• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    留言板

    尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

    姓名
    邮箱
    手机号码
    标题
    留言内容
    验证码

    苏鲁造山带北侧构造演化的几何学运动学特征

    吴冲龙 张善文 毛小平 柳忠泉 宋立军 佟彦明

    吴冲龙, 张善文, 毛小平, 柳忠泉, 宋立军, 佟彦明, 2006. 苏鲁造山带北侧构造演化的几何学运动学特征. 地球科学, 31(6): 817-822.
    引用本文: 吴冲龙, 张善文, 毛小平, 柳忠泉, 宋立军, 佟彦明, 2006. 苏鲁造山带北侧构造演化的几何学运动学特征. 地球科学, 31(6): 817-822.
    WU Chong-long, ZHANG Shan-wen, MAO Xiao-ping, LIU Zhong-quan, SONG Li-jun, TONG Yan-ming, 2006. Geometry and Kinematics of Tectonic Evolution in Northern Part of Sulu Orogenic Belt. Earth Science, 31(6): 817-822.
    Citation: WU Chong-long, ZHANG Shan-wen, MAO Xiao-ping, LIU Zhong-quan, SONG Li-jun, TONG Yan-ming, 2006. Geometry and Kinematics of Tectonic Evolution in Northern Part of Sulu Orogenic Belt. Earth Science, 31(6): 817-822.

    苏鲁造山带北侧构造演化的几何学运动学特征

    基金项目: 

    国家攻关项目 2004B616A-06-01

    详细信息
      作者简介:

      吴冲龙(1945-),男,教授,博士生导师,从事矿产普查勘探和地学信息工程的教学与科研工作.E-mail:wucl@eug.edu.cn

    • 中图分类号: P542

    Geometry and Kinematics of Tectonic Evolution in Northern Part of Sulu Orogenic Belt

    • 摘要: 横穿诸城凹陷的南北向反射地震剖面揭示, 苏鲁造山带北侧边界的中上地壳中存在着三层结构, 即上部的胶莱盆地沉积盖层、中部的苏鲁楔状地体和下部代表华北板块的胶北地体; 诸城凹陷边缘和内部断裂均显示同沉积正断层性质, 苏鲁楔状地体中发育一组向北仰起的叠瓦状逆冲断层, 而胶北地体显示了向南俯冲的态势.由此而论, 可能存在着华北板块与扬子板块相向俯冲于苏鲁地体之下的陆陆碰撞机制, 苏鲁地体可能具有与大别地体相似的花状造山带结构.

       

    • 图  1  地震测线位置与诸城凹陷地质简图(据胜利石油管理局地质研究院, 2003)

      1.第四系; 2.王氏群上部; 3.王氏群下部; 4.中白垩统大盛群; 5.中下白垩统青山群; 6.下白垩统莱阳群

      Fig.  1.  Location of seismic lines and the geology map of Zhucheng sag

      图  2  胶莱盆地西南部南北向692.9地震测线(A-A′) 构造解释剖面

      Fig.  2.  Structure interpretation profile of S-N-strike seismic line 692.9 (A-A′) in the southwest part of Jiaolai basin

      图  3  胶莱盆地西南部南北向696.1地震测线(B-B′) 反射地震叠加偏移剖面与层速度结构(图中等值线单位为m/s)

      Fig.  3.  Reflecting seismic migration profile and its velocity structure of S-N-strike seismic line 696.1 (B-B′) in the southwest part of Jiaolai basin

      图  4  胶莱盆地西南部南北向696.1地震测线(B-B′) 构造解释剖面(图例同图 2)

      Fig.  4.  Structure interpretation profile of S-N-strike seismic line 696.1 (B-B′) in the southwest part of Jiaolai basin

      图  5  苏鲁花状造山带结构和南北两侧的双俯冲模式

      Fig.  5.  Structure of Sulu orogenic belt and both dive pattern in its south and north

    • [1] Banno, S., Enami, M., Hiraji ma, T., et al., 2000. Decom-pression P-T path of coesite eclogite to granulite fromWeihai, eastern China. Lithos, 52: 97-108. doi: 10.1016/S0024-4937(99)00086-9
      [2] Cao, G. Q., 1990. Preli minary discusston on"Jiaonan terra-ne". Geology of Shandong, 6 (2): 1-10 (in Chinese with English abstract).
      [3] Chen, W. J., Harrison, T. M., Heizerler, M. T., et al., 1992. The cooling history of mélange zone in North Jiangsu-South Shandong region: Evidence from multiple diffusion domain 40Ar-39Ar thermal geochronology. Acta Petrologica Sinica, 8 (1): 1-17 (in Chinese with English abstract). doi: 10.3321/j.issn:1000-0569.1992.01.001
      [4] Eide, E. A., Mc Williams, M. O., Liou, J. G., 1994. 40Ar-39Argeochronology and exhumation of high-pressure to ultrahigh pressure metamorphic rocks in East Central China. Geology, 22: 601-604.
      [5] Faure, M., Breton, N. L., Lin, W., et al., 2002. Where is theNorth China-South China block boundary in easternChina?Reply. Geology, 30: 668.
      [6] Faure, M., Lin, W., Le Breton, N., 2001. Where is theNorth China-South China block boundary in easternChina? Geology, 29: 119-122.
      [7] Lin, W., Michel, F., Wang, Q. C., 2003. Mesozoic geometryand kinematics in the Jiaodong Peninsula and itstectonic evolution. Chinese Journal of Geology, 38 (4): 495-505 (in Chinese with English abstract).
      [8] Ling, X. C., 1996. Basic characteristics and boundaries of Ludong orogenic belt. Journal of Harbin University of Civil Engineering and Architecture, 31 (5): 116-121 (in Chinese with English abstract).
      [9] Ma, Z. T., Liu, H. Q., Ma, Z. X., 1997. Features of gravityand magnetic fields and geological explanation of theJiaonan orogenic belt and its neighbour areas. Geologyof Shandong, 13 (1): 92-102 (in Chinese with English abstract).
      [10] Suo, S. T., Zhong, Z. Q., You, Z. D., et al., 2000. Relic UHP structures in Dabie-Sulu region, China: Structural ex-pression and geodynamic significance. Earth Science—Journal of China University of Geosciences, 25 (6): 557-563 (in Chinese with English abstract).
      [11] Wallis, S., Hiraji ma, T., Banno, S., 1999. The Sulu UHP terrane: A review of the petrology and structural geology. International Geol. Rev. , 41: 906-920. doi: 10.1080/00206819909465178
      [12] Wang, Q. C., Cong, B. L., 1998. Tectonic framework of theultra-high pressure metamorphic zone from the Dabie Mountains. Acta Petrologica Sinica, 14 (4): 481-492 (in Chinese with English abstract).
      [13] Wang, Q. C., Zhang, R. Y., Cong, B. L., et al., 1992. Eclogites in eastern Shandong-northem Jiangsu region: Their structure and exhumation mechanism. Acta Petrologica Sinica, 8 (2): 153-160 (in Chinese with English abstract).
      [14] Wu, Y. B., Zheng, Y. F., Zhou, J. B., 2004. Neoproterozoicgranitoidin northwest Sulu andits bearing onthe North China-South China blocks boundary in east China. Geophysical Research Letters, 31, L07616, doi: 10.1029/2004GL019785.
      [15] Xu, G. Z., Zhou, R., Yan, Z., et al., 2001. Discussion onthe evidences of Mesozoic lithosphere thinning and its dynamicmechanismin Jiaodong area. Geotectonica et Metallogenia, 25 (4): 368-380 (in Chinese with English abstract).
      [16] Xu, Z. Q., Zhang, J. X., Xu, H. F., 1997. Ductile shear zoneand dynamics of main continental mountain chain inChina. Geological Publishing House, Beijing (in Chinese).
      [17] Yang, T. N., Xu, H. F., Song, M. C., et al., 1997. Uplift-extension structure of the Jiaonan block. Geology of Shandong, 13 (1): 67-76 (in Chinese with English abstract).
      [18] Yang, W. C., Chen, Z. Y., Cheng, G. J., et al., 1999. Geophysical investigations in northern Sulu UHPM belt, Part I: Deep seismic reflection. Chinese Journal of Geophysics, 42 (1): 41-52 (in Chinese with English abstract).
      [19] Yang, W. C., Cheng, Z. Y., Zhang, C. H., 2003. Geophysical investigation for site-selection of Chinese Continental Scientific Drilling and Dabie-Sululithosphere. Acta Geoscientia Sinica, 24 (5): 391-404 (in Chinese with English abstract).
      [20] Zhai, M. G., 2002. Where is the North China-South Chinablock boundary in eastern China? Comment. Geology, 30: 667.
      [21] Zhang, G. W., Meng, Q. R., Liu, S. F., et al., 1997. Huge intra-continental subductionzone at south margin of North Chinablock and present 3D lithospheric framework of the Qinling orogenic belt. Geological Journal of China Universities, 3 (2): 129-143 (in Chinese with English abstract).
      [22] Zhang, J. X., Yang, T. N., Xu, Z. Q., et al., 1997. Extension of Jiaonan areain Shandong. Acta Geoscientia Sinica, 18 (2): 122-128 (in Chinese with English abstract).
      [23] 曹国权, 1990. 试论"胶南地体". 山东地质, 6 (2): 1-10. https://www.cnki.com.cn/Article/CJFDTOTAL-SDDI199002000.htm
      [24] 陈文寄, Harrison, T. M., Heizerler, M. T., 等, 1992. 苏北-胶南构造混杂岩冷却历史的多重扩散域40Ar-39Ar热年代学研究. 岩石学报, 8 (1): 1-17. doi: 10.3321/j.issn:1000-0569.1992.01.001
      [25] 林伟, Michel, F., 王清晨, 2003. 胶东半岛中生代构造演化的几何学和运动学. 地质科学, 38 (4): 495-505. doi: 10.3321/j.issn:0563-5020.2003.04.008
      [26] 凌贤长, 1996. 鲁东造山带基本特征及边界确定. 哈尔滨建筑大学学报, 31 (5): 116-121. https://www.cnki.com.cn/Article/CJFDTOTAL-HEBJ805.021.htm
      [27] 马兆同, 刘慧勤, 马兆祥, 1997. 胶南造山带及邻近地区的重磁特征及地质解释. 山东地质, 13 (1): 92-102. https://www.cnki.com.cn/Article/CJFDTOTAL-SDDI199701009.htm
      [28] 索书田, 钟增球, 游振东, 等, 2000. 大别-苏鲁区残余超高压构造及其动力学意义. 地球科学——中国地质大学学报, 25 (6): 557-563. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200006001.htm
      [29] 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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB804.006.htm
      [30] 王清晨, 张儒瑗, 从柏林, 等, 1992. 鲁东-苏北榴辉岩的构造特征及其折返机制. 岩石学报, 8 (2): 153-160. doi: 10.3321/j.issn:1000-0569.1992.02.005
      [31] 徐贵忠, 周瑞, 闫臻, 等, 2001. 论胶东地区中生代岩石圈减薄的证据及其动力学机制. 大地构造与成矿学, 25 (4): 368-380. doi: 10.3969/j.issn.1001-1552.2001.04.003
      [32] 许志琴, 张建新, 徐惠芬, 1997. 中国主要大陆山链韧性剪切带及动力学. 北京: 地质出版社, 1-246.
      [33] 杨天南, 徐惠芬, 宋明春, 等, 1997. 胶南地块的隆升-伸展构造. 山东地质, 13 (1): 67-76. https://www.cnki.com.cn/Article/CJFDTOTAL-SDDI199701006.htm
      [34] 杨文采, 程振炎, 陈国九, 等, 1999. 苏鲁超高压变质带北部地球物理调查(Ⅰ)——深反射地震. 地球物理学报, 42 (1): 41-52. doi: 10.3321/j.issn:0001-5733.1999.01.005
      [35] 杨文采, 程振炎, 张春贺, 2003. 中国科学深钻选址地球物理调查与大别-苏鲁岩石圈. 地球学报, 24 (5): 391-404. doi: 10.3321/j.issn:1006-3021.2003.05.001
      [36] 张国伟, 孟庆任, 刘少峰, 等, 1997. 华北地块南部巨型陆内俯冲带与秦岭造山带岩石圈现今三维结构. 高校地质学报, 3 (2): 129-143. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX702.000.htm
      [37] 张建新, 杨天南, 许志琴, 等, 1997. 胶南地区的伸展作用——以胶南诸城一带为例. 地球学报, 18 (2): 122-128. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB702.001.htm
    • 加载中
    图(5)
    计量
    • 文章访问数:  3740
    • HTML全文浏览量:  87
    • PDF下载量:  9
    • 被引次数: 0
    出版历程
    • 收稿日期:  2006-02-26
    • 刊出日期:  2006-11-25

    目录

      /

      返回文章
      返回