REGIONAL GEOLOGICAL FEATURES AND NEOTECTONIC MOVEMENT OF TAIWAN INLAND AND OFFSHORE AREAS
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摘要: 台湾位于欧亚板块与菲律宾海板块的交界带,中中新世开始的吕宋岛弧与欧亚大陆边缘碰撞造山运动形成了现今台湾及其附近海域的基本构造格局和特有的区域地质特征。通过对台湾岛地质考察和研究区各种调查资料的分析,总结台湾及其附近海域区域地质特征,具有出露地层新、构造活动年轻且强烈、受马尼拉和琉球两个俯冲带共同影响等特点;研究区的新构造运动主要受到弧陆碰撞的影响,表现出各种断裂作用极其发育、逆冲-褶皱带多见、火山和地震活动频发、地热温度比较高等特征,研究区中西部麓山带和台东纵谷-海岸山脉以及台湾南部和东北部海域是新构造运动的活跃区。Abstract: Taiwan is located at the junction of the Eurasian Plate and the Philippine Sea Plate. The tectonic framework and regional geological features of the inland and its offshore owe their origin to the collision of the Luzon Arc and the Eurasian Continent (arc-continent collision) in Middle Miocene. We summarized in this paper the regional geological features of the study area based on field geological observation and survey data. The geology of Taiwan is characterized by young strata, strong and young active tectonics and the influence of both Manila subduction and Ryukyu subduction. The neotectonic movement in Taiwan is also effected by arc-continent collision. There are numerous faults, thrust-fold belts, frequent volcanic eruptions and earthquakes and higher geothermal anomalies in the study area. Neotectonic movement is particularly active in the Western Foothills, the Longitudinal Valley-the Coastal Rang and the southern and northeastern seas.
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Key words:
- arc-continent collision /
- regional geological features /
- neotectonic movement /
- Taiwan
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[1] Biq C. Dual-trench in the Taiwan-Luzon region[J]. Proceedings of the Geological Society of China, 1972, 15:65-75.
[2] Bowin C, Lu R S, Lee C S, et al. Plate convergence and accretion in Taiwan-Luzon region[J]. American Association of Petroleum Geologists Bulletin, 1978, 62:1645-1672.
[3] Karig D E. Basin genesis in the Philippine Sea[C]//DSDP Initial Report. 1975, 31:857-879.
[4] Huang C Y, Shyu C T, Lin S B, et al. Marine geology in the arc-continent collision zone off southeastern Taiwan:Implications for late Neogene evolution of the Coastal Range[J]. Marine Geology, 1992, 107:183-212.
[5] Huang C Y, Xia K Y, Yuan P B, et al. Structural evolution from Paleogene extension to Latest Miocene-Recent arc-continent collision offshore Taiwan[J]. Journal of Asian Earth Science, 2001, 19:619-639.
[6] Reed D L, Lundberg N, Liu C S, et al. Structural relations along the margins of the offshore Taiwan accretionary wedge:Implications for accretion and crustal kinematics[J]. Acta Geologica Taiwanica, 1992, 30:105-122.
[7] Liu C S, Huang I L, Teng L S. Structural styles offshore southwestern Taiwan[J]. Marine Geology, 1997, 137:305-319.
[8] Malavieille J, Lallemand S E, Dominguez S, et al. Arc-continent collision in Taiwan:New marine observations and tectonic evolution[J]. Geological Society of America Bulletin, Special Paper, 2002, 358:187-211.
[9] Ho C S. Structural evolution of Taiwan[J]. Tectonophysics, 1967, 4:367-378.
[10] Chai B H T. Structure and tectonic evolution of Taiwan[J]. American Journal of Science, 1972, 272:389-422.
[11] Jahn B M, Martineau F, Peucat J J, et al. Geochronology of the Tananao Schist Complex, Taiwan[J]. Tectonophysics, 1986, 125:103-124.
[12] Teng L S. Tectnostratigraphic facies and geological evolution of the Coastal Range, eastern Taiwan[J]. Memoir of the Geological Society of China, 1987, 8:229-250.
[13] Teng L S. Geotectonic evolution of late Cenozoic arc-continental collision in Taiwan[J]. Tectonophysics, 1990, 183:67-76.
[14] Chung S L, Sun S S. A new genetic model for the East Taiwan ophiolite and its implications for dupal domains in the Northern hemisphere[J]. Earth and Planetary Science Letters, 1992, 109:133-145.
[15] Huang C Y, Yin Y C. Bathymetric ridges and troughs in the active arc-continent collision region off southeastern Taiwan[J]. Proceedings of the Geological Society of China, 1990, 33(4):351-372.
[16] Huang C Y. Bathymetric ridges and troughs in the active arc-continent collision region off southeastern Taiwan:Reply and discussions[J]. Journal of the Geological Society of China, 1993, 36:91-109.
[17] Liu C S, Liu S Y, Lallemand S, et al. Digital elevation model offshore Taiwan and its tectonic implications[J]. Tao, 1998, 9:705-738.
[18] Huang C Y, Yuan P B, Song S R, et al. Tectonic of short-lived intra-arc basins in the arc-continent collision terrane of the Coastal Range, eastern Taiwan[J]. Tectonics, 1995, 14(1):19-38.
[19] Huang C Y, Wu W Y, Chang C P, et al. Tectonic evolution of accretionary prism in the arc-continent collision terrane of Taiwan[J]. Tectonophysics, 1997, 281:31-51.
[20] Huang C Y, Yuan P B, Lin C W, et al. Geodynamic processes of Taiwan arc-continent collision and comparison with analogs in Timor, Papua New Guinea, Urals and Corsica[J]. Tectonophysics, 2000, 325:1-21.
[21] Huang C Y, Yuan P B, Tsao S J. Temporal and spatial records of active arc-continent collision in Taiwan:A synthesis[J]. Bulletin of Geological Society of American, 2006, 118:274-288.
[22] Huang C Y, Jien C W, Chang C P, et al. The Lichi Melange:a tectonic collision complex originated form sheared forearc in Coastal Range, eastern Taiwan[J]. Geological Society of America Bulletin, Special Paper, 2008, 436:127-154.
[23] Chang C P, Angelier J, Huang C Y. origin and evolution of a melange:the active plate boundary and suture zone of the Longitudinal Valley, Taiwan[J]. Tectonophysics, 2000, 325:43-62.
[24] Chang C P, Angelier J, Huang C Y, et al. Structural evolution and significance of a melange in a collision belt:the Lichi Melange and the Taiwan arc-continent collision[J]. Geological Magazine, 2001, 138:633-651.
[25] 黄奇瑜. 由西部麓山带始新世张裂盆地层序的认识检讨雪山山脉的地层[J]. 经济部中央地质调查所特刊, 2009, 22:47-62.[HUANG Chiyue. Significance of Eocene extension basin sequences in the northern Western Foothills:a key point in study of Hsü
;ehshan Range stratigraphy[J]. Central Geological Survey Special Publication, 2009, 22:47-62.]
[26] Huang T C, Ting J S. Calcareous nannofossils succession from the Oligo-Miocene Peikangchi section and revised stratigraphic correlation between northern and central Taiwan[J]. Proceedings of the Geological Society of China, 1979, 22:105-120.
[27] Sun S C. The Tertiary basins of offshore Taiwan[C]//Proceedings of 2nd ASCOPE Conference and Exhibition, Manila, Philippines. 1982:125-135.
[28] 刘建华, 吴健生, 方银霞, 等. 东海陆架盆地的前新生界[J]. 海洋学报, 2007, 29(1):66-75.
[LIU Jianhua, WU Jiansheng, FANG Yinxia, et al. Pre-Cenozoic groups in the shelf basin of East China Sea[J]. Acta Oceanologica Sinica, 2007, 29(1):66-75.]
[29] Li P, Rao C. Tectonic characteristics and evolution history of the Pearl River Mouth Basin[J]. Tectonophysics, 1994, 235:13-25.
[30] Chen J, Xu S, Sang J. The depositional characteristics and oil potential of paleo Pearl River delta systems in the Pearl River Basin, South China Sea[J]. Tectonophys, 1994, 235:1-11.
[31] Taylor B, Hayes D E. Origin and history of the South China Sea Basin[C]//The Tectonic and Geological Evolution of Southeast Asian Seas and Islands Part Ⅱ, AGU Monogr, 1983, 20:129-155.
[32] Chi W C, Reed D L, Moore G, et al. Tectonic wedging along the rear of the offshore Taiwan accretionary prism[J]. Tectonophysics, 2003, 374:199-217.
[33] Fuh S C, Liu C S, Lundberg N, et al. Strike-slip faults offshore southern Taiwan; implications for the oblique arc-continent collision processes[J]. Tectonophysics, 1997, 274:25-39.
[34] Yang T F, Tien J, Chen C H, et al. Fission-track dating of volcanics in the northern part of the Taiwan Luzon Arc:eruption ages and evidence for crustal contamination[J]. Journal of Southeast Asian Earth Science, 1995, 11:81-93.
[35] Yang T Y, Liou T K, Chen C H. Thermal event records of the Chimei Igneous Complex:Constraint on the ages of magma activities and the structural implication based on fission track dating[J]. Acta Geologica Taiwanica, 1988, 26:237-246.
[36] Chen C H, Shieh Y N, Lee T, et al. Nd-Sr-O isotopic evidence for source contamination and an unusual mantle component under Luzon Arc[J]. Geochimica et Cosmochimica Acta, 1990, 54:2473-2483.
[37] Lo C H, Onstott T C, Chen C H, et al. An assessment of 40Ar/39Ar dating for the whole-rock volcanic samples from the Luzon Arc near Taiwan[J]. Chemical Geology (Isotope Geoscience Section), 1994, 114:157-178.
[38] Deschamps A, Monie P, Lallemand S, et al. Evidence for Early Cretaceous oceanic crust trapped in the Philippine Sea Plate[J]. Earth and Planetary Science Letters, 2000, 179:503-516.
[39] Schn rle P, Liu C S, Serge E, et al. Structural insight into the south Ryukyu margin:effects of the subducting Gagua Ridge[J]. Tectonophysics, 1998, 288:237-250.
[40] Seno T, Stein S, Gripp A E. A model for the motion of the Philippine Sea plate consistent with NUVEL-1 and geologic data[J]. Journal of Geophysical Research, 1993, 98(B17):941-948.
[41] 高祥林. 琉球海沟的构造和运动特征[J]. 地球物理学进展, 2003, 18(2):293-301.
[GAO Xianglin. Tectonics and motion of the Ryukyu trench[J]. Progress in Geophysics, 2003, 18(2):293-301.]
[42] 傅命佐, 刘乐军, 郑彦鹏, 等. 琉球"沟-弧-盆系"构造地貌:地质地球物理探测与制图[J]. 科学通报, 2004, 49(14):1447-1460.
[FU Mingzuo, LIU Lejun, ZHENG Yanpeng. Geological and geophysical exploration and mapping of tectonic geomorphology of the Ryukyu Trench-Arc-Basin[J]. Chinese Science Bulletin, 2004, 49(14):1447-1460.]
[43] Lee C S, Shor G G, Bibee L D, et al. Okinawa Trough-Origin of a back-arc basin[J]. Marine Geology, 1980, 35:219-241.
[44] Letouzey J, Kimura M. The Okinawa Trough:Genesis of back-arc basin developing along a continental margin[J]. Tectonophysics, 1986, 125:209-230.
[45] Suppe J. Kinematics of arc-continent collision, flipping of subduction, and back-arc spreading near Taiwan[J]. Memoir of the Geological Society of China, 1984, 6:21-33.
[46] 张徽正, 林启文, 陈勉铭, 等. 台湾活动断层概论(1:50000)台湾活动断层分布图说明书[J]. 经济部中央地质调查所特刊, 1998.[CHANG Huicheng, LIN Chiiwen, CHEN Menming, et al. Introduction of Taiwan active faults (1:50000)[J]. Central Geological Survey Special Publication, 1998.
]
[47] 林启文, 陈文山, 饶瑞钧.台湾活动断层调查的近期发展[J]. 经济部中央地质调查所特刊, 2007, 18:85-110.[LIN ChiiWen, CHEN Wenshan, RAU Rueyjuin. Recent Advances in the Study of Active Faults in Taiwan[J]. Central Geological Survey Special Publication, 2007
, 18:85-110.]
[48] Chen W S, Huang M T, Liu T K. Neotectonic significance of the Chimei fault in the Coastal Range, eastern Taiwan[J]. Proceedings of the Geological Society of China, 1991, 34(1):43-56.
[49] 李乃胜. 冲绳海槽断裂构造的研究[J]. 海洋与湖沼, 1988, 19(4):347-358.
[LI Naisheng. On the fracturing structures of the Okinawa Through[J]. Oceanologia et Limnologia Sinica, 1988, 19(4):347-358.]
[50] 王舒畋, 李斌. 东海新构造与新构造运动[J]. 海洋地质与第四纪地质, 2010, 30(4):141-150.
[WANG Shutian, LI Bin. Neotectonic features and movement in the East China Sea[J]. Marine Geology and Quaternary Geology, 2010, 30(4):141-150.]
[51] 中央经济部中央地质调查所. 1:50000地质图(大禹岭幅, 1994; 东势幅, 2000; 雾社幅, 2002; 台东-知本幅, 2008)[M]. 台北:台湾中央经济部中央地质调查所.[Central Geological Survey. Geologic Map of Taiwan, 1:50000(Tayuling, 1994
; Tungshih, 2000; Wushe, 2002; Taitung and Jhiben, 2008)[M]. Taipei:Central Geological Survey, Ministry of Economic Affairs.]
[52] 李春峰, 周祖翼, 李家彪,等. 台湾岛南部海域的前碰撞构造地球物理特征[J]. 中国科学D辑:地球科学, 2007, 27(5):649-659.
[LI Chunfeng, ZHOU Zuyi, LI Jiabiao. Tectonics geophysical characteristics of the Seas of south Taiwan before collision[J]. Science in China Series D:Earth Sciences, 2007, 27(5):649-659.]
[53] Tsai Y B. Seismotectonics of Taiwan[J]. Tectonophys, 1986, 125:17-37.
[54] Rau R J, Wu F T. Tomographic imaging of lithospheric structures under Taiwan[J]. Earth and Planetary Science Letters, 1995, 133:517-532
[55] 何春荪.台湾地质概论-台湾地质图说明书[M]. 台北:台湾中央经济部中央地质调查所, 1986:118-125.[HO Chunsun. Geology of Taiwan[M]. Taipei:Central Geological Survey, Ministry of Economic Affairs, 1986:118
-125.]
[56] Lin C H. Thermal modeling of continental subduction and exhumation constrained by heat flow and seismicity in Taiwan[J]. Tectonophysics, 2000, 324:189-201
[57] 刘昭民. 台湾的地热资源[J]. 中国地质, 1992(5):25-28.[LIU Zhaomin. Geothermal resources of Taiwan[J]. Geology in China, 1992
(5):25-28.]
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