• 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

    东吴运动性质的厘定及其时空演变规律

    何斌 徐义刚 王雅玫 肖龙

    何斌, 徐义刚, 王雅玫, 肖龙, 2005. 东吴运动性质的厘定及其时空演变规律. 地球科学, 30(1): 89-96.
    引用本文: 何斌, 徐义刚, 王雅玫, 肖龙, 2005. 东吴运动性质的厘定及其时空演变规律. 地球科学, 30(1): 89-96.
    HE Bin, XU Yi-gang, WANG Ya-mei, XIAO Long, 2005. Nature of the Dongwu Movement and Its Temporal and Spatial Evolution. Earth Science, 30(1): 89-96.
    Citation: HE Bin, XU Yi-gang, WANG Ya-mei, XIAO Long, 2005. Nature of the Dongwu Movement and Its Temporal and Spatial Evolution. Earth Science, 30(1): 89-96.

    东吴运动性质的厘定及其时空演变规律

    基金项目: 

    国家自然科学基金重点项目 40234046

    中国科学院知识创新工程项目 A15-041107

    国家“973”项目 G1999043205

    详细信息
      作者简介:

      何斌(1963-), 男, 博士后, 副教授, 主要从事构造地质学研究.E-mail: hebin@gig.ac.cn

    • 中图分类号: P542

    Nature of the Dongwu Movement and Its Temporal and Spatial Evolution

    • 摘要: 东吴运动是华南地区二叠纪影响较大的一次地壳运动, 然而对其涵义、起始时间、构造界面位置、影响范围和运动属性等方面一直存在争议.通过对上扬子茅口组对比、不整合面特征和岩浆活动等方面的研究, 结合对华南地区二叠纪的地层、沉积及岩相古地理等综合分析, 对东吴运动的性质、地球动力学背景和时空演变规律进行了探讨.认为茅口末期峨眉山地幔柱上升引起的地壳抬升、峨眉山玄武岩的喷发和东吴运动这三者之间存在成因联系; 上扬子中晚二叠世之间的东吴运动是峨眉山地幔柱上升所造成的地壳快速差异抬升.东吴运动具有明显的时空演变规律, 空间上西强东弱、南强北弱, 时间上西早东晚、南早北晚.下扬子及华南地块可能不存在东吴运动, 其中晚二叠世的沉积作用主要受华夏古陆控制.

       

    • 图  1  峨眉山大火成岩省上扬子茅口组差异剥蚀平面图

      1.峨眉山玄武岩; 2.地层剖面位置; 3.联合剖面位置; 4.茅口组等厚线(m); 5.剥蚀程度分界线; 6.断层

      Fig.  1.  Emeishan large igneous rock province and differential erosion of Maokou Formation in the Upper Yangtze block

      图  2  上扬子茅口组地层对比联合剖面

      Fig.  2.  Biostratigraphic correlation of the Maokou Formation in the Upper Yangtze block

      图  3  华南地区二叠系年代地层对比剖面(a)和峨眉山地幔柱上升引起的地壳抬升示意图(b)

      Fig.  3.  Chronostratigraphic correlation of the Permian across South China (a) and a sketch showing the crust uplift caused by rising of the Emeishan mantle-plume (b)

    • Bureau of Geology and Mineral Resources of Jiangsu Province, 1982. Regional geology of Jiangsu Province and Shanghai area. Geological Publishing House, Beijing, 487(in Chinese).
      Campbell, I. H., Griffiths, R. W., 1990. Implications of mantle plume structure for the evolution of flood basalts. Earth and Planetary Science Letters, 99: 79-93. doi: 10.1016/0012-821X(90)90072-6
      Chen, X. Q., Liu, Y. K., Tong, P., 1987. Query about Dongwu movement and new opinion on Chuanqian movement. Oil & Gas Geology, 8(4): 1-13(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-SYYT198704013.htm
      Chen, Z. L., Chen, S. Y., 1987. Tectonic evolution of the western margin of Yangtze block. Chongqing Publishing House, Chongqing, 236(in Chinese).
      Cox, K. G., 1989. The role of mantle plumes in the development of continental drainage patterns. Nature, 342: 873-877. doi: 10.1038/342873a0
      Dam, G., Larsen, M., Sonderholm, M., 1998. Sedimentary response to mantle plumes: Implications from Paleocene onshore successions, West and East Greenland. Geology, 26: 207-210.
      Editing Committee of Stratigraphy in China, 2000. Permian in China. Geological Publishing House, Beijing, 147(in Chinese).
      Feng, S. N., 1991. New knowledge on Dongwu movement. Geoscience, 5(4): 378-384(in Chinese with English abstract).
      Feng, Z. Z., Jin, Z. K., Yang, Y. Q., et al., 1994. Lithofacies paleogeography of Permian of Yunnan-Guizhou-Guangxi region. Geological Publishing House, Beijing, 146(in Chinese).
      He, B., Wang, Y. M., Jiang, X. W., 2004. Paleo-karst landforms on the top of Maokou Formation in the west of the Upper Yangtze platform and its geological significance. Geology in China, 1: 50-55(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI200401005.htm
      He, B., Xu. Y. G., Xiao, L., et al., 2003. Generation and spatial distribution of the Emeishan large igneous province: New evidence from stratigraphic records. Acta Geologica Sinica, 77: 194-202(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200302012.htm
      Hu, S. Z., 1994a. On the event of Dongwu movement and its relation with Permian subdivision. Journal of stratigraphy, 18(4): 309-315(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DCXZ404.015.htm
      Hu, S. Z., 1994b. The event of Dongwu movement should be ideal separation boundary between Upper and Lower Permian. Geology of Coal Mine in the Southeast of China, 1 (11): 16-20(in Chinese with English abstract).
      Huang, J. Q., Chen, B. W., 1987. The evolution of Tethy sea in China and its adjacent area. Geological Publishing House, Beijing, 249(in Chinese).
      Institute of Geology, Chinese Academy of Sciences, 1979. Study of karst in China. Science Press, Beijing, 285(in Chinese).
      Li, R. N., 1989. New knowledge on boundary between Upper and Lower Permian in the foreland of Daba Mountain: A discussion on Dongwu movement. Acta Geologica Sinica of Sichuan Province, 8(2): 16-23(in Chinese with English abstract).
      Li, S. G., 1931. Variscan orogeny of the southeast of China. Bull. Geol. Soc. China, 11(2): 200-217.
      Li, W. H., 1992. "Dongwu movement" should be not boundary between Upper and Lower Permian. Journal of Stratigraphy, 16(2): 138-141(in Chinese with English abstract).
      Liang, D. Y., Nie, Z. T., Song, Z. M., 1994. Extensional Dongwu movement in the western margin of Yangtze region. Earth Science—Journal of China University of Geosciences, 19(4): 443-453(in Chinese with English abstract).
      Wang, L. T., Lu, Y. B., Zhao, S. J., et al., 1994, Permian lithofacies, paleogeography and mineralization in South China. Geological Publishing House, Beijing, 147(in Chinese).
      White, R., McKenzie, D., 1995. Mantle plumes and flood basalts. Journal of Geophysical Research, 100: 17543-17585. doi: 10.1029/95JB01585
      Wignall, P. B., 2001. Large igneous provinces and mass extinctions. Earth Science Reviews, 53: 1-33. doi: 10.1016/S0012-8252(00)00037-4
      Xu, Y. G., 2002. Mantle plumes, large igneous provinces and their geologic consequences. Earth Science Frontiers, 9 (4): 341-353(in Chinese with English abstract).
      Yi, Z. X., Xu, D. Y., Pu, Q. Y., 1965. Collection of names of crustal movements in China. Geological Review, 23(Suppl.): 20-81(in Chinese with English abstract).
      Zhang, Z. Q., 1983. On Dongwu movement. Geology and Exploration of Coal Mine, (3): 14-21(in Chinese with English abstract).
      江苏省地质矿产局, 1982. 江苏省及上海地区区域地质志. 北京: 地质出版社, 487.
      陈显群, 刘应楷, 童鹏, 1987. 东吴运动质疑及川黔运动之新见. 石油及天然气地质, 8(4): 1-13. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT198704013.htm
      陈智梁, 陈世瑜, 1987. 扬子地块西缘地质构造演化. 重庆: 重庆出版社, 236.
      中国地层典编委会, 2000. 中国地层典———二叠系. 北京: 地质出版社, 147.
      冯少南, 1991. 东吴运动的新认识. 现代地质, 5(4): 378-384. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ199104003.htm
      冯增昭, 金振奎, 杨玉卿, 等, 1994. 滇黔桂地区二叠纪岩相古地理. 北京: 地质出版社, 146.
      何斌, 王雅玫, 姜晓玮, 2004. 茅口灰岩顶部古喀斯特地貌的厘定. 中国地质, 1: 50-55. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200401005.htm
      何斌, 徐义刚, 肖龙, 等, 2003. 峨眉山大火成岩省的形成机制及空间展布: 来自沉积地层学研究的新证据. 地质学报, 77: 194-202. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200302012.htm
      胡世忠, 1994a. 论东吴运动构造事件与二叠纪分统界线问题. 地层学杂志, 18(4): 309-315. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ404.015.htm
      胡世忠, 1994b. 东吴运动构造事件应是上下二叠统的理想界线. 中国东南煤田地质, 1(11): 16-20.
      黄汲清, 陈炳蔚, 1987. 中国及邻区特提斯海的演化. 北京: 地质出版社, 249.
      中国科学院地质研究所岩溶研究组, 1979. 中国岩溶研究. 北京: 科学出版社, 285.
      李汝宁, 1989. 大巴山前缘上下二叠统分界的新认识———兼论东吴运动. 四川地质学报, 18(2): 16-23. https://www.cnki.com.cn/Article/CJFDTOTAL-SCDB198902003.htm
      李文恒, 1992. "东吴运动"不应做为上下二叠统的界线. 地层学杂志, 16(2): 138-141. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ199202008.htm
      梁定益, 聂泽同, 宋志敏, 1994. 扬子西缘东吴伸展运动. 地球科学———中国地质大学学报, 19(4): 443-453. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX199404007.htm
      王立亭, 陆彦邦, 赵时久, 等, 1994. 中国南方二叠纪岩相古地理与成矿作用. 北京: 地质出版社, 147.
      徐义刚, 2002. 地幔柱构造、大火成岩省及其地质效应. 地学前缘, 9(4): 341-353. doi: 10.3321/j.issn:1005-2321.2002.04.014
      尹赞勋, 徐道一, 浦庆余, 1965. 中国地壳运动名称资料汇编. 地质论评, 23(增刊): 20-81. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP1965S1003.htm
      张祖圻, 1983. 论东吴运动. 煤田地质与勘探, (3): 14-21. https://www.cnki.com.cn/Article/CJFDTOTAL-MDKT198303002.htm
    • 加载中
    图(3)
    计量
    • 文章访问数:  4022
    • HTML全文浏览量:  527
    • PDF下载量:  14
    • 被引次数: 0
    出版历程
    • 收稿日期:  2004-04-28
    • 刊出日期:  2005-01-25

    目录

      /

      返回文章
      返回