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[1]李鸿莉,冯俊熙,佟宏鹏,等.台湾利吉蛇纹岩角砾碎屑岩地球化学特征及其指示意义[J].地球化学,2020,49(01):50-61.[doi:10.19700/j.0379-1726.2020.01.004]
 LI Hong-li,FENG Jun-xi,TONG Hong-peng,et al.Geochemical characteristics and their indicative significance of serpentine breccia clasolites in Lichi, Taiwan, China[J].Geochimica,2020,49(01):50-61.[doi:10.19700/j.0379-1726.2020.01.004]
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台湾利吉蛇纹岩角砾碎屑岩地球化学特征及其指示意义

参考文献/References:

[1]Proskurowski G, Lilley M D, Seewald J S, Früh-Green G L, Olson E J, Lupton J E, Sylva S P, Kelley D S. Abiogenic hydrocarbon production at Lost City hydrothermal field[J]. Science, 2008, 319(5863): 604-607.
[2]Bradley A S, Summons R E. Multiple origins of methane at the Lost City Hydrothermal Field[J]. Earth Planet Sci Lett, 2010, 297(1/2): 34-41.
[3]申婷婷, 张立飞, 陈晶. 俯冲带蛇纹岩的变质过程[J]. 岩石学报, 2016, 32(4): 1206-1218.
Shen Ting-ting, Zhang Li-fei, Chen Jing. Metamorphism of subduction zone serpentines[J]. Acta Petrol Sinica, 2016, 32(4): 1206-1218 (in Chinese with English abstract).
[4]李旭平, Rahn M, Bucher K, 张立飞. 蛇绿岩套中超基性岩体的岩石组合: 蛇纹岩、异剥钙榴岩和蛇绿碳酸岩——以西阿尔卑斯 Zermatt-Saas蛇绿岩为例[J]. 地学前缘, 2003, 10(4): 457-468.
Li Xu-ping, Rahn M, Bucher K, Zhang Li-fei. Lithological association of ultramafic rocks in ophiolites: Serpentinite, rodingite and ophicarbonatean example from Zermatt-Saas of western Alps[J]. Earth Sci Front, 2003, 10(4): 457-468 (in Chinese with English abstract).
[5]Dilek Y, Furnes H. Ophiolite genesis and global tectonics: Geochemical and tectonic fingerprinting of ancient oceanic lithosphere[J]. Geol Soc Am Bull, 2011, 123(3/4): 387-411.
[6]王先彬, 欧阳自远, 卓胜广, 张明峰, 郑国东, 王永莉. 蛇纹石化作用、非生物成因有机化合物与深部生命[J]. 中国科学(地球科学), 2014, 44(6): 1096-1106.
Wang Xianbin, Ouyang Ziyuan, Zhuo Shengguang, Zhang Mingfeng, Zheng Guodong, Wang Yongli. Serpentinization, abiogenic organic compounds, and deep life[J]. Sci China Earth Sci, 2014, 44(6): 1096-1106 (in Chinese).
[7]王先彬, 郭占谦, 妥进才, 郭洪岩, 李振西, 卓胜广, 蒋鸿亮, 曾龙伟, 张铭杰, 王连生, 柳春雪, 闫宏, 李立武, 周晓峰, 王永莉, 杨辉, 王广. 中国松辽盆地商业天然气的非生物成因烷烃气体[J]. 中国科学(D辑), 2009, 39(5): 602-614.
Wang Xianbin, Guo Zhanqian, Tuo Jincai, Guo Hongyan, Li Zhenxi, Zhuo Shengguang, Jiang Hongliang, Zeng Longwei, Zhang Mingjie, Wang Liansheng, Liu Chunxue, Yan Hong, Li Liwu, Zhou Xiaofeng, Wang Yongli, Yang Hui, Wang Guang. Abiogenic hydrocarbons in commercial gases from the Songliao Basin, China[J]. Sci China (D), 2009, 39(5): 602-614 (in Chinese).
[8]Parnell J, Boyce A J, Blamey N J F. Follow the methane: The search for a deep biosphere, and the case for sampling serpentinites, on Mars[J]. Int J Astrobiol, 2010, 9(4): 193-200.
[9]Schrenk M O, Brazelton W J, Lang S Q. Serpentinization, carbon, and deep life[J]. Rev Mineral Geochem, 2013, 75(1): 575-606.
[10]Kelley D S, Karson J A, Fruh Green G L, Yoerger D R, Shank T M. A serpentinite hosted ecosystem: The Lost City hydrothermal field[J]. Science, 2005, 307(5714): 1428-1434.
[11]Russell M, Hall A, Martin W. Serpentinization as a source of energy at the origin of life[J]. Geobiology, 2010, 8(5): 355-371.
[12]Schwarzenbach E M, Frueh-Green G L, Bernasconi S M, Alt J C, Plas A. Serpentinization and carbon sequestration: A study of two ancient peridotite-hosted hydrothermal systems[J]. Chem Geol, 2013, 351: 115-133.
[13]耿威, 张训华, 刘昌岭, 孙治雷, 孙建业, 尚鲁宁, 马雪. 台湾利吉混杂岩中蛇纹岩岩石学和U-Pb年代学及其地质意义[J]. 海洋地质与第四纪地质, 2018, 38(2): 129-135.
Geng Wei, Zhang Xun-hua, Liu Chang-ling, Sun Zhi-lei, Sun Jian-ye, Shang Lu-ning, Ma Xue. Petrology and U-Pd geochronology of the serpentinite in the Lichi mélange implications[J]. Mar Geol Quatern Geol, 2018, 38(2): 129-135 (in Chinese with English abstract).
[14]Huang C Y, Shyu C T, Lin S B, Lee T Q, Sheu D D. Marine geology in the arc-continent collision zone off southeastern Taiwan: Implications for late Neogenew volution of the Coastal Range[J]. Mar Geol, 1992, 107(3): 183-212.
[15]Huang C Y, Wu W Y, Chang C P, Tsao S, Yuan P B, Lin C W, Xia K Y. Tectonic evolution of accretionary prism in the arc-continent collision terrane of Taiwan[J]. Tectonophysics, 1997, 281(1/2): 31-51.
[16]Huang C Y, Yuan P B, Lin C W, Wang T K, Chang P. Geodynamic processes of Taiwan arc-continent collision and comparison with analogs in Timor, Papua New Guinea, Urals and Corsica[J]. Tectonophy, 2000, 325(1/2): 1-21.
[17]Huang C Y, Chen C W, Yao B, Chang C P. The Lichi Mélange: A collision mélange formation along early arcward back thrusts during forearc basin closure, Taiwan arc-continent collision[J]. Geol Soc Am Spec Pap, 2008, 436: 127-154.
[18]Reed D L, Lundberg N, Liu C S, Kuo B Y. Structural relations along the margins of the offshore Taiwan accretionary wedge: Implications for accretion and crustal kinematics[J]. Acta Geol Taiwan, 1992, 30: 105-122.
[19]Lundberg N, Reed D L, Liu C S and Lieske J. Forearc-basin closure and arc accretion in the submarine suture zone south of Taiwan[J]. Tectonophysics, 1997, 274(1): 5-23.
[20]Ho C S. A synthesis of the geological evolution of Taiwan[J]. Tectonophysics, 1986, 125(1-3): 1-16.
[21]Malavieille J, Lallemand S E, Dominguez S, Deschamps A, Lu C Y. Arc-continent collision in Taiwan: New marine observations and tectonic evolution[J]. Geol Soc Am Bull Spec Pap, 2002, 358: 187-211.
[22]Chi W C, Reed D L, Moore G, Nguyen T, Liu C S, Lundberg N. Tectonic wedging along the rear of the offshore Taiwan accretionary prism[J]. Tectonophysics, 2003, 374(3/4): 199-217.
[23]Biq C. Comparison of mélange tectonic in Taiwan and some other mountain belts[J]. Pet Geol Taiwan, 1971, 9: 79-106.
[24]Biq C. Kinematic pattern of Taiwan as an example of actual continent-arc collision[J]. Rep Semin Seismol US-ROC Coop Sci Progr, 1973, 25: 21-26.
[25]Teng L S. Geotectonic evolution of late Cenozoic arc-continent collision in Taiwan[J]. Tectonophysics, 1990, 183(1): 57-76.
[26]Liu C S, Liu S Y, Lallemand S, Lundberg N, Reed D. Digital elevation model offshore Taiwan and its tectonic implications[J]. Terre Atmos Ocean Sci, 1998, 9(4): 705-738.
[27]Biq C C. Dual-trench structure in the Taiwan-Luzon region[J]. Proc Geol Soc China, 1972, 15: 65-75.
[28]Bowin C, Lu R S, Lee C S, Schouten H. Plate convergence and accretion in Taiwan-Luzon region[J]. Am Assoc Petrol Geol Bull, 1978, 62(2): 1645-1672.
[29]Chen C H, Yeh Y H. Bathymetric ridges and troughs in the active arc-continent collision region off southeastern Taiwan[J]. Proc Geol Soc China, 1990, 33(4): 351-372.
[30]Chung S L, Sun S-s. A new genetic model for the East Taiwan Ophiolite and its implication for dupal domains in the Northern hemisphere[J]. Earth Planet Sci Lett, 1992, 109(1/2): 133-145.
[31]Sibuet J C, Hsu S K. How was Taiwan created[J]. Tectonophysics, 2004, 379(1-4): 159-181.
[32]Chang C P, Angelier J, Huang C Y, Liu C S. Structural evolution and significance of a mélange in a collision belt: The Lichi mélange and the Taiwan arc-continent collision[J]. Geol Mag, 2001, 138(6): 633-651.
[33]Chi W C, Chen L W, Liu C S, Brookfield M. 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[J]. Tectonophysics, 2014, 636: 70-82.
[34]Huang C Y, Yuan P B, Tsao S J. Temporal and spatial records of active arc-continent collision in Taiwan: A synthesis[J]. Geol Soc Am Bull, 2006, 118(3/4): 274-288.
[35]徐铁良. 台湾东部海岸山脉地质[J]. 台湾省地质调查所汇刊, 1956, 8: 15-63.
Xu Tie-liang. Geology of coastal mountains in eastern Taiwan[J]. Taiwan Geol Surv, 1956, 8: 15-63 (in Chinese).
[36]Chang C P, Angelier J, Huang C Y. Origin and evolution og a mélange: The active plate boundary and suture zone of the Longitudinal valley, Taiwan[J]. Tectonophysics, 2000, 325(1/2): 43-62.
[37]Liou J G, Lan C Y, Ernst W G. The East Taiwan Ophiolite: Its occurrence, petrology, metamorphism, and tectonic setting[J]. Min Res Serv Organ Spec Pap, 1977, 1: 1-212.
[38]Page B M, Suppe J. The Pliocene Lichi Mélange of Taiwan: Its plate tectonic and olistostromal origin[J]. Am J Sci, 1981, 281(3): 193-227.
[39]Yui T F, Jeng R C. A stable-isotope study of the hydrothermal alteration of the East Taiwan ophiolite[J]. Chem Geol, 1990, 89(1/2): 65-85.
[40]Hsu T L. The Lichi mélange in the coastal range framework[J]. Bull Geol Surv Taiwan, 1976, 25: 87-95.
[41]冯俊熙. 极端环境自生碳酸盐岩成因机制研究: 以垃圾填埋场与蛇纹岩中的碳酸盐岩为例[D]. 广州: 中国科学院广州地球化学研究所, 2016.
Feng Jun-xi. A study of formation mechanisms of authigenic carbonates from extreme environments including landfill and serpentinite[D]. Guangzhou: Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, 2016 (in Chinese with English abstract).
[42]Taylor J. Computer programs for standard less quantitative analysis of minerals using the full powder diffraction profile[J]. Pow Diff, 1991, 6(1): 2-9.
[43]耿威. 台湾海岸山脉岩石地球化学特征及其构造意义[D]. 青岛: 中国科学院海洋研究所, 2013.
Geng Wei. The rocks in the Coastal Range, eastern Taiwan: Petrology, geochemistry and tectonic implications[D]. Qingdao: Institute of Oceanology, Chinese Academy of Sciences, 2013 (in Chinese with English abstract).
[44]Lin C T, Ron H, Sun W D, Zhang G L. Geochemical and geochronological constraints on the origin and emplacement of the East Taiwan ophiolite[J]. Geochem Geophys Geosyst, 2019. Doi: 10.1029/2018GC007902.
[45]Bonatti E, Michael P J. Mantle peridotites from continental rifts to ocean basins to subduction zones[J]. Earth Planet Sci Lett, 1989, 91(3/4): 297-311.
[46]Fryer P, Lockwood J P, Becker N, Phipps S, Todd C S. Significance of serpentine mud volcanism in convergent margins[J]. Spec Pap Geol Soc Am, 2000: 35-52.
[47]Grimmer J C, Greiling R O. Serpentinites and low-K island arc metavolcanic rocks in the lower Koli Nappe of the central Scandinavian Caledonides: Late Cambrian-Early Ordovician serpentinite mud volcanoes in a fore-arc; basin?[J]. Tectonophysics, 2012, 541/543: 19-30.
[48]耿威, 张训华, 黄龙. 台湾海岸山脉利吉混杂岩基质来源分析[M]. 北京: 中国学术期刊电子出版社, 2013: 1298.
Geng Wei, Zhang Xun-hua, Huang long. Matrix Source Analysis of Lichi Mélange in Taiwan Coastal Mountains[M]. Beijing: China Academic Journal Electronic Publishing House, 2013: 1298 (in Chinese).
[49]林秋婷, 黄奇瑜, 孙卫东. 台湾弧陆碰撞带海岸山脉利吉混杂岩中枕状玄武岩研究: 马尼拉海沟俯冲初期弧前拉张的证据[M]. 北京: 地质出版社, 2012: 188-189.
Lin Qiu-ting, Huang Qi-yu, Sun Wei-dong. Pillow Basalts in Lichi mélange in the Coastal Range of Taiwan Arc-Continental Collision Zone: Evidence of Pre-arc Tension at the Initial Stage of Manila Trench Subduction[M]. Beijing: Geological Publishing House, 2012: 188-189 (in Chinese).
[50]Coleman R G. Ophiolites[M]. New York: Springer, 1977: 229.
[51]Ei Bahariya G A, Arai S. Petrology and origin of Pan-African serpentinites with particular reference to chromian spinel compositions, Eastern Desert, Egypt: Implication for supra-subduction zone ophiolite[J]. 3rd Int Conf Geol Afr, 2003, 1: 371-388.
[52]Azer M K, Stern R J. Neoproterozoic(835-720 Ma) serpentinites in the Eastern Desert, Egypt: Fragments of forearc mantle[J]. Geology, 2007, 115(4): 457-472.
[53]Bonatti E, Michael P J. Mantle peridotites from continental rifts to ocean basins to subduction zones[J]. Earth Planet Sci Lett, 1989, 91(3/4): 297-311.
[54]Ernst W G. Franciscan mélanges: Coherent blocks in a low-density, ductile matrix[J]. Int Geol Rev, 2015, 58(5): 626-642.
[55]Cheng W B, Hsu S K, Chang C H. Tomography of the southern Taiwan subduction zone and possible emplacement of crustal rocks into the forearc mantle[J]. Glob Planet Chang, 2012, 90/91: 20-28.
[56]Doo W B, Lo C L, Kuo-Chen H, Brown D, Hsu S K. Exhumation of serpentinizedperidotite in the northern Manila subduction zone inferred from forward gravity modeling [J]. Geophys Res Lett, 2015, 42(19): 7977-7982.
[57]Yang T F, Yeh G H, Fu C C, Wang C C, Lan T F, Lee H F, Chen C H, Walia V, Sung Q C. Composition and exhalation flux of gases from mud volcanoes in Taiwan[J]. Envir Geol, 2004, 46(8): 1003-1011.
[58]Chen W H, Huang C Y, Yan Y, Dilek Y, Chen D F, Wang M H, Zhang X C, Lan Q, Yu M M. Stratigraphy and provenance of forearc sequences in the Lichi mélange, Coastal Range: Geological records of the active Taiwan arc-continent collision[J]. J Geophys Res Solid Earth, 2017, 122(9): 7408-7436.
[59]Fryer P. Serpentinite mud volcanism: Observations, processes, and implications[J]. Ann Rev Marine Sci, 2012, 4(1): 345-373.
[60]Mottl M J, Wheat C G, Fryer P, Gharib J, Martin J B. Chemistry of springs across the Mariana forearc shows progressive devolatilization of the subducting plate[J]. Geochim Cosmochim Acta, 2004, 68(23): 4915-4933.
[61]Hulme S M, Wheat C G, Fryer P, Mottl M J. Pore water chemistry of the Mariana serpentinite mud volcanoes: A window to the seismogeniczone[J]. Geochem Geophys Geosyst, 2010, 11(1): 1-29.
[62]Fryer P, Wheat C G, Mottl M J. Mariana blueschist mud volcanism: Implications for conditions within the subduction zone[J]. Geology, 1999, 27(2): 103-106.
[63]Mottl M J, Komor S C, Fryer P, Moyer C L. Deep-slab fluids fuel extreme ophilic Archaea on a Mariana forearc serpentinite mud volcano: Ocean Drilling Program Leg 195[J]. Geochem Geophys Geosyst, 2003, 4(11): 1-14.
[64]陈文煌. 海岸山脉中南段弧前盆地地层研究: 台湾弧陆碰撞记录及其对南海深水古海洋的控制[D]. 广州: 中国科学院广州地球化学研究所, 2015.
Chen Wen-huang. Stratigraphic study of the forearc basin in the middle-south section of the coastal mountains: Taiwan arc-continental collision records and their controls on the deep-water paleooceans in the South China Sea[D]. Guangzhou: Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, 2015 (in Chinese with English abstract).

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备注/Memo

收稿日期(Received): 2019-01-10; 改回日期(Revised): 2019-04-08; 接受日期(Accepted): 2019-04-30
基金项目: 国家自然科学基金(41673029)
作者简介: 李鸿莉(1978-), 女, 讲师, 从事地球化学方面的工作。E-mail: hlli@ shou.edu.cn
* 通讯作者(Corresponding author): CHEN Duo-fu, E-mail: dfchen@ shou.edu.cn; Tel: +86-21-61900542

更新日期/Last Update: 2020-02-20