DING Daogui, LI Fengli. Mesozoic and Cenozoic diktyogenese in the Lower Yangtze region[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2020, 42(5): 687-697, 876. doi: 10.11781/sysydz202005687
Citation: DING Daogui, LI Fengli. Mesozoic and Cenozoic diktyogenese in the Lower Yangtze region[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2020, 42(5): 687-697, 876. doi: 10.11781/sysydz202005687

Mesozoic and Cenozoic diktyogenese in the Lower Yangtze region

doi: 10.11781/sysydz202005687
  • Received Date: 2020-06-22
  • Rev Recd Date: 2020-08-10
  • Publish Date: 2020-09-28
  • Three stages of metamorphic tectonic movements took place in the Lower Yangtze region due to the joint action of the Tethys and the Pacific plates from the Middle/Late Triassic to the Early/Middle Jurassic, the Late Jurassic to the Early Cretaceous, and the Late Cretaceous to the Tertiary. They made the Paleozoic basin basements undergo detachable progressive deformations, and formed foredeep basins in the Upper Triassic and Middle/Lower Jurassic. The translational strike-slip of a large-scale fault zone formed pyroclastic pull-apart basins in the Upper Jurassic-Lower Cretaceous. The Upper Cretaceous-Tertiary semi-graben basins, which are arranged in a domino style, are extensional basins formed by lithospheric extension and detachment structures. The three transformations promoted the formation, accumulation and redistribution of oil and gas.

     

  • [1]
    朱夏. 我国中新生界含油气盆地的大地构造特征及有关问题[M]//朱夏论中国含油气盆地构造. 北京: 石油工业出版社, 1986: 4-26.

    ZHU Xia. Geotectonic characteristics of Mesozoic and Cenozoic petroliferous basins in China[M]//ZHU Xia's discussion on China's petroleum basin. Beijing: Petroleum Industry Press, 1986: 4-26.
    [2]
    朱夏, 陈焕疆. 论中国油气盆地的构造演化[M]//朱夏论中国含油气盆地构造. 北京: 石油工业出版社, 1986: 8-60.

    ZHU Xia, CHEN Huanjiang. Discussions on geological evolution of petroliferous basins in China[M]// ZHU Xia's discussion on China's petroleum basin. Beijing: Petroleum Industry Press, 1986: 8-60.
    [3]
    朱夏, 陈焕疆. 中国大陆边缘构造和盆地演化[M]//朱夏论中国含油气盆地构造. 北京: 石油工业出版社, 1986: 87-93.

    ZHU Xia, CHEN Huanjiang. Tectonic evolution of the continental margin and basins in China[M]// ZHU Xia's discussion on China's petroleum basin. Beijing: Petroleum Industry Press, 1986: 87-93.
    [4]
    丁道桂, 王东燕, 刘运黎. 下扬子地区古生代盆地的改造变形[J]. 地学前缘, 2009, 16(4): 61-73. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200904009.htm

    DING Daogui, WANG Dongyan, LIU Yunli. Transformation and deformation of the Paleozoic basins in lower Yangtze areas[J]. Earth Science Frontiers, 2009, 16(4): 61-73. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200904009.htm
    [5]
    艾伦P A, 艾伦J R. 盆地分析: 原理与应用[M]. 陈全茂, 张学预, 李大成, 等译. 北京: 石油工业出版社, 1995: 1-384.

    Allen P A, Allen J R. Basin analysis: principles and applications[M]. CHEN Quanmao, ZHANG Xueyu, LI Dacheng, et al, trans. Beijing: Petroleum Industry Press, 1995: 1-384.
    [6]
    朱夏. 关于中国大陆边缘构造演化[J]. 海洋地质与第四纪地质, 1987, 7(3): 115-120. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198703020.htm

    ZHU Xia. Structure and evolution of continental margins in China[J]. Marine Geology and Quaternary Geology, 1987, 7(3): 115-120. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198703020.htm
    [7]
    XU Jinghua. Thin-skinned plate-tectonic model for collision-type orogenesis[J]. Scientia Sinica, 1981, 24(1): 100-110.
    [8]
    ENGEBRETSON D C, COX A, GORDON R G. Relative motions between oceanic and continental plates in the Pacific Basin[M]. [S. l. ]: Geological Society of America, 1985: 17.
    [9]
    朱光, 刘国生, DUNLAP W J, 等. 郯庐断裂带同造山走滑运动的40Ar/39Ar年代学据[J]. 科学通报, 2004, 49(2): 190-198. doi: 10.3321/j.issn:0023-074X.2004.02.015

    ZHU Guang, LIU Guosheng, DUNLAP W J, et al. Evidence from 40Ar/39Ar geochronology of syn-orogenic strike-slip movement along the Tanlu fault zone, eastern China[J]. Chinese Science Bulletin, 2004, 49(2): 190-198. doi: 10.3321/j.issn:0023-074X.2004.02.015
    [10]
    刘国生, 朱光, 牛漫兰, 等. 郯庐断裂带肥东段走滑40Ar/39Ar法定年[C]//中生代以来中国大陆板块作用过程学术研讨会论文摘要集. 合肥: 合肥工业大学, 2005: 22-23.

    LIU Guosheng, ZHU Guang, NIU Manlan, et al. The characteristics of strike-slip movements and 40Ar/39Ar dating of Feidong, Anhui, along Tanlu fault zone[C]// Abstracts of papers from academic conference on continental plates process since the Mesozoic era. Hefei: Hefei University of Technology, 2005: 22-23.
    [11]
    郝天珧, SUH M, 刘建华, 等. 黄海深部结构与中朝—扬子块体结合带在海区位置的地球物理研究[J]. 地学前缘, 2004, 11(3): 51-61. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200403008.htm

    HAO Tianyao, SUH M, LIU Jianhua, et al. Deep-structure and boundary belt position between Sino-Korea and Yangtze blocks in Yellow Sea[J]. Earth Science Frontiers, 2004, 11(3): 51-61. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200403008.htm
    [12]
    黄汲清, 任纪舜, 姜春发. 中国大地构造基本轮廓[J]. 地质学报, 1977, 51(2): 117-135. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE197702002.htm

    HUANG Jiqing, REN Jishun, JIANG Chunfa, et al. An outline of the tectonic characteristics of China[J]. Acta Geologica Sinica, 1977, 51(2): 117-135. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE197702002.htm
    [13]
    朱夏. 关于盆地研究的几点意见[J]. 石油实验地质, 1980, 2(3): 19-24. doi: 10.11781/sysydz198003019

    ZHU Xia. Comments on basin research[J]. Petroleum Geology & Experiment, 1980, 2(3): 19-24. doi: 10.11781/sysydz198003019
    [14]
    DAVIS G A, ZHENG Y. A possible cordilleran type metamorphic core complex beneath the Great Wall near Hefangkou, Huairou County, northern China[J]. Geologica Society of America Abstracts with Programs, 1988, 20: A324.
    [15]
    LISTER G S, DAVIS G A. The Origin of metamorphic core complexes and detachment fault formed during Tertiary continental extension in the Northern Colorado River region, U.S. A[J]. Journal of Structural Geology, 1988, 11(1-2): 65-94.
    [16]
    郑亚东, 张青. 内蒙古亚干变质核杂岩核内递进伸展作用[M]//钱祥麟. 伸展构造研究. 北京: 地质出版社, 1994: 4-11.

    ZHENG Yadong, ZHANG Qing. Progressive extension within the core of metamorphic core complex from the Yagan area, inner Mongolia[M]//QIAN Xianglin. Extensional tectonics research. Beijing: Geological Publishing House, 1994: 4-11.
    [17]
    宋鸿林. 秦岭—大别造山带早期的伸展构造[M]//钱祥麟. 伸展构造研究. 北京: 地质出版社, 1994: 12-21.

    SONG Honglin. Earlier extensional tectonics along Qinling-Dabie orogenic belt[M]//QIAN Xianglin. Extensional tectonics research. Beijing: Geological Publishing House, 1994: 12-21.
    [18]
    王小凤, 李中坚, 陈柏林, 等. 郯庐断裂带[M]. 北京: 地质出版社, 2000: 1-374.

    WANG Xiaofeng, LI Zhongjian, CHEN Bailin, et al. The Tan-Lu Fault Zone[M]. Beijing: Geological Publishing House, 2000: 1-374.
    [19]
    丁道桂, 罗开平, 刘光祥. 下扬子区伸展拆离构造[J]. 石油实验地质, 2016, 38(1): 1-8. doi: 10.11781/sysydz201601001

    DING Daogui, LUO Kaiping, LIU Guangxiang, et al. Extensional detachment structures in the Lower Yangtze region[J]. Petroleum Geology & Experiment, 2016, 38(1): 1-8. doi: 10.11781/sysydz201601001
    [20]
    朱光, 谢成龙, 向必伟. 洪镇变质核杂岩的形成机制及其大地构造意义[J]. 中国科学(D辑: 地球科学), 2007, 37(5): 584-592. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200705001.htm

    ZHU Guang, XIE Chenglong, XIANG Biwei. Genesis of the Hongzhen metamorphic core complex and its tectonic implications[J]. Science in China(Series D: Earth Sciences), 2007, 50(5): 649-659. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200705001.htm
    [21]
    王金渝, 周荔青, 郭念发. 苏浙皖石油天然气地质[M]. 北京石油工业出版社, 2000: 53-54.

    WANG Jinyu, ZHOU Liqing, GUO Nianfa. Geology of petroleum and natural gas among Jiangsu, Zhejiang and Anhui provinces[M]. Beijing: Petroleum Industry Press, 2000: 53-54.
    [22]
    闵庆魁. 宁镇山脉发现前震旦系——埤城群[J]. 地层学杂志, 1987(2): 130-134, 162. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ198702006.htm

    MIN Qingkui. Picheng groups were discovered in Ningzhen Mountains from the Pre-Sinian system[J]. Journal of Stratigraphy, 1987(2): 130-134, 162. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ198702006.htm
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