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地质学报  2001 

扬子板块俯冲的构造加积楔

, PP. 338-352

Keywords: 加积楔板块构造扬子板块浅变质岩大别-苏鲁造山带

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Abstract:

在总结大洋板块俯冲形成加积楔的基础上,对大别-苏鲁造山带内部及北缘浅变质岩进行了系统的研究,指出它们是扬子大陆板块俯冲的构造加积楔,这些浅变质岩既有产出在造山带北缘,也有少量出露在超高压变质带的内部,它们均形成于前印支期扬子板块北缘,主体为低绿片岩相变质的复理石相沉积岩和少量侵入岩,并遭受了与造山带超高为质岩相同的加里东-印支期构造热事件的改造,具有板块俯冲过程中被刮削下来的构造残睛-加积楔的形成机制和特征。垂向剖面上,这些浅变质岩原岩主要由表层浅海复理石相沉积岩系和下伏陆壳基底岩石(花岗质侵入体-变质中基性杂-岩大理岩组合)两部分组成,而超高压变质岩原岩主要为扬子板块北缘的俯冲击壳基底岩石,将构造加积楔形成理论纳入到印支期扬了变质岩及构造加积楔形成过程的时空耦合关系,确定子扬子板块俯冲加积楔不同构造部位浅变质岩的构造组合特点,探讨了扬子板块俯冲过程中构造加积楔形成的动力学过程。

References

[1]  安徽省地质矿产局. 1997. 安徽省岩石地层. 武汉:中国地质大学出版社.
[2]  程裕淇,刘敦-,Williams I S, 简平,庄育勋,高天山. 2000. 大别山碧溪岭深色榴辉岩和片麻状花岗质岩石SHRIMP分析. 地质学报, 74(3): 193-205.
[3]  董树文, 王小凤, 黄德志. 1996a. 大别山超高压变质带浅变质岩片的发现及意义. 科学通报, 41(9): 815-820.
[4]  董树文, 张勇, 黄德志. 1996b. 苏北超高压变质带石桥构造窗地质特征. 安徽地质,6(1): 9~13.
[5]  傅斌, 郑永飞, 肖益林,等. 1998. 大别山苏家河地区榴辉岩和大理岩的地球化学研究. 地质学报, 72(4): 323~339.
[6]  郝杰, 刘小汉. 1988. 桐柏-大别碰撞造山带推覆-滑脱构造及演化. 地质科学, (1): 1~9.
[7]  河南省地质矿产局. 1989. 河南省区域地质志. 北京:地质出版社.
[8]  河南省地质矿产局. 1997. 河南省岩石地层. 北京:中国地质大学出版社.
[9]  江苏省地质矿产局. 1995. 江苏省岩石地层. 武汉:中国地质大学出版社.
[10]  刘若新, 樊祺诚, 李惠民,等. 1995. 大别山碧溪岭石榴橄榄岩榴辉岩体的原岩性质及同位素地质年代学启示. 岩石学报, 11(3): 243-256.
[11]  马文璞, 刘文灿, 王国胜. 1997. 梅山群的再定位、区域对比和构造含义. 现代地质, 11(1): 95~101.
[12]  马杏垣,刘昌栓,刘国栋. 1986. 江苏响水至内蒙古满都拉地学断面. 北京:地质出版社.
[13]  牛宝贵,富云莲,刘志刚,等. 1994. 桐柏(大别山主要构造热事件及40Ar/39Ar地质定年研究. 地球学报, 15(1~2):20~33.
[14]  山东省地质矿产局. 1991. 山东省区域地质志. 北京:地质出版社.
[15]  山东省地质矿产局. 1996. 山东省岩石地层. 武汉:中国地质大学出版社.
[16]  史大年,姜枚,彭聪,等. 1999. 大别-苏鲁造山带东部地壳结构的层析成像及广角反射的地震学研究. 地震学报, 21(4): 403-410.
[17]  谭应佳. 1997. 北淮阳梅山群的隶属及其地质构造若干问题. 现代地质, 11(2): 221~228.
[18]  汤加富, 钱存超, 高天山. 1995. 大别山区榴辉岩带中浅变质火山碎屑岩组合的发现及其地质意义. 安徽地质, 5(2): 29~36.
[19]  谢智, 陈江峰, 董树文. 1999. 大别造山带南部浅变质岩的锆石U-Pb年龄. 地球科学, 20(4):335~340.
[20]  杨巍然, 游振东, 韩郁菁, 张泽民, 韦必则, 刘嵘. 1995. 秦岭-大别高压超高压变质带构造特征及构造演化. 高校地质学报, 1(2): 53~64.
[21]  杨志坚. 1964. 佛子岭群的地质时代问题. 地质论评, 22(5): 327~336.
[22]  杨文采, 程振炎, 陈国九,等. 1999a. 苏鲁超高压变质带北部地球物理调查(1)深反射地震.地球物理学报, 42(1): 41~52.
[23]  叶伯丹, 简平, 许俊文,等. 1993. 桐柏大别山北坡苏家河地体拼接带及其构成和演化. 武汉:中国地质大学出版社.
[24]  张增奇, 迟守祥, 宋志勇,等. 1994. 山东胶南岩群重新厘定及朋河石组的建立. 中国区域地质, 13(4): 354~356.
[25]  Ames L, Tilton G R, Zhou G. 1993. Timing of collision of the Sino-Korean and Yangtse cratons: U-Pb zircon dating of coesite-bearing eclogites. Geology, 21: 339~342.
[26]  Anhui Bureau of Geology and Mineral Resoueces. 1997. Stratigraphy of Anhui Province.Wuhan: China University of Geosciences Press(in Chinese).
[27]  Brown D, Spadea P. 1999. Processes of forearc and accretionary complex formation during arc-continental collision in the southern Ural Mountains. Geology, 27: 649~652.
[28]  Carswell D A, Wilson R N, Zhai M G. 2000. Metamorphic evolution, mineral chemistry and thermobarometry of schists and orthogneisses hosting ultra-high pressure eclogites in the Dabieshan of central China. Lithos., 52: 121~155.
[29]  Chen Daogong, Isachsen C, Zhi Xiachen, Zhou Taixi, Cheng Hao, Xia Qunke. 2000. Zircon U-Pb ages of gneiss from Qianshan in Anhui. Chinese Sci. Bull., 45(2): 214~217 (in Chinese).
[30]  Cheng Yuqi. 1994. Regional Geology Conspectus in China.Beijing: Geological Publishing House (in Chinese).
[31]  Cloos M. 1984. Flow melanges and the structural evolution of accretionary wedges. In: Melanges, Their Nature, Origin and Significance. Special Paper of the Geological Society of America, 198: 71~79.
[32]  Cowan D S. 1985. Structural styles in Mesozoic and Cenozoic melanges in the western Cordillera of North America. Geol. Soc. Am. Bull., 96: 451~462.
[33]  Dahlen F A.1990.Critical taper model of fold-and-thrust belts and accretionary wedges. Annu. Rev. Ear. Planet. Sci.,18:55~99.
[34]  Dong Shuwen, Wang Xiaofeng, Huang Dezhi, 1996a. Discovery of low-grade metavolcanic rock sheets within UHP belt in Dabieshan and its implications. Chinese Sci. Bull., 41(9): 815~820 (in Chinese).
[35]  Dong Shuwen, Zhang Yong, Huang Dezhi, 1996b. Geological feature of a tectonic window at Shiqiao within ultrahigh pressure metamorphic belt in North Jiangsu. Anhui Geology, 6(1): 9~13 (in Chinese with English abstract).
[36]  Du Jianguo, Zhang Peng, Jiang Junfeng. 1996. The division and comparison of the Beihuaiyang tectonic facies belts, Anhui. Anhui Geology, 6(1):19~27 (in Chinese with English abstract).
[37]  Fu Bin, Zheng Yongfei, Xiao Yilin, et al. 1998. Geochemical studies of eclogites and marbles from Sujiahe in the western Dabie Mountains. Acta Geologica Sinica, 72(4): 323~339 (in Chinese with English abstract).
[38]  Giunchi C, Richard Y. 1999. High-pressure/low-temperature metamorphism and the dynamics of an accretionary wedge. Geophys. J. Intern., 136: 620~628.
[39]  Hacker B R, Ratschbacher L, Webb L, McWilliams M O, Ireland T, Calvert A, Dong S, Wenk H-R, Chateigner D. 2000. Exhumation of ultrahigh-pressure continental crust in east central China: Late Triassic-Early Jurassic tectonic unroofing. J. Geophys. Res., B105: 13339~13364.
[40]  Hao Jie, Liu Xiaohan. 1988. The large thrust-decollement structure and its evolution of Tongbai-Dabie collision type orogenic belt. Scientia Geologica Sinica, (1):1~9 (in Chinese with English abstract).
[41]  Henan Bureau of Geology and Mineral Resoueces. 1997. Stratigraphy of Henan Province.Wuhan: China University of Geosciences Press (in Chinese).
[42]  Hu Shiling, Hao Jie, Li Yuejun, Dai Tongmo, Pu Zhiping. 1999. Laser probe 40Ar/39Ar isochron age of eclogite from Bixiling, Dabie UHP orogenic belt. Scientia Geologica Sinica, 34(4): 427~431 (in Chinese with English abstract).
[43]  Jiangsu Bureau of Geology and Mineral Resoueces. 1997. Stratigraphy of Jiangsu Province. Wuhan: China University of Geosciences Press (in Chinese).
[44]  Karig D E, Sharman G F. 1975. Subduction and accretion in trenchs. Geol. Soc. Am. Bull., 86: 377~389.
[45]  Leggett J K, McKerrow W S, Eales M H. 1979. The Southern Uplands of Scotland: a Lower Paleozoic accretionary prism. Jour. Geol. Soc. London, 136: 755~770.
[46]  Li S-G, Wang S-S, Chen Y-Z, Liu D-L, Qiu J, Zhou H-X, Zhang Z-M. 1994. Excess argon in phengite from eclogite: Evidence from dationg of eclogite minerals by Sm-Nd, Rb-Sr and 40Ar/39Ar methods, Chem.Geol., 112: 343~350.
[47]  Li S-G, Chen Y, Ge N. 1994. U-Pb dating of zircon from eclogite and gneiss from South Shangdong. Chinese Sci. Bull., 38(20): 1773~1777 (in Chinese).
[48]  Li S-G, Jagoutz E, Chen Y-Z, Li Q-L. 2000. Sm-Nd and Rb-Sr isotopic chronology and cooling history of ultrahigh pressure metamorphic rocks and their country rocks at Shuanghe in the Dabie Moumtains, Central China. Geochim. Cosmochim. Acta, 64: 1077~1093.
[49]  Li Yuejun, Hu Shiling, Jin Fuquan, et al. 1997. The genetic type of Yangshan Upper Paleozoic basin and its relation to the Tongbai-Dabie orogenic belt. Scientia Geologica Sinica, 32(1): 19~26 (in Chinese with English abstract).
[50]  Liou J G, Zhang R Y, Jahn B-M. 1997. Petrology, geochemistry and isotope data on a ultrahigh-pressure jadeite quartzite from Shuanghe, Dabie Mountains, East-central China. Lithos, 41: 59~78.
[51]  Ma Wenpu. 1991. The Carboniferous at the northern foot of the Dabie mountains and its tectonic implications. Acta Geologica Sinica, 65(1): 17~26 (in Chinese with English abstract).
[52]  Ma Wenpu, Liu Wencan, Wang Guosheng. 1997. Replacing of Meishan Group, north Dabie mountains and its correlation and tectonic implication. Geoscience, 11(1):95~101 (in Chinese with English abstract).
[53]  Mattauer M, Matte P, Malavieille J, Tapponnier P, Maluski H, Qin X Z, Lun L Y, Qin T Y. 1985. Tectonics of the Qinling Belt: Build-up and evolution of eastern Asia. Nature, 317: 496~500.
[54]  Moore J C, Vrolijk P. 1992. Fluids in accretionary prisms. Rev. Geophys., 30: 113~135.
[55]  Niu Baogui, Fu Yunlian, Liu Zhigang, et al. 1994. Main tectonothermal events and 40Ar/39Ar dating of the Tongbai-Dabie mts. Acta Geoscientia Sinica, 15(1~2):20~33(in Chinese with English abstract).
[56]  Okay A I, Sengor A M C, Satir M. 1993. Tectonics of an ultrahigh-pressure metamorphic terrane: the Dabie Shan/Tongbai Shan orogen, China. Tectonics, 12: 1320~1334.
[57]  Okay A I, Xu S-T, Sengor A M C. 1989. Coesite from the Dabieshan eclogites, Central China. Eur. J. Mineral., 1: 595~598.
[58]  Platt J P. 1986. Dynamics of orogenic wedges and the uplift of high-pressure metamorphic rocks. Geol. Soc. Am. Bull., 97: 1037~1053.
[59]  Qian Cunchao. 1996. Geological features and tectonic settings of low-grade metamorphic volcaniclastics within eclogite belt in Dabieshan. Anhui Geology, 6(2): 15~20 (in Chinese with English abstract).
[60]  Rowley D B, Xue F, Tucker R D, Peng Z X, Baker J, Davis A. 1997. Ages of ultrahigh pressure metamorphism and protolith orthogneisses from the eastern Dabie Shan: U/Pb zircon geochronology. Earth Planet. Sci. Lett., 151: 191~203.
[61]  Sengor A M C,Altmer D,Cin A,Ustaoemer.1988.Origin and assembly of the Tethyside orogenic collage at the expense of Gondwana Land. Geol. Soc. Spec. Publ. London,37:119~181.
[62]  Sengor A M C, Okurogullari A H. 1991. The role of accretionary wedges in the growth of continents: Asiatic examples from Argand to plate tectonics. Ecl. Geol. Helv., 84: 535~597.
[63]  Shandong Bureau of Geology and Mineral Resoueces. 1997. Stratigraphy of Shandong Province. Wuhan: China University of Geosciences Press (in Chinese).
[64]  Song Mingchun, Song Zhiyong. 1998. Some new pointviews on Pengheshi Group in Jiaonan orogen. Shandong Geology, 14(1): 25 (in Chinese).
[65]  von Huene R, Scholl D W. 1991. Observation at convergent margins concerning sediment subduction, subduction erosion, and the growth of continental crust. Rev. Geophys., 29: 279~316.
[66]  Wakabayashi J, Unruh J R. 1995. Tectonic wedging, blueschist metamorphism, and exposure of blueschists: are they compatible? Geology, 23: 85~88.
[67]  Wang Qingchen, Cong Bolin. 1998. Tectonic framework of the ultrahigh-pressure metamorphic zone from the Dabie Mountains. Acta Petrologica Sinica, 14(4): 481~492( in Chinese with English abstract).
[68]  Wang X-M, Zhang R Y, Liou J G. 1995. UHPM terrane in east central China. In: Coleman R, Wang X M, ed. Ultrahigh Pressure Metamorphism. Cambridge: Cambridge University Press, 356~390.
[69]  Warr L N, Primmer T J, Robinson D. 1991. Variscan very low-grade metamorphism in southwest England: a diastathermal and thrust-related origin. Jour. Metamor. Geol., 9: 751~764.
[70]  Windley B F. 1995. The Evolving Continents. 3rd Edition. Chichester: John Wiley and Sons, 526.
[71]  Wei Chunjing, Shan Zhenggang, Zhang Lifei, et al. 1996. Occurrence of eclogite in North Dabie and its geological significance. Chinese Science Bulletin, 42(17): 1832~1835 (in Chinese).
[72]  Xie Z, Chen J-F, Zhou T-X. 1998. U-Pb zircon ages of the rocks in the North Dabie terrain, China. Scientia Geologica Sinica, 7: 501~511.
[73]  Xie Zhi, Chen Jiangfeng, Dong Shuwen, Li Huimin, Zhou Taixi, Zuo Yicheng, Zhou Hongying. 1999. The zircon U-Pb ages of the low-grade metamorphic rocks in the southern part of Dabie Mountains, China. Acta Geoscientia Sinica, 20(4): 335~340 (in Chinese with English abstract).
[74]  Xu Shutong, Liu Yican, Jiang Laili, et al. 1994. Tectonic Regime and Evolution of the Dabie Mountains. Beijing: Science Press (in Chinese with English abstract).
[75]  Yang Weiran, Yang Kunguang, Liu Zhongming, et al.1999. Caledonian tectono thermal event in Tongbal-Dabei orogenic belt and its singnificance. Earth Science Frontiers, 6(4): 247~253 (in Chinese with English abstract).
[76]  Yang Wencai, Hu Zhengyuan, Cheng Zhenjiu, et al. 1999b. Long profile of geophysical investigation from Tanchen to Lianshui, east-central China. Chinese Journal of Geophysics, 42(2): 206~217 (in Chinese with English abstract).
[77]  Yin A, Nie S Y. 1993. An identation model for North and South China collision and the development of the Tan-Lu and Honam fault systems, eastern Asia. Tectonics, 12: 801~813.
[78]  Ye Boden, Xu Junwen, Li Zhichang, et al. 1991. Discovery of animal fossil within Sujiahe Group in Tongbai-Dabie region and its significance. China Geology, (3): 28~29 (in Chinese).
[79]  Zhang Guowei, Meng Qinren, Yu Zaiping, et al. 1996. Orogenic processes of Qinling orogenic belt and its dynamic features. Science in China (D), 26(3): 193~200 (in Chinese).
[80]  Zhang Zengqi, Chi Shouxiang, Song Zhiyong, et al. 1994. Redetermination of Jiaonan Group in Shandong and establishment of Pengheshi Group. Regional Geology of China, 13(4): 354~356 (in Chinese).
[81]  Zhao Da, Cheng Liren, Liu Maoxiu. 1995. The discovery of solenopora in the Wulian group in the Jiaonan area, Shandong, and its significance. Regional Geology of China, 14(4): 379~384 (in Chinese with English abstract).
[82]  Zheng Y-F, Fu B, Gong B, Xiao Y-L, Ge N-J. 1997. U-Pb dating of marble associated with eclogite from the Dabie Mauntains, East China. Chinese J. Geochem., 16(3): 193~201.
[83]  安徽省地质矿产局. 1987. 安徽省区域地质志. 北京:地质出版社.
[84]  曹荣龙, 朱寿华. 1995. 安徽碧溪岭含柯石英榴辉岩U-Pb和40Ar/39Ar年代学研究. 地球化学, 24(2): 152-161.
[85]  陈道公,Isachsen C, 支霞臣, 周泰禧,程昊,夏群科. 2000. 安徽潜山片麻岩锆石U-Pb年龄. 科学通报, 45(2): 214~217.
[86]  程裕淇. 1994. 中国区域地质概论. 北京:地质出版社.
[87]  杜建国, 张鹏, 姜俊峰. 1996. 安徽北淮阳地区构造岩相带的划分与对比. 安徽地质, 6(1): 19~27.
[88]  Howell D G. 1991. 地体构造学--山脉形成和大陆生长. 成都:四川科技出版社.
[89]  胡世玲, 郝杰, 李曰俊,等. 1999. 大别山碧溪岭榴辉岩激光探针40Ar- 39Ar年龄. 地质科学, 34(4): 427~431.
[90]  简平, 扬巍然, 李志昌, 周慧芳. 1997. 大别山西部熊店加里东期榴辉岩同位素地质年代学的证据. 地质学报, 71(2): 133~141.
[91]  简平. 1999. 大别山东部榴辉岩同位素体系和变质作用的关系. 地球学报, 20(4): 341~348.
[92]  金福全, 颜怀学, 吕培基. 1987. 北淮阳区地层研究的新进展. 合肥工业大学学报,(9): 3~10.
[93]  李曙光, 陈移之, 葛宁杰. 1994. 青岛榴辉岩及胶南片麻岩的锆石年龄. 科学通报, 38(20):1773~1777.
[94]  李曰俊, 胡世玲, 金福全,等. 1997. 扬山晚古生代沉积盆地成因类型及其与桐柏-大别造山带关系探讨. 地质科学, 32(1): 19-26.
[95]  刘贻灿, 徐树桐, 江来利,等. 1998. 大别山北部的变质复理石推覆体. 中国区域地质, 17(2): 156~162.
[96]  马文璞. 1991. 大别山北麓的石炭系及其大地构造意义. 地质学报, 65(1): 17~26.
[97]  聂宗笙. 1964. 大别山北麓石炭系划分对比问题. 地质论评, 22(6): 406~417.
[98]  钱存超. 1996. 大别山榴辉岩带中浅变质火山碎屑岩特征及其构造背景. 安徽地质, 6(2):15~20.
[99]  宋明春, 宋志勇. 1998. 对胶南造山带朋河石组的几点新认识. 山东地质, 14(1): 25.
[100]  苏育民. 1960. 大别山北麓变质岩系的时代问题. 地质论评, 20(6): 258~266.
[101]  王清晨, 从柏林. 1998. 大别山超高压变质带的大地构造框架. 岩石学报, 14(4): 481~492.
[102]  魏春景, 单振刚, 张立飞,等. 1996. 北大别榴辉岩的确定及其地质意义. 科学通报, 42(17): 1832~1835.
[103]  徐树桐, 刘贻灿, 江来利, 苏文, 季寿元. 1994. 大别山的构造格局与演化. 北京:科学出版社.
[104]  杨巍然, 王林森, 韩郁菁,等. 1994. 大别山蓝片岩榴辉岩年代学研究. 见:陈好寿主编,同位素地球化学研究. 杭州:浙江大学出版社,177~195.
[105]  杨巍然, 杨坤光, 刘忠明,等. 1999. 桐柏-大别造山带加里东期构造-热事件及其意义. 地学前缘, 6(4): 247~253.
[106]  杨文采, 胡振远, 程振炎,等. 1999b. 郯城-涟水综合地球物理剖面. 地球物理学报, 42(2): 206~217.
[107]  叶伯丹, 许俊文, 李志昌,等. 1991. 桐柏-大别山地区苏家河群动物化石的发现及其意义. 中国地质, (3): 28~29.
[108]  张国伟, 孟庆任, 于在平, 孙勇, 周鼎武, 郭安林. 1996. 秦岭造山带的造山过程及其动力学特征. 中国科学(D辑),26(3): 193~200.
[109]  张仁杰, 陈孝红. 1998. 桐柏-大别造山带苏家河群早奥陶世微体化石及其意义. 微体古生物学报, 15(2): 125~133.
[110]  赵达, 程立人,刘茂修. 1995. 胶南地区五莲群中管孔藻类的发现及其意义. 中国区域地质, 14(4): 379~384.
[111]  郑文武. 1964. 大别山东段"佛子岭群"的划分和时代问题. 地质论评, 22(5): 338~347.
[112]  周建波, 郑永飞, 李龙, 谢智. 2001. 大别-苏鲁超高压变质带内部的浅变质岩. 岩石学报, 17(1):39~48.
[113]  Ames L, Zhou G, Xiong B. 1996. Geochronology and geochemistry of ultrahigh-pressure metamophism with implications for collision of the Sino-Korean and Yangtze cratons, central China. Tectonics, 15: 472~489.
[114]  Anhui Bureau of Geology and Mineral Resoueces. 1987. Regional Geolgy of Anhui Province. Beijing:Geological Publishing House(in Chinese).
[115]  Cao Ronglong, Zhu Shouhua. 1995. U-Pb and 40Ar/39Ar geochronological studies of coesite-bearing eclogite at Bixiling in Anhui. Geochimica, 24(2): 152~161 (in Chinese with English abstract).
[116]  Carson B, Screaton E J. 1998. Fluid flow in accretionary prisms: evidence for focused, time-variable discharge. Rev. Geophys., 36: 329~351.
[117]  Chavagnac V, Jahn B-m. 1996. Coesite-bearing eclogites from the Bixiling Complex, Dabie Mountains, China: Sm-Nd ages, geochemical characteristics and tectonic implications. Chem. Geol., 133: 29~51.
[118]  Cheng Yuqi, Liu Dunyi, Williams I S, Jian Ping, et al. 2000. SHRIMP U-Pb dating of zircons of a dark-coloured eclogite and a garnet-bearing gneissic-granitic rock from Bixiling in eastern Dabie area. Acta Geologica Sinica, 74(3): 193~205 (in Chinese with English abstract).
[119]  Cloos M. 1983. Comparative study of melange matrix and metashales from the Franciscan subduction complex with the the basal Great Valley sequence, California. Jour. Geol., 91: 291~306.
[120]  Cong B L. 1996. Ultrahigh-Pressure Metamorphic Rocks in the Dabieshan-Sulu Region of China.Beijing: Science Press, 224.
[121]  Davis D, Suppe J, Dahlen F A. 1983. Mechanics of fold and thrust belts and accretionary wedges. J. Geophys, 88: 1153~1172.
[122]  Davis E E, Hyndman R D. 1989. Accretion and recent deformation of sediments along the northern Cascadia subduction zone. Geol. Soc. Am. Bull., 101: 1465~1480.
[123]  Ernst W G, Liou J G. 1995. Contrasting plate-tectonic styles of the Qinling-Dabie-Sulu and Franciscan metamorphic belts. Geology, 23: 253~256.
[124]  Hacker B R, Wang X, Eide E A, Ratschbacher L. 1996. Qinling-Dabie ultrahigh-pressure collisional orogeny. In:Yin A, Harrison T M, ed.The Tectonic Evolution of Asia. Cambridge: Cambridge University Press, 345~370.
[125]  Hacker B R, Ratschbacher L, Webb L, Ireland T, Walker D, Dong S. 1998. U/Pb zircon ages constrain the architecture of the ultrahigh-pressure Qinling-Dabie Orogen, China. Earth Planet. Sci. Lett., 161: 215~230.
[126]  Hamilton W B. 1988. Plate tectonics and island arcs. Geol. Soc. Am. Bull., 100: 1503~1527.
[127]  Henan Bureau of Geology and Mineral Resoueces. 1989. Regional Geolgy of Henan Province.Beijing: Geological Publishing House (in Chinese).
[128]  Jahn B-m. 1998. Geochemical and isotopic characteristics of UHP eclogites and ultramafic rocks of the Dabie orogen: implications for continental subduction and collisional tectonics. In: Hacker B, Liou J G, ed. When Continents Collide: Geodynamics and Geochemistry of Ultrahigh Pressure Rocks. Dordrecht: Kluwer Academic Publishing, 203~239.
[129]  Jian Ping, Yang Weiran, Li Zhichang, Zhou Huifang. 1997. Isotopic geochronological evidence for the Caledonian Xiongdian eclogite in the western Dabie Mountains, China. Acta Geologica Sinica, 71(2): 134~141 (in Chinese with English abstract).
[130]  Jin Fuquan, Yan Huaixue, Nue Peiji. 1987. New progress in the study of stratigraphy in Beihuaiyang region. Bulletin of Hefei University of Technology, (9): 3~10 (in Chinese).
[131]  Le Pichon X, Henry P, Lallemant S. 1993. Accretion and erosion in subduction zones: the role of fluids. Ann. Rev. Earth Planet. Sci., 21: 307~338.
[132]  Li S-G, Xiao Y-L, Liou D-L, Chen Y-Z, Ge N-J, Zhang Z-Q, Sun S-S, Cong B-L, Zhang R-Y, Hart S R, Wang S-S. 1993. Collision of the North China and Yangtze Blocks and formation of coesite-bearing eclogites: timing and processes. Chem. Geol.,109: 89~111.
[133]  Li Shuguang, Han Weili, Huang Fang, et al. 1998. Sm-Nd and Rb-Sr ages and geochemistry of volcanics from the Dingyuan Formation in Dabie Mountains, Central China: Evidence for the Paleozoic magmatic arc. Scientia Geologica Sinica, 7(4): 461~470.
[134]  Li S-G, Jagoutz E, Lo C-H, Chen Y-Z, Li Q-L, Xiao Y-L. 1999. Sm/Nd, Rb/Sr, and 40Ar/39Ar isotopic systematics of the ultrahigh-pressure metamorphic rocks in the Dabie-Sulu Belt, Central China: A Retrospective View. Intern. Geol. Review, 41:1114~1124.
[135]  Liou J G, Zhang R-Y, Eide E A, Wang X M, Ernst W G, Maruyama S. 1996. Metamorphism and tectonics of high-pressure and ultra-high-pressure belts in the Dabie-Sulu region, China. In: Harrison M T, Yin A, ed.The Tectonics of Asia. Cambridge: Cambridge University Press, 300~344.
[136]  Liu Ruoxin, Fan Qicheng, Li Huimin, Zhang Qi, Zhao Dasheng, Ma Baolin. 1995. The protolith nature of garnet peridotite-eclogite intrusion at Bixiling in Dabieshan as implied by isotope geochronology. Acta Petrologica Sinica, 11(3): 243~256 (in Chinese with English abstract).
[137]  Liu Yican, Xu Sutong, Jiang Laili. 1998. The meta-flysch nappe in the northern part of the Dabie mountains. Regional Geology of Chian, 17(2): 156~162 (in Chinese with English abstract).
[138]  Ma Xingyuan, Liu Cangshuan, Liu Guodong. 1986. Geoscience transest from Jiangsu Jiashan to Inner Mongolia Mandula.Beijing: Geological Publishing House (in Chinese).
[139]  McKerrow W S,Leggett J K,Eales M H.1977.Imbricate thrust model of the Southern Uplands of Scotland.Nature,267:237~239.
[140]  Moore J C. 1989. Tectonics and hydrogeology of accretionary prisms: role of the decollement zone. J. Struct. Geol., 11: 95~106.
[141]  Moores E M, Twiss R J. 1995. Tectonics. New York: W H Freeman and Company, 415.
[142]  Nie Zongsun. 1964. On division and comparison of Carboneceous stratigraphy in the norther Dabie Mountains. Geological Review, 22(6): 406~417 (in Chinese).
[143]  O?Hara K D, Yang X-Y, Xie G-Y, Li Z-C. 1997. Regional δ18O gradients and fluid-rock interaction in the Altay accretionary complex, northwest China. Geology, 25: 443~446.
[144]  Oliver N H S. 1996. Review and classification of structural controls on fluid flow during regional metamorphism. J. Metamorph. Geol., 14: 477~492.
[145]  Ring U, Brandob M T. 1999. Ductile deformation and mass loss in the Franciscan subduction complex: implications for exhumation processes in accretionary wedges. In: Ring U, Brandon M T, Lister G S, Willett S D, ed. Exhumation Processes: Normal Faulting, Ductile Flow and Erosion. Geological Society Special Publications, 154: 55~86.
[146]  Schulmann K, Gayer R. 2000. A model for a continental accretionary wedge developed by oblique collision: the NE Bohemian Massif. J. Geol. Soc. London, 157: 401~416.
[147]  Sengor A M C, Natal?n B A, Burtman V S. 1993. Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia. Nature, 364: 299~304.
[148]  Shandong Bureau of Geology and Mineral Resoueces. 1987. Regional Geolgy of Shandong Province. Beijing: Geological Publishing House (in Chinese).
[149]  Shi Danian, Jiang Mei, Peng Cong, et al. 1999. Results on the crustal strusture of the eastenrn Dabie orogenic belt from the Seismic tomography and wide-angle reflection studies. Acta Seismologica Sinica, 21(4): 403~410 (in Chinese).
[150]  Su Yuming. 1960. On the times of metamorphic rocks in the northern Dabie Mountains. Geological Review, 20(6): 258~266.
[151]  Tan Yingjia. 1997. An Attribution of Meishan group and discussion on some questions about geological structures in Beihuaiyang area. Geoscience, 11(2):221~228 (in Chinese with English abstract).
[152]  Tang Jiafu, Qian Cunchao, Gao Tianshan. 1995. Association of low-grade metamorphic volcaniclastics within eclogite belt in Dabieshan and its geological significance. Anhui Geology, 5(2): 29~36 (in Chinese with English abstract).
[153]  Tarbuck E J, Lutgens F K. 1994. Earth Science. 7th Edition. New York: Macmillan College Publishing Company.
[154]  Wakabayashi J. 1992. Nappes, tectonics of oblique plate convergence, and metamorphic evolution related to 140 million years of continuous subduction, Franciscan Complex, California. Jour. Geol., 100: 19~40.
[155]  Wang Qincheng, Cong Bolin. 1999. Exhumation of UHP terranes: a case study from the Dabie Mountains, eastern China. Intern. Geol., Rev., 41: 994~1004.
[156]  Wang X-M, Liou J G, Mao H-K. 1989. Coesite-bearing eclogites from the Dabie Mountains in central China. Geology, 17: 1085~1088.
[157]  Warr L N, Greiling R O, Zachrisson E. 1996. Thrust related very low grade metamorphism in the marginal part of an orogenic wedge, Scandinavian Caledonides. Tectonics, 15: 1213~1229.
[158]  Webb L E, Hacker B R, Ratschbacher L, McWilliams M O, Dong S. 1999. Thermochronological constraints on deformation and cooling history of high- and ultrahigh-pressure rocks in the Qinling-Dabie orogen, eastern China. Tectonics, 18: 621~638.
[159]  Xu S T, Okay A I, Ji S Y, Sengor A M C, Su W, Liu Y-C, Jiang L-L. 1992. Diamond from the Dabie Shan metamorphic rocks and its implication for tectonic setting. Science, 256: 80~82.
[160]  Yang Weiran, Wang Lisen, Han Yujing, Zhang Zemin, Liu Rong. 1994. A study on geochronology of the Dabie blueschists-eclogites in central China. In: Chen Haoshou, ed. Studies of Isotope Geochemistry. Hangzhou:Zhejiang University Press, 177~186 (in Chinese).
[161]  Yang Weiran, You Zhengdong, Han Yuqing, Zhang, et al. 1995. The tectonic characteristics and evolution of the Qinling-Dabie high-pressure and ultrahigh-pressere metamorphic belt, Central China. Geological Journal Uneversities, 1(2): 53~64 (in Chinese with English abstract).
[162]  Yang Wencai, Cheng Yanjiu, Chen Guojiu, et al. 1999a. Geophysical investigations in northern Sulu UHPM belt, part I:deep seismic reelection. Chinese Journal of Geophysics, 42(1):41~52 (in Chinese with English abstract).
[163]  Yang Zhijian. 1964. On the geological times of Foziling Group. Geological Review, 22(5): 327~336 (in Chinese).
[164]  Ye Boden, Jian Ping, Xu Junwen, et al. 1993. The Sujiahe Terrane Collage Belt and Its Constitution and Evolution along the North Hillslope of the Tongbai-Dabie Orogenic Belt.Wuhan: Press of China University of Geosciences, 81 (in Chinese with English abstract).
[165]  Zhang R Y, Liou J G. 1998. Ultrahigh-pressure metamorphism of the Sulu terrane, eastern China: a prospective review. Cintinental Dynamics, 3: 32~53.
[166]  Zhang Renjie, Cheng Xiaohong. 1998. The discovery of early ordovician microfossils from the Sujiahe group of Tongbo-Dabie orogenic belt and its significances. Acta Micropalaeonlogogica Sinica, 15(2): 125~133 (in Chinese with English abstract).
[167]  Zheng Wenwu. 1964. Division of Foziling Group in eastern Dabie and its times. Geological Review, 22(5): 338~347 (in Chinese).
[168]  Zhou Jianbo, Zheng Yongfei, Li Long, Xie Zhi. 2001. On low-grade metamorphic rock within Dabie-Sulu ultrahigh pressure metamorphic belt. Acta Petrologica Sinica,17(1): 39~48 (in Chinese with English abstract).

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