變率為0.15-2.32 µstrain/yr,最小主軸應變率為-2.24-0.65 µstrain/yr。且主軸應 變伸張方向,由西向東的變化從西北-東南逐漸轉成接近南北走向,故其伸張 µradian/yr及0.12-0.71 µradian/yr,宜蘭平原內部及牛鬥地區則為逆時針旋轉,
分別為-0.90至-0.02 µradian/yr及-0.52至-0.09 µradian/yr。
5. 藉由速度場速度向量的不連續及地質資料,推測宜蘭平原上可能有四條主要 的活動構造,由北而南分別為牛鬥斷層、坑四斷層、濁水斷層及三星斷層等 活動構造。
6. 綜合速度剖面及剪應變之結果,以蘭陽溪為界,蘭陽溪北側平原內為一系列
正斷層系統,唯坑四斷層帶有右移之分量。蘭陽溪南側則以正斷層系統帶有 左移分量的橫移伸張變形為主。
7. 近期台灣東北地區受到沖繩海槽張裂之影響,造成早期造山時呈東北-西南走 向之山脈,在受力彎曲時發生層間的左移滑動,此一構造行為即沿著地質弱 帶發生,使得觀測到宜蘭平原南邊之正斷層帶有左移的分量。
8. 由速度剖面分析得知,蘭陽溪兩側之南北方向速度分量差異很大,南側之速 度分量大於北側之速度分量,由此可知沖繩海槽為不對稱之弧後張裂,且南 側之張裂速度較北側快。
9. 宜蘭平原觀察到速度場旋轉以及伸張應變旋轉之現象,是由於宜蘭平原西側 同時受到菲律賓板塊的擠壓應力及琉球海溝隱沒後退所產生之伸張應力,形 成了西北-東南之伸張方向之橫移壓縮環境;而平原東側則受到沖繩海槽張裂 作用向南延伸之影響大於板塊碰撞之擠壓應力,因而轉為南北方向之伸張應 變,因而轉為東北-西南或南北方向之橫移伸張變形或伸張變形之模式。
參考文獻
Altamimi, Z., Sillard, P. & Boucher, C. 2002. ITRF2000: A new release of the International Terrestrial Reference Frame for earth science applications. J.
Geophys. Res.107(B10), 2214, doi:10.1029/2001JB000561.
Angelier, J. 1986. Perface. Geodynamics of the Eurasia-Philippine Sea plate boundary.
Spec. Issue. Tectonophysics125, IX-X.
Angelier, J., Chang, T.-Y., Hu, J.-C., Chang, C.-P., Siame, L., Lee, J.-C., Deffontaines, B., Chu, H.-T., & Lu, C.-Y. 2008. Does extrusion occurs at both tips of the Taiwan collision belt? Insights from active deformation studies in the Ilan Plain and Pingtung Plain regions. Tectonophysics, doi: 10.1016/j.tecto.2007.11.015.
Biq, C.-C. 1971. Some aspects of post-orogenic block tectonics in Taiwan: Recent crustal movements. Royal Soc. New Zealand Bull. 9, 19-24.
Chan, Y.-C., Chen, R.-F., Lee, J.-C., Chang, K.-J., Hsieh, Y.-C. & Tsao, S.-J. 2008.
Active normal faulting revealed by the LiDAR DTM in the mountainous area, north of the Lanyang plain, Taiwan. 2008 Annual Conference of Geological Society of China , Tainan, Taiwan.
Ching, K.-E. 2007. Kinematics of Taiwan Collision Zone from GPS Observations.
Doctoral thesis, National Cheng Kung University, Tainan, Taiwan, 102 pp.
Hou, C.-S., Hu, J.-C., Ching, K.-E., Chen, Y.-G., Chen, C.-L., Cheng, L.-W., Tang, C.-L., Huang, S.-H. & Lo, C.-H., 2008. The crustal deformation of the Ilan Plain acted as a westernmost extension of the Okinawa Trough. Tectonophysics, doi:
10.1016/j.tecto.2007.11.022.
Hu, J.-C., Angelier, J., Lee, J.-C., Chu, H.-T. & Byrne, D. 1996. Kinematics of convergence, deformation and stress distribution in the Taiwan collision area: 2-D finite-element numerical modeling. Tectonophysics255(3-4), 243-268.
Hu, J.-C., Yu, S.-B., Chu, H.-T. & Angelier, J. 2002. Transition tectonics of northern Taiwan induced by convergence and trench retreat. Geol. Soc. Am. Special Paper 358, 149-162.
Hugentobler, U., Schaer, S. & Fridez, P. 2001. Bernese GPS Software Version 4.2.
Astronomical Institute, University of Berne, 515 pp.
Kao, H., Shen, S.-S. J. & Ma, K.-F. 1998. Transition from oblique subduction to collision: Earthquakes in the southernmost Ryukyu arc-Taiwan region. J. Geophys.
Res.103, 7211-7229.
Lee, T.-Q., 1993. Preliminary paleomagnetic study on lake sediments at Yuanshan, Ilan, northeastern Taiwan. J. Geol. Soc. China36(4), 419-436.
Liang, W.-T., Lee, J.-C. & Kuo, B.-Y. 2005. Left-lateral strike-slip faulting in Ilan:
Lateral extrusion at the transition between Taiwan mountain range and Okinawa Through. Geodynamics and Environment in East Asia International Conference &
5th Taiwan-France Earth Science Symposium, 100-103.
Lin, K.-C, Ching, K.-E., Hu, J.-C., Yu, T.-T., & Rau, R.-J. 2006. Current crustal deformation and strain rate in Taiwan deduced from continuous GPS measurements. EGU06-A-07160, G11/GD17-1TH2P-0522.
Liu, C.-C. 1995. The Ilan plain and the southwestward extending Okinawa Trough. J.
Geol. Soc. China38, 229-242.
Lu, C.-Y., Angelier, J., Chu, H.-T. & Lee, J.-C. 1995. Contractional, transcurrent, rotational and extensional tectonics: Examples from Northern Taiwan.
Tectonophysics256(1-3), 129-146.
Mallet, J. L. 1989. Discrete smooth interpolation. ACM transactions on Graphics 8, 121-144.
Nakamura, M. 2004. Crustal deformation in the central and southern Ryukyu Arc estimated from GPS data. Earth Planet. Sci. Lett.217, 389-398.
Nishimura, S., Hashimoto, M. & Ando, M. 2004. A rigid block rotation model for the GPS derived velocity field along the Ryukyu arc. Phys. Earth Planet. Inter.
142(3-4), 185-203.
Prescott, W. H., Savage, J. C. & Kinoshita, W. T. 1979. Strain accumulation rates in the western United-States between 1970 and 1978. J. Geophys. Res. 84(10), 5423-5435.
Rau, R.-J., Ching, K.-E., Hu, J.-C. and Lee, J.-C. 2008. Crustal deformation and block kinematics in transition from arc-continent collision to subduction: GPS measurements in northern Taiwan, 1995-2005. J. Geophys. Res., doi:10.1029/2007JB005414.
Sagiya, T., Miyazaki, S. & Tada, T. 2000. Continuous GPS array and present-day crustal deformation of Japan. Pure Appl. Geophys.157(11-12), 2303-2322.
Segall, P. & Davis, J. L. 1997. GPS Applications for geodynamics and earthquake studies. Annu. Rev. Earth Planet. Sci.,25, 301-336.
Shen, Z.-K., Jackson, D. D. & Ge, B. X. 1996. Crustal deformation across and beyond the Los Angeles basin from geodetic measurements. J. Geophys. Res. 101(B12), 27957-27980.
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.
110(B08402), doi: 10.1029/2004JB003251.
Sibuet, J.-C., Deffontaines, B., Hsu, S.-K., Thareau, N., Le Formal, J.-P. & Liu, C.-S.
1998. Okinawa trough backarc basin: Early tectonic and magmatic evolution. J.
Geophys. Res.103(B12), 30245-30267.
Suppe, J. 1984. Kinematics of arc-continental collision, flipping of subduction, and back-arc spreading near Taiwan. Mem. Geol. Soc. China6, 21-33.
Tabei, T. & Amin, W. L. 2002. Common-mode errors in the GPS coordinates time series. Application of spatial filtering technique. J. Geod. Soc. Japan48, 229-241.
Teng, L. S. 1992. Geotectonic evolution of Tertiary continental margin basins of Taiwan. Petrol. Geol. Taiwan27, 1-19.
Teng, L. S. 1996. Extensional collapse of the northern Taiwan mountain belt. Geology 24(10), 949-952.
Teng, L. S. & Lee, C.-T. 1996. Geomechanical appraisal of seismogenic faults in northeast Taiwan. J. Geol. Soc. China39(2), 125-142.
Teng, L. S., Lee, C.-T., Tsai, Y.-B., & Hsiao, L.-Y. 2000. Slab breakoff as a mechanism for flipping of subduction polarity in Taiwan. Geology28, 155-158.
Thatcher, W. 2003. GPS constraints on the kinematics of continental deformation. Int.
Geol. Rev. 45(3), 191-212.
Thomas, A. L. 1993. Poly3D: A three-dimensional, polygonal element, displacement discontinuity boundary element computer program with applications to fractures, faults, and cavities in the Earth’s crust. Unpublished Master Thesis, Geology Department, Stanford University, 52p.
Tsai, Y.-B., Feng, C.-C., Chiu, J.-M., & Liaw, H.-B. 1975. Correlation between microearthquakes and geology fault in the Hsintien-Ilan area, Taiwan. Petrol. Geol.
Taiwan12, 149-167.
Wallace, L. M., McCaffrey, R., Beavan, J. & Ellis, S. 2005. Rapid microplate rotations and backarc rifting at the transition between collision and subduction. Geology33, 857-860.
Wang, W.-H. & Chen, C.-H. 1990. The volcanology and fission track age dating of pyroclastic deposits in Tatun volcano group. Acta Geol. Taiwanica28, 1-30.
Ward, S. N. 1994. A multidisciplinary approach to seismic hazard in southern California. Bull. Seismol. Soc. Am.84(5), 1293-1309.
Ward, S. N. 1998. On the consistency of earthquake moment rates, geological fault data, and space geodetic strain: The United States. Geophys. J. Int.134(1), 172-186.
Wdowinski, S., Bock, Y., Zhang, J., Fang, P. & Genrich, J. 1997. Southern California Permanent GPS Geodetic Array: Spatial filtering of daily positions for estimating coseismic and postseismic displacements induced by the 1992 Landers earthquake.
J. Geophys. Res. 102(B8), 18057-18070.
Wu, F. T., 1978. Recent tectonics of Taiwan. J. Phys. Earth 26, Suppl. S265-S299.
Wu, Y.-M., Chang, C.-H., Zhao, L., Teng, T.-L. & Nakamura, M. 2008a. A comprehensive relocation of earthquakes in Taiwan from 1991 to 2005. Bull.
Seismol. Soc. Am, 98(3), 1471-1481, doi: 10.1785/0120070166.
Wu, Y.-M., Zhao, L., Chang, C.-H., & Hsu, Y.-J. 2008b. Focal-mechanism determination in Taiwan by genetic algorithm. Bull. Seismol. Soc. Am. 98(2), 651-661, doi: 10.1785/0120070115.
Yeh, Y.-H., Lin, C.-H. & Roecker, S. W. 1989. A study of upper crustal structures beneath northeastern Taiwan: Possible evidence of the western extension of Okinawa Trough. Proc. Geol. Soc.China32(2), 139-156.
Yu, S.-B. & Tsai, Y.-B. 1979. Geomagnetic anomalies of the Ilan Plain. Petrol. Geol.
Taiwan16, 19-27.
Yu, S.-B. 1990. Establishing a GPS network for studying crustal deformation in the Taiwan area. Proc. Second Int. Symp. on Precise Position with GPS, Ottawa, Canada, 556-571.
Yu, S.-B., Chen, H.-Y. & Kuo, L.-C. 1997. Velocity field of GPS stations in the Taiwan area. Tectonophysics 274(1-3), 41-59.
Yu, S.-B., Kuo, L.-C., Punongbayan, R. S. & Ramos, E. G. 1999. GPS observation of crustal deformation in the Taiwan-Luzon region. Geophys. Res. Lett. 26(7), 923-926.
Zang, S.-X., Chen, Q.-Y., Ning, J.-Y., Shen, Z.-K. & Liu, Y.-G. 2002. Motion of the Philippine Sea plate consistent with the NUVEL-1A model. Geophys. J. Int.150(3), 809-819.
江新春(1976)宜蘭平原之震測。礦業技術第十四卷,第六期,第215-221頁。
蔡旻穎(2007)台灣GPS連續觀測站坐標時間序列分析方法研究。國立成功大學地 球科學系碩士論文,共97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154-161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 學會九十二年年會論文集,第119頁。
謝孟龍、賴慈華、吳樂群、陳文山(2006)台灣山脈晚冰期及後冰期侵蝕速率是 否不同?-曾文溪及蘭陽溪平原岩芯紀錄的檢視。第十一屆「台灣之第四紀」
研討會論文集,第53-57頁。
饒瑞鈞、余致義、洪日豪、胡植慶、李建成、詹瑜璋、許麗文(2006)地震地質 調查及活動斷層資料庫建置計畫-活動斷層監測系統計畫總報告。經濟部中央 地質調查所,共234頁。
附錄 A
Station Lon Lat VE VN SE SN V Azi
附錄 B
宜蘭地區內插點之應變率、旋轉率、面膨脹率以及剪應變率。
Lon Lat Eps1 Eps1(sig) Eps2 Eps2(sig) Theta The.(sig) Rotation Rot.(sig) Dilatation Dila.(sig) Gamma Gam.(sig) ( o ) ( o ) (strain/yr) (strain/yr) (strain/yr) (strain/yr) ( o ) ( o ) (radian/yr) (radian/yr) (strain/yr) (strain/yr) (strain/yr) (strain/yr) 121.78 24.53 2.32E-07 1.31E-07 -4.49E-07 1.92E-07 15.97 13.12 7.12E-07 1.72E-07 -2.18E-07 2.09E-07 6.81E-07 1.99E-07 121.81 24.53 2.57E-07 1.01E-07 -6.95E-07 1.12E-07 12.06 7.31 5.83E-07 1.29E-07 -4.38E-07 1.37E-07 9.53E-07 1.36E-07 121.84 24.53 2.47E-07 1.00E-07 -8.18E-07 1.14E-07 15.04 5.89 5.28E-07 1.20E-07 -5.71E-07 1.35E-07 1.07E-06 1.31E-07 121.54 24.56 6.66E-07 1.16E-07 -1.38E-07 8.67E-08 -55.62 4.93 -1.26E-07 7.02E-08 5.28E-07 1.49E-07 8.04E-07 8.48E-08 121.57 24.56 1.18E-06 1.68E-07 -8.45E-08 1.44E-07 -50.18 4.96 -1.47E-07 1.10E-07 1.10E-06 2.23E-07 1.27E-06 1.15E-07 121.75 24.56 1.14E-06 2.42E-07 -4.80E-07 1.18E-07 -29.04 4.95 3.10E-07 8.72E-08 6.57E-07 3.11E-07 1.62E-06 1.80E-07 121.81 24.56 1.99E-07 2.02E-07 -6.22E-07 1.55E-07 10.06 11.08 4.32E-07 1.63E-07 -4.23E-07 2.49E-07 8.21E-07 2.41E-07 121.84 24.56 1.83E-07 2.17E-07 -8.23E-07 1.96E-07 15.85 9.74 3.49E-07 1.82E-07 -6.40E-07 2.80E-07 1.01E-06 2.56E-07 121.51 24.59 1.46E-07 2.85E-08 -1.04E-06 2.19E-08 69.97 0.56 -5.13E-07 1.80E-08 -8.98E-07 3.60E-08 1.19E-06 2.99E-08 121.54 24.59 1.50E-07 3.67E-08 -6.29E-07 2.52E-08 77.03 0.72 -3.99E-07 2.22E-08 -4.79E-07 4.45E-08 7.80E-07 4.12E-08 121.57 24.59 3.56E-07 6.17E-08 -2.37E-07 4.00E-08 -78.45 1.39 -3.34E-07 3.70E-08 1.19E-07 7.35E-08 5.93E-07 6.92E-08 121.6 24.59 2.01E-06 1.86E-08 3.45E-08 1.64E-08 -39.23 0.31 -1.73E-07 1.40E-08 2.04E-06 2.13E-08 1.97E-06 1.44E-08 121.72 24.59 1.22E-06 2.19E-07 -1.18E-06 1.68E-07 -29.24 3.28 1.78E-07 1.40E-07 3.68E-08 2.74E-07 2.40E-06 1.86E-07 121.75 24.59 1.33E-06 1.71E-07 -9.56E-07 9.10E-08 -29.92 2.54 1.16E-07 6.70E-08 3.78E-07 2.22E-07 2.29E-06 1.26E-07 121.78 24.59 1.31E-06 1.26E-07 -4.53E-07 5.07E-08 -28.92 2.29 1.24E-07 3.91E-08 8.56E-07 1.59E-07 1.76E-06 9.09E-08 121.81 24.59 8.27E-07 1.56E-07 -3.73E-07 1.36E-07 -16.83 5.71 2.56E-07 1.28E-07 4.54E-07 1.97E-07 1.20E-06 1.78E-07 121.84 24.59 7.58E-07 1.53E-07 -4.88E-07 2.02E-07 -12.98 7.11 1.94E-07 1.61E-07 2.70E-07 2.45E-07 1.25E-06 2.31E-07 121.54 24.62 2.06E-07 3.72E-08 -8.90E-07 3.09E-08 75.00 0.63 -5.24E-07 2.41E-08 -6.84E-07 4.83E-08 1.10E-06 4.35E-08 121.57 24.62 5.47E-07 7.79E-08 -3.78E-07 7.49E-08 -80.48 1.09 -5.00E-07 5.37E-08 1.68E-07 1.08E-07 9.25E-07 1.04E-07 121.6 24.62 1.90E-06 2.79E-08 2.55E-08 2.56E-08 -41.59 0.54 -9.38E-08 2.02E-08 1.93E-06 3.52E-08 1.88E-06 2.05E-08
Lon Lat Eps1 Eps1(sig) Eps2 Eps2(sig) Theta The.(sig) Rotation Rot.(sig) Dilatation Dila.(sig) Gamma Gam.(sig) ( o ) ( o ) (strain/yr) (strain/yr) (strain/yr) (strain/yr) ( o ) ( o ) (radian/yr) (radian/yr) (strain/yr) (strain/yr) (strain/yr) (strain/yr) 121.66 24.62 1.43E-06 1.00E-07 -5.64E-07 9.93E-08 -42.09 1.82 -3.01E-07 7.73E-08 8.69E-07 1.27E-07 2.00E-06 7.79E-08 121.69 24.62 1.40E-06 1.18E-07 -9.13E-07 1.15E-07 -38.70 1.77 -3.00E-07 9.38E-08 4.91E-07 1.41E-07 2.32E-06 9.65E-08 121.75 24.62 1.04E-06 6.97E-08 -6.21E-07 5.99E-08 -31.58 1.57 1.90E-07 4.79E-08 4.14E-07 8.93E-08 1.66E-06 5.87E-08 121.78 24.62 1.08E-06 1.18E-08 -5.17E-07 1.12E-08 -33.86 0.29 1.52E-07 8.17E-09 5.65E-07 1.63E-08 1.60E-06 9.76E-09 121.81 24.62 1.28E-06 1.54E-07 -5.73E-10 1.21E-07 -15.72 4.60 -1.53E-07 1.05E-07 1.28E-06 1.93E-07 1.28E-06 1.74E-07 121.84 24.62 2.32E-06 3.56E-07 -1.48E-06 4.47E-07 -7.85 4.47 -8.95E-07 2.97E-07 8.43E-07 5.70E-07 3.79E-06 5.55E-07 121.6 24.65 1.54E-06 4.59E-08 -4.26E-07 6.41E-08 -55.84 1.07 1.16E-07 3.95E-08 1.11E-06 7.87E-08 1.96E-06 4.68E-08 121.63 24.65 1.57E-06 3.93E-08 -4.11E-07 5.02E-08 -53.43 0.85 5.95E-08 3.32E-08 1.16E-06 6.15E-08 1.98E-06 3.64E-08 121.66 24.65 1.39E-06 9.10E-08 -4.98E-07 9.16E-08 -43.49 1.69 -2.56E-07 7.25E-08 8.92E-07 1.11E-07 1.89E-06 7.26E-08 121.69 24.65 1.41E-06 4.15E-08 -5.10E-07 4.16E-08 -44.55 0.86 -1.49E-07 2.99E-08 9.02E-07 5.77E-08 1.92E-06 2.99E-08 121.72 24.65 1.30E-06 6.69E-08 -4.79E-07 6.88E-08 -42.66 1.57 -5.25E-08 4.73E-08 8.20E-07 9.73E-08 1.78E-06 4.78E-08 121.75 24.65 3.92E-07 1.13E-07 -5.08E-07 1.10E-07 -28.98 5.00 8.04E-08 8.06E-08 -1.16E-07 1.55E-07 8.99E-07 1.07E-07 121.78 24.65 4.61E-07 1.21E-07 3.23E-07 1.15E-07 -31.80 33.64 2.12E-07 8.92E-08 7.84E-07 1.58E-07 1.38E-07 1.06E-07 121.81 24.65 1.33E-06 1.31E-07 4.59E-07 1.15E-07 -1.09 6.32 -1.01E-07 9.59E-08 1.79E-06 1.74E-07 8.69E-07 1.74E-07 121.6 24.68 1.51E-06 7.58E-08 -2.75E-07 6.81E-08 -50.94 1.62 2.40E-07 5.04E-08 1.23E-06 1.03E-07 1.78E-06 5.37E-08 121.63 24.68 1.48E-06 1.54E-08 -2.61E-07 1.28E-08 -52.90 0.32 1.55E-07 9.88E-09 1.21E-06 2.02E-08 1.74E-06 1.10E-08 121.66 24.68 1.19E-06 7.30E-08 -3.64E-07 7.49E-08 -43.17 1.59 -7.43E-08 6.02E-08 8.23E-07 8.60E-08 1.55E-06 6.04E-08 121.69 24.68 1.23E-06 1.26E-08 -4.54E-07 1.29E-08 -43.83 0.31 -4.21E-08 8.96E-09 7.80E-07 1.81E-08 1.69E-06 8.98E-09 121.72 24.68 1.32E-06 4.76E-08 -4.01E-07 4.65E-08 -47.33 1.12 -1.19E-07 3.26E-08 9.22E-07 6.77E-08 1.72E-06 3.30E-08 121.75 24.68 1.33E-06 7.41E-08 1.95E-07 7.02E-08 -48.26 2.37 6.75E-08 5.46E-08 1.53E-06 9.47E-08 1.14E-06 5.53E-08 121.78 24.68 8.96E-07 6.37E-08 6.54E-07 1.12E-07 -18.57 17.06 -3.27E-07 7.79E-08 1.55E-06 1.22E-07 2.43E-07 1.08E-07 121.81 24.68 1.17E-06 1.38E-07 2.77E-08 1.66E-07 22.44 5.53 -3.81E-07 1.15E-07 1.20E-06 2.11E-07 1.14E-06 1.70E-07 121.84 24.68 1.33E-06 1.09E-07 -2.43E-07 1.90E-07 6.12 4.35 -5.92E-07 1.20E-07 1.09E-06 2.19E-07 1.57E-06 2.16E-07
Lon Lat Eps1 Eps1(sig) Eps2 Eps2(sig) Theta The.(sig) Rotation Rot.(sig) Dilatation Dila.(sig) Gamma Gam.(sig) ( o ) ( o ) (strain/yr) (strain/yr) (strain/yr) (strain/yr) ( o ) ( o ) (radian/yr) (radian/yr) (strain/yr) (strain/yr) (strain/yr) (strain/yr) 121.54 24.71 4.68E-07 1.51E-07 -5.47E-07 9.15E-08 -65.57 3.41 4.56E-07 1.06E-07 -7.98E-08 1.60E-07 1.01E-06 1.32E-07 121.63 24.71 1.01E-06 9.03E-08 -2.88E-07 1.03E-07 -39.01 2.94 9.09E-08 7.03E-08 7.23E-07 1.33E-07 1.30E-06 7.41E-08 121.66 24.71 1.06E-06 7.64E-08 -4.58E-07 8.03E-08 -40.84 1.98 1.88E-07 5.87E-08 6.00E-07 1.04E-07 1.52E-06 6.00E-08 121.69 24.71 1.15E-06 3.06E-08 -1.67E-07 2.77E-08 -41.47 0.89 5.04E-08 2.07E-08 9.86E-07 4.12E-08 1.32E-06 2.12E-08 121.72 24.71 1.29E-06 2.06E-08 -9.55E-08 1.92E-08 -39.16 0.58 -1.84E-08 1.42E-08 1.19E-06 2.79E-08 1.38E-06 1.50E-08 121.75 24.71 1.34E-06 5.99E-08 3.86E-07 6.24E-08 -43.67 2.64 -2.19E-07 4.25E-08 1.73E-06 8.79E-08 9.54E-07 4.26E-08 121.78 24.71 1.12E-06 3.01E-08 6.34E-07 1.57E-07 -1.90 7.69 -7.24E-07 6.47E-08 1.75E-06 1.60E-07 4.82E-07 1.60E-07 121.81 24.71 1.11E-06 2.99E-08 -8.16E-08 1.89E-07 -2.78 3.20 -8.05E-07 6.63E-08 1.03E-06 1.91E-07 1.19E-06 1.90E-07 121.57 24.74 6.09E-07 9.40E-08 -2.02E-07 2.23E-07 -11.02 4.63 -1.09E-07 4.93E-08 4.07E-07 2.50E-07 8.11E-07 2.32E-07 121.66 24.74 1.10E-06 8.09E-08 -4.56E-07 8.21E-08 -40.95 1.97 2.95E-07 6.17E-08 6.45E-07 1.07E-07 1.56E-06 6.29E-08 121.69 24.74 1.22E-06 2.92E-08 -1.25E-07 2.34E-08 -37.49 0.77 -1.89E-09 1.94E-08 1.10E-06 3.61E-08 1.35E-06 2.10E-08 121.72 24.74 1.32E-06 1.54E-08 -9.10E-08 1.28E-08 -35.73 0.40 -7.67E-08 1.03E-08 1.23E-06 1.96E-08 1.41E-06 1.16E-08 121.75 24.74 1.16E-06 5.36E-08 5.41E-07 9.27E-08 -28.72 4.96 -4.80E-07 5.21E-08 1.70E-06 1.09E-07 6.20E-07 7.31E-08 121.78 24.74 1.13E-06 2.80E-08 4.37E-07 1.71E-07 -6.46 4.84 -7.29E-07 5.64E-08 1.56E-06 1.75E-07 6.90E-07 1.71E-07 121.81 24.74 1.09E-06 3.37E-08 1.13E-07 2.27E-07 -10.30 4.09 -6.86E-07 6.01E-08 1.21E-06 2.35E-07 9.79E-07 2.21E-07 121.69 24.77 1.04E-06 1.22E-07 9.97E-08 5.46E-08 -26.45 4.05 2.65E-07 5.69E-08 1.14E-06 1.42E-07 9.38E-07 9.70E-08 121.72 24.77 1.27E-06 3.22E-08 -3.80E-08 2.19E-08 -33.81 0.87 -2.28E-08 1.86E-08 1.23E-06 4.02E-08 1.31E-06 2.30E-08 121.75 24.77 1.09E-06 4.62E-08 4.10E-07 1.04E-07 -15.91 4.86 -5.18E-07 5.75E-08 1.50E-06 1.14E-07 6.76E-07 1.01E-07 121.78 24.77 1.06E-06 4.56E-08 3.66E-07 1.47E-07 -19.45 5.37 -5.18E-07 5.09E-08 1.43E-06 1.65E-07 6.95E-07 1.32E-07 121.81 24.77 1.02E-06 6.60E-08 2.72E-07 2.19E-07 -23.76 7.92 -4.76E-07 5.90E-08 1.29E-06 2.59E-07 7.47E-07 1.80E-07 121.72 24.8 5.37E-07 4.80E-08 3.54E-07 1.06E-07 5.96 27.35 1.26E-07 8.86E-08 8.91E-07 1.15E-07 1.83E-07 1.14E-07 121.75 24.8 5.39E-07 8.42E-08 3.63E-07 1.02E-07 36.56 19.68 5.99E-08 7.35E-08 9.02E-07 1.19E-07 1.77E-07 7.83E-08 121.78 24.8 4.68E-07 2.43E-08 -1.93E-07 1.19E-07 -2.90 4.05 2.66E-07 4.65E-08 2.76E-07 1.21E-07 6.61E-07 1.21E-07
Lon Lat Eps1 Eps1(sig) Eps2 Eps2(sig) Theta The.(sig) Rotation Rot.(sig) Dilatation Dila.(sig) Gamma Gam.(sig) ( o ) ( o ) (strain/yr) (strain/yr) (strain/yr) (strain/yr) ( o ) ( o ) (radian/yr) (radian/yr) (strain/yr) (strain/yr) (strain/yr) (strain/yr) 121.81 24.8 4.18E-07 2.65E-08 -4.33E-07 1.51E-07 -4.08 3.38 3.08E-07 4.96E-08 -1.54E-08 1.54E-07 8.51E-07 1.52E-07 121.75 24.83 7.02E-07 3.06E-08 -5.66E-07 8.51E-08 -11.38 2.35 6.59E-07 5.33E-08 1.37E-07 8.90E-08 1.27E-06 8.46E-08 121.78 24.83 6.62E-07 2.27E-08 -1.01E-06 8.35E-08 -8.05 1.35 7.36E-07 3.91E-08 -3.49E-07 8.68E-08 1.67E-06 8.41E-08 121.81 24.83 6.02E-07 3.08E-08 -1.15E-06 9.46E-08 -8.60 1.43 7.44E-07 4.29E-08 -5.47E-07 1.00E-07 1.75E-06 9.64E-08 121.72 24.86 8.18E-07 4.45E-08 3.77E-08 7.30E-08 -84.10 0.64 -6.91E-08 4.62E-08 8.55E-07 8.53E-08 7.80E-07 8.41E-08 121.75 24.86 5.83E-07 5.65E-08 -5.74E-07 6.69E-08 -61.68 1.79 7.48E-09 4.46E-08 9.55E-09 8.67E-08 1.16E-06 6.05E-08 121.78 24.86 5.81E-07 1.77E-07 -1.45E-06 7.13E-08 -0.25 2.00 1.21E-06 7.09E-08 -8.72E-07 1.91E-07 2.03E-06 1.91E-07 121.81 24.86 3.59E-07 2.07E-07 -1.38E-06 8.31E-08 -5.11 3.61 1.06E-06 1.10E-07 -1.02E-06 2.23E-07 1.74E-06 2.20E-07 121.75 24.89 4.82E-07 5.26E-08 -1.59E-06 5.28E-08 -48.62 1.01 -1.51E-07 3.76E-08 -1.11E-06 7.37E-08 2.08E-06 3.85E-08 121.78 24.89 4.53E-07 4.96E-08 -2.24E-06 4.98E-08 -43.86 0.75 -2.89E-07 3.51E-08 -1.78E-06 7.03E-08 2.69E-06 3.52E-08
Eps1 為最大主應變速率。
Eps2 為最小主應變速率。
Theta 為最大主應變速率之方位角。
Rotation 為旋轉率。
Dilatation 為面膨脹率。
Gamma 為最大剪應變率。
(sig)為各項之誤差值。
附錄 C
宜蘭地區GPS 觀測站之時間序列。