於中央山脈與海岸山脈之間的台灣東部縱谷位於是歐亞大陸板塊與菲律賓海板塊之縫合帶，其南段為二者初始聚合之處地下構造甚為複雜。由於台東縱谷內之構造大致呈現南北走向，然而至南段卑南山地區，構造發育分散並轉為向東南出海，東部縱谷南端構造及卑南山地區的構造地形演化至今仍是值得探討的議題。
本研究使用衛星大地測量及野外量測卑南山礫岩和台東市區鯉魚山的層態，探討台東縱谷南端的構造活動。永久散射體差分干涉法 (Persistent Scatterer Interferometric Synthetic Aperture Rader, PSI)為較新的衛星大地測量法，傳統DInSAR技術受限由於山區植被，容易導致測量誤差，造成地表監測的不準確性，而永久散射體差分干涉可以解決空間性、時間性誤差。本研究測量地區雖有稻田、茂密樹木，但測量結果證明永久散射體差分干涉仍可獲得地表變形資訊。
利用永久散射體差分干涉法監測所得的地表變形資訊配合野外實際量測的層態與構造結果進一步做比對，可將東部縱谷南端卑南山南冀延伸至卑南溪口及卑南山一帶的活動構造，做完整的探討與推論。

Located between The Central Range and Coastal Range, the Longitudinal Valley is the convergent boundary of Eurasian Plate and The Philippine Sea Plate. The southerly side is where the convergence happened at the beginning stage. The active tectonic underground is beyond complication. The Longitudinal Valley is linear, narrow, and vertical structured. However, the southern tip of Longitudinal Valley is scattered structured and turned to the south-east dripping to the Pacific Ocean. More investigations are needed to study this intricate tectonic issue related to the structure of Pinanshan and the southern tip of the Longitudinal Valley.
The work based on satellite imagery measured and field study of the fault formation of Pinanshan and LiYuShan located in Taitung city. Persistent Scatterer Interferometric Synthetic Aperture Rader (PSI) is a new meothod of satellite imagery measurement. The traditional method of measurement, DInSAR is comparatively easily to lead to inaccuracy because of the limitation of the technology. PSI, in the other hand, provides a way to get away for, the inaccuracy of space and time. Though there are some distracters, such as forests and rice paddy, founded in the region which has been measured. The result still proves that the PSI a effective method to gain the transformation information on the surface to the earth.
With the use of Persistent Scatterer Interferometric Synthetic Aperture Rader (PSI) and the data acquired in the field research, the author compared the tectonic transformation monitored by PSI to the result of the data gained from the field research. The author provides a thorough discussion and inference of the exact nature of the fault tectonics in the southern tip of Longitudinal Valley extended to the Pinanshan as well as the Pinan region.

王鑫，1980。台灣的地形景觀， 台北： 渡假出版社。
何春蓀，1975。台灣地質概論— 台灣地質圖說明書， 台北： 經濟部中央
地質調查所。
何春蓀，1982。台灣地體構造的演變—台灣地體構造圖說明書，經濟部出版，台
北，153頁。
林明德、蔡義本，1981。台灣-呂宋地區之大地構造，中央研究院地球科學
研究所集刊，第一卷，51-82。
林俊全，1991。台灣東部海岸山脈的新構造運動模式， 中國地理學會會
刊， 19： 43-55。
林啟文、張徽正、盧詩丁、石同生、黃文正，2000，台灣活動斷層概論－五十萬
分之一臺灣活動斷層分布圖說明書，第二版。經濟部中央地質調查所特
刊，第十三號，共122頁。
林啟文，石瑞銓，林燕慧，2004，台東縱谷南段的活動斷層特性研究。經濟部中
央地質調查所特刊，第十五號，161-174。
紀文榮，1981。台灣利吉層與墾丁層內之超微化石及其在地質構造上之意義：地
質，第四卷，第一期，99-144。
紀權窅，2006。南段花東縱谷之新期構造研究－利吉斷層與鹿野斷層的活動特
性。國立台灣大學地質科學所碩士論文，共84 頁。
畢慶昌，1969。俯衝運動在台灣地體構成中的作用。台灣省地質調查所彙刊，第
二十號，1-4。
畢慶昌，1972。深海槽溝在台灣與呂宋之間的雙軌構造，中國地質學會會
刊，第十五號，65-75。
畢慶昌，1974。從剛塊構造申論台灣的區域成礦作用，台灣省地質調查所
彙刊，第二十四號，139-156。
徐鐵良，1976。台灣東部縱谷的新構造。台灣省地質調查所彙刊，第二十五號，
53-62。
張麗旭，1972。台灣中央山脈畢祿山階與盧山階間之間隙及N礫岩。中國地質學會彙刊，第十五號，93-98。
張中白、王皓正、陳錕山，2003。地震地質調查及活動斷層資料庫建置計畫－地殼變形研究計畫。經濟部中央地質調查所報告第92-10號。
陳文山，1988。台灣海岸山脈沉積盆地之演化及其在地體構造上之意義。國立台
灣大學地質研究所博士論文，304頁。
陳文山、王源，1996。台灣東部海岸山脈地質， 台北： 經濟部中央地質調查
所。
陳文山，2002。車籠埔斷層的古地震事件與地質的意義。臺灣之活動斷層與地震
災害研討會，83-88。
張徽正、林啓文、陳勉銘、盧詩丁 (1998) 臺灣活動斷層概論：五十萬分之一臺
灣活動斷層分布圖說明書。經濟部中央地質調查所特刊，第十號，共103
頁。
游明聖，1996。台東縱谷斷層中之橫移斷層特徵，地質，14（1）：121-147。
游明聖，1996。台東卑南山地區的新期構造運動， 中國地質學會85 年年會暨東
亞岩石圈學術研討會摘要，273-277。
楊榮堃，1990。台灣台東縱谷南段重力與地質之研究，博士論文，中央大學地球
物理研究所。
鄧屬予，1980。蕃薯寮層的岩性與來源。中國地質學會彙刊，第二十三號，
118-129。
鄧屬予，1997。台灣的沈積岩， 台北： 經濟部中央地質調查所。
Biq, C. C., 1965. The East Taiwan Rift: Petroleum Geology of Taiwan, 9, 79-106.
Biq, C. C., 1971. Comparison of melange tectonics in Taiwan and in some other mountain belts, Petrol. Geol. Taiwan, 9, 79-106.
Biq, C. C., 1972a. Dual-trench structure in the Taiwan-Luzon region, Proc. Geol. Soc. China, 15, 65-75.
Biq, C. C., 1972b. Weatern Taiwan thrusts, active or inactive ? Acta Geol Taiwan, 15, 69-81
Barrier, E., Angelier J., Chu, H. T., Teng, L. S., 1982. Tectonic analysis of
compressional structure in an active collision zone: the deformation of the
Pinanshan conglomerates, eastern Taiwan: Proceedings of the Geological Society of China, 25, 123-138.
Barrier, E., Angelier J., 1986. Active collision in eastern Taiwan: the Coastal Range:
Memoir of the Geological Society of China, 7, 135-159.
Chai, B. H. T.,1972. Structure and tectonic evolution of Taiwan, Am. Jour. Sci, 272, 389-422.
Chang, L. S., Hu, C. C., 1981. Gravity and magnetic anomalies of Taiwan and their tectonic implication, Mem. Geol. Soc. China, 4, 121-142.
Chang, C.P., Angelier, J. and Huang, C.Y., 2000. Origin and evolution of a melange: the active plate boundary and suture zone of the Longitudinal Valley, Taiwan. Tectonophysics, 325, 43-62.
Chen , J. S, 1976. The analysis and design of refraction and reflection seismic survey of the Taitung area. Petro Geol. Taiwan, 13, 225-246.
Chen, H.Y, Y.J. Hsu, J.C. Lee, S.B. Yu, L.C. Kuo, Y.L. Jiang, C.C. Liu and C.S. Tsai, 2009. Coseismic Displacements and Slip Distribution from GPS and Leveling Observations for the 2006 Peinan Earthquake (Mw 6.1) in Southeastern Taiwan, Earth Planets Space, 61, 1-20. IESAS1311
Ferretti, A., Prati, C. and Rocca, F., 2001. Permanent scatterers in SAR interferometry, IEEE Trans. on Geosci. and Remote Sensing, 39 (1), 8 – 20.
Hoffmann, J., 2003. The application of satellite radar interferometry to the study of
land subsidence over developed aquifer systems, Ph.D. thesis, Stanford
University.
Hooper, A., Zebker, H., Segall, P. and Kampes, B., 2004.A new method for
measuring deformation on volcanoes and other natural terrains using InSAR
persistent scatterers. Geophys. Res. Letter, 31, L23611,
doi:10.1029/2004GL021737.
Hooper, A., Segall, P. and Zebker, H., 2007. Persistent scatterer interferometric
synthetic aperture radar for crustal deformation analysis, with application to
Volcan Alcedo, Galapagos. J. Geophys. Res., 112, B07407,
doi:10.1029/2006JB004763.
Hsu, T. L., 1956. Geology of the Coastal Range, eastern Taiwan: Bull. Geol. Surv.
Taiwan, 8, 39-63.
Hsu, T. L., 1962. Recent faul t ing in the Longitudinal Valley of eastern Taiwan, Mem. Geol. Soc. China , 1:95-102.
Hu, C. C., Chen, W. S., 1986. Gravity and magnetic anomalies of eastern Taiwan, Mem. Geol. Soc. China, 7, 341-352.
Karig, D. E., 1973. Plate convergence between the Philippine and the Ryukyu Island,
Marine Geology, 76, 2542-2561.
Lee, T. Q., 1983. Focal mechanism solutions and their tectonic implications in Taiwan region, Bull. Inst. Earth Sci. Academia Sinica, 3, 37-54.
Lee, J. C., Angelier, J., Chu, H. T., Yu, S. B., and Hu, J. C., 1998. Plate- boundary strain partitioning along the sinistral collision suture of the Philippine and Eurasian plates: analysis of geodetic data and geological observation: Tectonics, 17, 859-871.
Lin, C. H., Yeh, Y. H., Tsai, Y. B., 1985. Determination of regional principal stress directions in Taiwan form fault plane solutions, Bull .Inst. Earth Sci. Academia Sinica, 5, 67-85.
Liou, J. G., Suppe, J. and Ernst, W. G., 1977. Conglomerates and pebbly mudstonesin the Lichi Mélange, eastern Taiwan. Mem. Geol. Soc. China, no. 2, p. 115-128.
Shyu, J.B.H., Sieh, K., Chen,Y.G., Chuang, R.Y., Wang, Y. and Chung, L.H., 2008. Geomorphology of the southernmost Longitudinal Valley fault: Implications for evolution of the active suture of eastern Taiwan, Tectonics, 27, TC1019, doi:10.1029/2006TC002060.
Teng, L. S., Chen, W. C., Wang Y., Sung, S. R., Lo, H. J., 1988. Toward a comprehensive stratigraphic system of coastal range, eastern Taiwan, Acta. Geol. Taiwan, 26, 19-35.
Teng, L. S., 1990. Geotectonic ecolution of late Cenozoic arc-continent collision in Taiwan, Tectonophy. 183, 57-76.
Tsai, Y. B., Teng, T. L., Chiu, J. M., Liu, H. L., 1977. Tectonic implications of recent seismicity in the Taiwan region, Mem. Geol. Soc. China, 2, 13-41.
Wu, F. T., Lu, C. P., 1976. Recent tectonics of Taiwan, Bull. Geol. Surv. Taiwan, 25, 97-111.(in Chinese)
Yen, T. P., 1954. The gneisses of Taiwan, Bull. Geol. Surv. Taiwan, 5, 1-100.
Yen, T. P., 1960. A stratigraphic study of the Tananao Schist in northern Taiwan, TAICRUST workshop proc., Taipei, Taiwan, 49-62.
Yen, T. P., 1963. The metamorphic belts within the Tananao Schist terrain of Taiwan, Proc. Geol. Soc. China, 6, 72-74.
Yu, S. B., Tsai, Y. B.,1982. A study of microseismicity and crustal deformation of the Kuanfu-Fuli area in E. Taiwan, Bull. Inst. Earth Sci., Academia Sinica, 2, 1-18.
Yu, S. B., Liu, C. C., 1989. Fault creep on the central segment of the Longitudal Valley fault, eastern Taiwan , Proc. Geol. Soc. China, 32, 209-231.
Yu, S. B., Jackson, D. D., Yu, G. K., Liu, C. C., 1990. Dislocation midel for crustal deformation in the Longitudal Valley area, eastern Taiwan, Techtonophys., 183, 97-109.
Yu, S. B., Yu, G. K., Kuo, L. C., Lee, C., 1992. Crustal deformation in the southern
Longitudinal Valley area, eastern Taiwan: Jour. Geol. Soc. China, 35, 219-230.
Yu, S. B., Chen, H. Y., Kuo, L.C., 1997, Velocity field of GPS stations in the Taiwan area: Tectonophysics, v. 274, 41-59.