DU Min, WANG Houjin, WANG Gaiyun, JIAN Xiaoling, WAN Xiaoming. CHARACTERISTICS AND FORMATION MECHANISM OF MESO-CENOZOIC SUPERIMPOSED BASINS IN THE EAST DEPRESSION OF THE NORTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2016, 36(5): 85-96. DOI: 10.16562/j.cnki.0256-1492.2016.05.009
Citation: DU Min, WANG Houjin, WANG Gaiyun, JIAN Xiaoling, WAN Xiaoming. CHARACTERISTICS AND FORMATION MECHANISM OF MESO-CENOZOIC SUPERIMPOSED BASINS IN THE EAST DEPRESSION OF THE NORTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2016, 36(5): 85-96. DOI: 10.16562/j.cnki.0256-1492.2016.05.009
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CHARACTERISTICS AND FORMATION MECHANISM OF MESO-CENOZOIC SUPERIMPOSED BASINS IN THE EAST DEPRESSION OF THE NORTH YELLOW SEA BASIN

  • MLR Key Laboratory of Marine Mineral Resources, Guangzhou Marine Geological Survey, Guangzhou 510075, Guangdong, China

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  • Received Date: November 18, 2015
  • Revised Date: January 04, 2016
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    • Abstract
  • Based on the latest geological-geophysical data, the faults characteristics and structural styles of the Eastern Depression of the Northern Yellow Sea Basin are studied, and the sedimentary-tectonic evolutionary stages summarized. The results show that faults in the Eastern Depression are well developed. The faults of F1 and F2 are the most important controlling ones, then followed by F9、F10、F11 and F8. The structural deformation, which is rather complex, includes the extensional, compressed, wrenching and inversed deformation. Seven sedimentary-tectonic evolutionary stages are recognized, namely the initial faulting and depressing stage(J2), the expanding stage of faults and depression (J3), the faulting and sag formation stage(K1), the tectonic inversion stage (late K1-E2), the intensive faulting and depression stage(E3), and the regional subsidence stage(N1-Q). The formation mechanism of the Eastern Depression is also discussed with reference to the regional geological background. In Middle Jurassic, the extension caused by block escape brought about the initial faulting and depression. In Late Jurassic, faulting and depressing continued and the crust became thinning due to plate subduction. In the Early Cretaceous, the Tanlu fault experienced a sinistral slip movement as the result of the change in motion of the Izanagi plate, and the faulting sag was formed in the stress field of sinistral rotation together with thermal subsidence. In Late Cretaceous, face to face subduction of plates led to compression inversion which had lasted up to the Eocene in Eastern Depression. In Oligocene, due to the re-orientation of the Pacific plate movement, the retreatment of the subduction zone and the collision of Indian and Eurasian plates, the Tanlu fault became dextral. Strong faulting and depressing of the study area has made the region a dextral transtensional tectonic setting. At the end of Oligocene, due to the increment in the subduction rate of the Pacific plate, the strengthening of Indian-Eurasian collision, and the slowing down of subduction, the inversion structures dominated again in the study area. Regional subsidence appeared again in the Eastern depression during the Miocene to Quaternary, due to thermal attenuation of lithosphere.
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    • References (26)
  • [1] 赖万忠. 中国海域中生界油气勘探[J]. 中国海上油气(地质), 2001, 15(5):311-316.[LAI Wanzhong. Mesozoic petroleum exploration in offshore china[J]. China Offshore Oil And Gas (Geology), 2001, 15(5):311-316.]
    [2]
    王强,王应斌,张友,等. 北黄海东部坳陷中生界储层特征[J].沉积与特提斯地质,2010, 30(4):97-103.

    [WANG Qiang, WANG Yingbin, ZHANG You, et al. Characteristics of the Mesozoic reservoirs in the eastern depression of the Northern Yellow Sea Basin[J]. Sedimentary Geology and Tethyan Geology, 2010, 30(4):97-103.]
    [3]
    Chough S K, Kwon S T, Ree J H, et al. Tectonic and sedimentary evolution of the Korean peninsula:a review and new view[J]. Earth-Science Reviews, 2000, 52:175-235.
    [4]
    Young Jae Shinn, Chough S K, In Gul Hwang. Structural development and tectonic evolution of Gunsan Basin (Cretaceous-Tertiary) in the central Yellow Sea[J]. Marine and Petroleum Geology, 2010, 27:500-514.
    [5]
    李文勇,李东旭,夏斌,等. 北黄海盆地构造演化特征分析[J]. 现代地质,2006, 20(2):268-276.

    [LI Wenyong, LI Dongxu, XIA Bin, et al. Characteristics of structural evolution in North Yellow Sea Basin[J]. Geoscience, 2006, 20(2):268-276.]
    [6]
    李文勇. 北黄海盆地构造变形及动力学演化过程[J]. 地质学报,2007,81(5):588-598.

    [LI Wenyong. Tectonic deformation mechanism and geodynamic process of North Yellow Sea Basin[J].Acta Geologica Sinica, 2007, 81(5):588-598.]
    [7]
    李文勇,曾祥辉,王信国,等. 北黄海盆地构造运动学解析[J]. 地学前缘,2009,16(4):74-86.

    [LI Wenyong, ZENG Xianghui, WANG Xinguo, et al. Analysis of structural kinematics of North Yellow Sea Basin[J]. Earth Science Frontiers, 2009, 16(4):74-86.]
    [8]
    王后金,梁世荣,陈强. 北黄海盆地褶皱分布与成因类型[J]. 海洋地质与第四纪地质,2006,26(6):65-70.

    [WANG Houjin, LIANG Shirong, CHEN Qiang. Distribution and origin types of the folds in the North Yellow Sea Basin[J]. Marine Geology and Quaternary Geology, 2006,26(6):65-70.]
    [9]
    王后金,王嘹亮,冯常茂. 北黄海盆地的成盆动力学机制探讨[J]. 石油天然气学报,2014,36(5):1-7.

    [WANG Houjin, WANG Liaoliang, FENG Changmao. Kinetics mechanism of the North Yellow Sea Basin[J]. Journal of Oil and Gas Technology,2014,36(5):1-7.]
    [10]
    陈亮,刘振湖,金庆焕,等. 北黄海盆地东部坳陷中新生代构造演化[J]. 大地构造与成矿学,2008, 32(3):308-316.

    [CHEN Liang, LIU Zhenhu, JIN Qinhuan, et al. Meso-Cenozoic tectonic evolution of the east depression of North Yellow Sea[J]. Geotectonica et Metallogenia, 2008, 32(3):308-316.]
    [11]
    刘振湖,高红芳,胡小强,等. 北黄海盆地东部拗陷中生界含油气系统研究[J].中国海上油气地质,2007, 19(4):229-233.

    [LIU Zhenhu, GAO Hongfang, HU Xiaoqiang, et al. A study on the Mesozoic petroleum system in East depression, North Yellow Sea basin[J]. China Offshore Oil and Gas, 2007, 19(4):229-233.]
    [12]
    Zhao G C, Sun M, Wilde S A, et al. Late Archean to Paleoproterozoic evolution of the North China Craton:Key issues revisited[J]. Precambrian Research, 2005, 136:177-202.
    [13]
    Yang J H, Wu F Y, Wilde S A, et al. Mesozoic decratonization of the North China block[J]. Geology, 2008, 36:467-470.
    [14]
    李三忠,刘鑫,索艳慧,等.华北克拉通东部地块和大别山-苏鲁造山带印支期褶皱:逆冲构造与动力学背景[J]. 岩石学报,2009,25(9):2031-2049.

    [LI SanZhong, LIU Xin, SUO YanHui, et al. Triassic folding and thrusting in the Eastern Block of the North China Craton and the Dabie-Sulu orogen and its geodynamics[J].Acta Petrologica Sinica,2009,25(9):2031-2049.]
    [15]
    刘建忠,李三忠,周立宏,等. 华北板块东部中生代构造变形与盆地格局[J]. 海洋地质与第四纪地质,2004,24(4):45-54.

    [LIU Jianzhong, LI Sanzhong, ZHOU Lihong, et al. Mesozoic tectonics and basin distribution in the Eastern North China Plate[J].Marine Geology and Quaternary Geology, 2004, 24(4):45-54.]
    [16]
    李三忠,余珊,赵淑娟,等. 东亚大陆边缘的板块重建与构造转换[J]. 海洋地质与第四纪地质,2013,33(3):65-94.

    [LI Shanzhong, YU Shan, ZHAO Shujuan, et al. Tectonic transition and plate reconstructions of the East Asia continental magin[J].Marine Geology and Quaternary Geology, 2013, 33(3):65-94.]
    [17]
    杜民,王改云,刘金萍,等. 北黄海盆地东部坳陷地层划分及沉积特征[J]. 特种油气藏,2014, 21(2):51-56.

    [DU Min, WANG Gaiyun, LIU Jinping, et al. Stratigraphy and sedimentary characters of the eastern depression in North Yellow Sea Basin[J]. Special Oil and Gas Reservoirs, 2014, 21(2):51-56.]
    [18]
    刘金萍,王改云,杜民,等. 北黄海盆地东部坳陷中生界烃源岩特征[J]. 中国海上油气,2013, 25(4):12-16.

    [LIU Jinping, WANG Gaiyun, DU Min, et al. Analyzing characteristics of Mesozoic hydrocarbon source rocks in the Eastern depression, North Yellow Sea basin[J]. China Offshore Oil and Gas, 2013, 25(4):12-16.]
    [19]
    王改云,刘金萍,王后金,等. 北黄海盆地东部坳陷中生界沉积特征及演化[J]. 沉积学报,2015, 33(3):561-567.

    [WANG Gaiyun, LIU Jinping, WANG Houjin, et al. Sedimentary characteristics and evolution of Mesozoic in the Eastern Depression, North Yellow Sea Basin[J]. Acta Sedimentologica Sinica, 2015, 33(3):561-567.]
    [20]
    侯旭波,催红庄,郇玉龙. 银川盆地不同构造层构造样式及形成演化分析[J]. 东北石油大学学报,2012, 36(6):28-33.

    [HOU Xubo, CUI Hongzhuang,XUN Yulong. Analysis of structural style and tectonic evolution in Yinchuan Basin[J]. Journal of North Petroleum University, 2012, 36(6):28-33.]
    [21]
    陆克政. 含油气盆地分析[M]. 石油大学出版社, 2001:67-70.[LU Kezheng. Petroleum Basin Analysis[M]. Petroluem University Press, 2001:67

    -70.]
    [22]
    廖远涛. 胶莱盆地的盆地样式及构造演化[J].新疆石油地质, 2002, 23(4):345-347.

    [LIAO Yuantao. The pattern and tectonic evolution of Jiaolai Basin[J]. Xinjiang Petroleum Geology, 2002, 23(4):345-347.]
    [23]
    朱丽旭,吕延防,吴宇,等. 海塔盆地中部断陷带反转构造特征及其对油气的控制[J]. 东北石油大学学报,2013, 37(2):46-54.

    [ZHU Lixu, LU Yanfang,WU Yu, et al. Feature of inversion tectonics and reservoir controlling significance of middle zone of Haita basin[J]. Journal of North Petroleum University, 2013, 37(2):46-54.]
    [24]
    张功成,金利. 论反转构造[J]. 海洋地质与第四纪地质,1997,17(4):83-90.

    [ZHANG Gongcheng, JIN Li. On inversion tectonics and structures[J]. Marine Geology and Quaternary Geology, 1997, 17(4):83-90.]
    [25]
    邵济安,牟保磊,何国琦,等.华北北部在古亚洲域与古太平洋域构造叠加过程中的地质作用[J].中国科学D辑,1997,27(5):390-394.

    [SHAO Ji'an, MU Baolei, HE Guoqi, et al. Geological processes of the process of structural overlapping between paleo-asia domain and paleo-pacific domain in northern part of North China[J]. Science in China:Series D, 1997,27(5):390-394.]
    [26]
    徐嘉炜,朱光. 中国东部郯庐断裂带构造模式讨论[J]. 华北地质矿产杂志,1995,10(2):121-134.

    [XU Jiawei, ZHU Guang. Discussion on tectonic model for the Tan-Lu fault zone, Eastern China[J]. Jour Geol & Min Res North China, 1995, 10(2):121-134.]
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