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城口?房县断裂带的构造变形分析

DOI: 10.16539/j.ddgzyckx.2015.05.001, PP. 755-768

Keywords: 大巴山构造带,城口-房县断裂带,右行走滑,左行走滑

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Abstract:

城口?房县断裂带位于上扬子板块北缘,以其为界可进一步将大巴山构造带划分为南大巴山弧形构造带(南大巴山)和北大巴山逆冲推覆构造带(北大巴山)。城口?房县断裂带不仅控制着该地区的岩浆活动和沉积作用,同时对大巴山的构造演化起到了重要的主导作用。综合大量的野外调查、构造解析和显微构造观察,对城口?房县断裂带进行了分段性的构造解析,厘定出城口?房县断裂带发育两条不同走滑性质的走滑断裂带,并追踪其展布范围。右行走滑断裂带自西向东贯穿城口?房县断裂带,与扬子板块相对华北板块的斜向俯冲碰撞有关;左行走滑断裂带发育于城口?房县断裂带东段,形成于陆内造山阶段,并改造了东段早期的右行走滑构造。在板块碰撞造山之前,早期的城口?房县断裂带处于伸展环境中呈线状分布。在陆内逆冲推覆过程中,由于东西两侧砥柱的阻碍作用,城口?房县断裂带发生弧形弯曲呈现SW向弧形展布。

References

[1]  Lin J L, Fuller M and Zhang W Y. 1985. Preliminary Phanerozoic polar wander paths for the North and South China Blocks. Nature, 313: 444?449.
[2]  Liu S F, Steel R and Zhang G W. 2005. Mesozoic sedimentary basin development and tectonic implication, northern Yangtze Block, eastern China: Record of continent-continent collision. Journal of Asian Earth Sciences, 25: 9?27.
[3]  Macedo C and Marshak S. 1999. Controls on the geometry of fold-thrust belt salients. Geological Society of America Bulletin, 111(12): 1808?1822.
[4]  Meng Q R, Wang E C and Hu J M. 2005. Mesozoic sedimentary evolution of the northwest Sichuan basin: Implication for continued clockwise rotation of the South China block. Geological Society of America Bulletin, 117: 396?410.
[5]  Meng Q R and Zhang G W. 2000. Geologic Framework and Tectonic Evolution of the Qin ling Orogen, Central China. Tectonophysics, 323(3/4): 183?196.
[6]  Okay A I and Sengor A M C. 1992. Evidence for intracontinental thrust-related exhumation of the ultrahigh-pressure rocks in China. Geology, 20: 411?414.
[7]  Zhang G W, Meng Q R, Yu Z P, Sun Y, Zhou D W and Guo A L. 1996. Orogenesis and dynamics of the Qinling orogen. Science in China (Series D), 39: 225?234.
[8]  Zhao X X and Coe R S. 1987. Paleomagnetic constraints on the collision and rotation of North and South China. Nature, 327: 141?144.
[9]  董云鹏, 查显峰, 付明庆, 张茜, 杨钊, 张燕. 2008. 秦岭南缘大巴山褶皱?冲断推覆构造的特征. 地质通报, 27(9): 1493?1508.
[10]  何建坤, 卢华复, 朱斌. 1999. 东秦岭造山带南缘北大巴山构造反转及其动力学. 地质科学, 34(2): 139?153.
[11]  胡健民, 董树文, 孟庆任, 施炜, 陈虹, 武国利. 2008. 大巴山西段高川地体的构造变形特征及其意义. 地质通报, 27(12): 2031?2044.
[12]  胡健民, 施炜, 渠洪杰, 陈虹, 武国利, 田蜜. 2009. 秦岭造山带大巴山弧形构造带中生代构造变形. 地学前缘, 16(3): 49?68.
[13]  李岩峰, 曲国胜, 刘殊, 张虹. 2008. 米仓山、南大巴山前缘构造特征及其形成机制. 大地构造与成矿学, 32(3): 285?292.
[14]  李智武, 刘树根, 罗玉宏, 刘顺, 徐国强. 2006. 南大巴山前陆冲断带构造样式及变形机制分析. 大地构造与成矿学, 30(3): 294?304.
[15]  刘战庆, 裴先治, 丁仨平, 李佐臣, 李瑞保, 陈有?, 刘智刚, 张晓飞, 陈国超, 王学良. 2011. 南大巴山西北段镇巴-下高川地区地质构造解析. 地球科学与环境学报, 33(1): 54?63.
[16]  雒昆利, 端木和顺. 2001. 大巴山区早古生代基性火成岩的形成时代. 中国区域地质, 20(3): 262?266.
[17]  曲国胜, Joseph Canerot, 王宗起, 赵民. 1996. 造山带弧形构造――西昆仑?帕米尔弧及其预测. 地质科学, 31(4): 313?325.
[18]  沈军, 汪一鹏, 赵瑞斌, 陈杰, 曲国胜. 2001. 帕米尔东北缘及塔里木盆地西北部弧形构造的扩展特征. 地震地质, 23(3): 381?389.
[19]  王存智, 杨坤光, 徐扬, 程万强. 2009. 北大巴基性岩墙群地球化学特征、LA-ICP-MS锆石U-Pb 定年及其大地构造意义. 地质科技情报, 28(3): 19?26.
[20]  王二七, 孟庆任. 2008. 对龙门山中生代和新生代构造演化的讨论. 中国科学(D缉), 38(10): 1221?1233.
[21]  王瑞瑞, 张岳桥, 解国爱, 许怀智. 2011. 大巴山前陆弧形构造的成因: 来自砂箱实验的认识. 地质学报, 85(9): 1409?1419.
[22]  徐扬, 王存智, 程万强, 杨坤光. 2009. 南大巴前陆冲断带构造变形几何类型、分布特征及其成因分析. 大地构造与成矿学, 33(4): 497?507.
[23]  张国伟, 程顺有, 郭安林, 董云鹏, 赖绍聪, 姚安平. 2004. 秦岭?大别中央造山系南缘勉略古缝合带的再认识――兼论中国大陆主体的拼合. 地质通报, 23(9?10): 846?853.
[24]  张国伟, 董云鹏, 赖绍聪, 郭安林, 孟庆任, 刘少峰, 程顺有, 姚安平, 张宗清, 裴先治, 李三忠. 2003. 秦岭?大别造山带南缘勉略构造带与勉略缝合带. 中国科学(D辑), 33(12): 1121?1135.
[25]  张国伟, 张本仁, 袁学诚, 肖庆辉. 2001. 秦岭造山带与大陆动力学. 北京: 科学出版社: 1?805.
[26]  张岳桥, 施炜, 李建华, 王瑞瑞, 李海龙, 董树文. 2010. 大巴山前陆弧形构造带形成机理分析. 地质学报, 84(9): 1300?1315.
[27]  邹先武, 段其发, 汤朝阳, 曹亮, 崔森, 赵武强, 夏杰, 王磊. 2011. 北大巴山镇坪地区辉绿岩锆石SHRIMP U-Pb定年和岩石地球化学特征. 中国地质, 38(2): 282?291.
[28]  Dong S W, Gao R, Yin A, Guo T L, Zhang Y Q, Hu J M, Li J H, Shi W and Li Q S. 2013. What drove continued continent-continent convergence after ocean closure? Insights from high-resolution seismic-reflection profiling across the Daba Shan in central China. Geology, 41(6): 671?674.
[29]  Eide E A. 1993. Petrology, Geochronology, and Structure of High-pressure Metamorphic Rocks in Hubei Province, East-central China, and Their Relationship to Continental Collision. Ph. D. dissertation, Stanford University: 1?470.
[30]  Enkin R J, Yang Z, Chen Y and Courtillot V. 1992. Paleomagnetic constraints on the geodynamic history of the major blocks of China from Permian to the present. Journal of Geophysical Research, 97: 13953?13989.
[31]  Gilder S and Courtillot V. 1997. Timing of the North?South China collision from new Middle to Late Mesozoic paleomagnetic data from the North China Block. Journal of Geophysical Research, 102: 17713?17727.
[32]  Gilder S A, Leloup P H, Courtillot V, Chen Y, Coe R S, Zhao X, Xiao W, Halim N, Cogne J P and Zhu R. 1999. Tectonic evolution of the Tancheng-Lujiang (Tan-Lu) fault via Middle Triassic to Early Cenozoic paleomagnetic data. Journal of Geophysical Research, 104(B7): 15365?15390.
[33]  Hu J M, Chen H, Qu H J, Wu G L, Yang J X and Zhang Z Y. 2012. Mesozoic deformations of the Dabashan in the southern Qinling orogen, central China. Journal of Asian Earth Sciences, 47: 171?184.
[34]  Huang K N and Opdyke N D. 1991. Paleomagnetism of Jurassic rocks from southwestern Sichuan and the timing of the closure of the Qinling suture. Tectonophysics, 200: 299?316.
[35]  Nie S, Yin A, Rowley D B and Jin Y. 1994. Exhumation of the Dabie Shan ultra-high-pressure rocks and accumulation of the Songpan Ganze flysch sequence, central China. Geology, 22: 999?1002.
[36]  Sengor A M C, Gorur N and Saroglu F. 1985. Strike-slip faulting and related basin formation in zones of tectonic escape: Turkey as a case study // Biddle K T and Christe-Blick N. Strike-slip deformation, basin formation and sedimentation. Society Economic Paleontologist and Mineralogists, Special Publication, 37: 227?265.
[37]  Shi W, Zhang Y Q, Dong S W, Hu J M, Wiesinger M, Ratschbacher L, Jonckheere R, Li J H, Tian M, Chen H, Wu G L, Ma L C and Li H L. 2012. Intra-continental Dabashan orocline, southwestern Qinling, Central China. Journal of Asian Earth Sciences, 46(2): 20?38.
[38]  Tan X D, Kodama K P, Gilder S, Courtillot V and Cogne J P. 2007. Paleomagnetic evidence and tectonic origin of clockwise rotations in the Yangtze fold belt, South China Block. Geophysical Journal International, 168: 48?58.
[39]  Wang E, Meng Q R, Burchfiel B C and Zhang G W. 2003. Mesozoic large-scale lateral extrusion, rotation, and uplift of the Tongbai-Dabie Shan belt in east China. Geology, 31(4): 307?310.
[40]  Yang Z Y, Courtillot V, Besse J, Ma X H, Xing L S, Xu S J and Zhang J X. 1992. Jurassic paleomagnetic constraints on the collision of the North and South China Blocks. Geophysical Research Letters, 19: 577?580.
[41]  Yin A and Nie S. 1993. An indentation model for the North and South China collision and the development of the Tan-Lu and Honam fault systems, eastern Asia. Tectonics, 12: 801?813.
[42]  Yokoyama M, Liu Y Y, Halim N and Otofuji Y. 2001. Paleomagnetic study of Upper Jurassic rocks from the Sichuan basin: Tectonic aspects for the collision between the Yangtze Block and the North China Block. Earth and Planetary Science Letters, 193: 273?285.
[43]  Zhang H, Tan X D and Han Y L. 2007. Cretaceous synfolding remagnetization components revealing tectonic rotation of the middle Yangtze fold belt. Chinese Science Bulletin, 52(20): 2837?2846.
[44]  Zhang K J. 2002. Escape hypothesis for the North and South China collision and the tectonic evolution of the Qinling orogen, eastern Asia. Eclogae Geologicae Helvetiae, 95: 237?247.
[45]  Zhu G, Liu G S, Niu M L, Xie C L, Wang Y S and Xiang B W. 2009. Syn-collisional transform faulting of the Tan-Lu fault zone, East China. International Journal of Earth Sciences, 98(1): 135?155.

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