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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2018  >  40(2): 177-184
DENG Mingzhe, HE Dengfa, ZHANG Yuying. Tectonic evolution of Xiannüshan fault and its influence on hydrocarbon traps in Changyang anticline, Western Hubei fold belt[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(2): 177-184. doi: 10.11781/sysydz201802177
Citation: DENG Mingzhe, HE Dengfa, ZHANG Yuying. Tectonic evolution of Xiannüshan fault and its influence on hydrocarbon traps in Changyang anticline, Western Hubei fold belt[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(2): 177-184. doi: 10.11781/sysydz201802177
shu

Tectonic evolution of Xiannüshan fault and its influence on hydrocarbon traps in Changyang anticline, Western Hubei fold belt

doi: 10.11781/sysydz201802177

  • Resource College, China University of Geosciences(Beijing), Beijing 100083, China

  • Received Date: 2017-12-04
  • Rev Recd Date: 2018-02-11
  • Publish Date: 2018-03-28
    Abstract
  • The Western Hubei fold belt is an important oil and gas exploration area in South China. Located in the northeast of the fold belt, the Xiannüshan fault intersects the Changyang anticline, and has an important influence on the hydrocarbon traps in the Changyang anticline. However, the geometrical morphology and evolution history of the Xiannüshan fault has not been well studied due to the lack of accurate depth information, and the influence on hydrocarbon trap evolution was still unclear. Based on the interpretation of the latest seismic section in the central part of the fault, the quasi-three-dimensional shape and the formation process of the Xiannüshan fault were analyzed. Combined with the regional geological evolution and hydrocarbon accumulation process, the influence of the formation and evolution of faults on the preservation units in the Changyang anticline was analyzed. (1)The Xiannüshan fault belt can be divided into three parts. The northern part is dipping westwards, while the middle and southern parts are dipping eastwards. (2)The Xiannüshan fault was first formed during the Late Jurassic as a strike slip fault, pulling apart during the Late Cretaceous, and thrusted during the Middle and Late Paleogene. (3)The strike slip of the Xiannüshan fault in the Late Jurassic was favorable for hydrocarbon migration in the Changyang anticline. However, the stretching of the Xiannüshan fault in the Late Cretaceous destroyed tectonic traps in the Changyang anticline, leading to hydrocarbon loss. In areas where similar faults have occurred in the western Hubei, the potential for oil and gas exploration may have been adversely affected.

     

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    • References(19)
  • [1]
    赵宗举,俞广,朱琰,等.中国南方大地构造演化及其对油气的控制[J].成都理工大学学报(自然科学版):2003,30(2):155-168. ZHAO Zongju,YU Guang,ZHU Yan,et al.Tectonic evolution and its control over hydrocarbon in southern China[J].Journal of Chengdu University of Technology (Science & Technology Edition),2003,30(2):155-168.
    [2]
    李玶,李愿军.长江三峡坝区地壳稳定性研究[J].中国工程科学,2004,6(6):26-34. LI Ping,LI Yuanjun.Study on the crustal stability in Three-Gorges area of the Yangtze River[J].Engineering Science,2004,6(6):26-34.
    [3]
    车用太,陈俊华,张莉芬,等.长江三峡工程库首区胡家坪MS4.1水库诱发地震研究[J].地震,2009,29(4):1-13. CHE Yongtai,CHEN Junhua,ZHANG Lifen, et al.Study of the reservoir-induced Hujiaping MS4.1 earthquake in the Three Gorges Dam area[J].Earthquake,2009,9(4):1-13.
    [4]
    毕珉烽,楚全芝,邓志辉,等.长江三峡地区仙女山断裂北端延伸问题探讨[J].地震地质,2012,34(2):294-302. BI Minfeng,CHU Quanzhi,DENG Zhihui,et al.Tectonic landform and location of the northern end of Xiannüshan fault at the Three Gorges area[J].Seismology and Geology,2012, 34(2):294-302.
    [5]
    吴树仁.长江三峡仙女山断层带微构造及变形环境探讨[J].地质科学,1994,29(3):220-227. WU Shuren.Study on the microstructures and deformational environment of Xiannüshan fault belt,east of Yangtze River Gorges[J].Chinese Journal of Geology,1994,29(3):220-227.
    [6]
    张峰,林文祝,周继颐.裂变径迹研究三峡仙女山断裂带断裂时期[J].科学通报,1998,43(23):2554-2556. ZHANG Feng,LIN Wenzhu,ZHOU Jiyi.The age of Xiannü Mountain fracture belt in Three-Gorge region:A fission track study[J].Chinese Science Bulletin,1999,44(8):744-747.
    [7]
    张峰,林文祝.磷灰石裂变径迹年龄分析三峡仙女山断裂带构造活动性[J].矿物学报,1999,19(1):98-102. ZHANG Feng,LIN Wenzhu.Discussion on activity of Xiannüshan fault belts in the Three-Gorges area in terms of fission-tracking age of apatite[J].Acta Mineralogica Sinica,1999,19(1):98-102.
    [8]
    吴树仁,吴淦国.长江三峡仙女山断层带的变形结构及其动力学分析[J].地质学报,1999,73(2):163-172. WU Shuren,WU Ganguo.Dynamic analysis of deformational structures of the Xiannüshan fault zone in the Three Gorges of the Yangtze River[J].Acta Geologica Sinica,1999,73(2):163-172.
    [9]
    吴世泽,罗飞,房艳国,等.三峡近坝库段水库诱发地震特征分析[J].工程地质学报,2013,21(6):932-937. WU Shize,LUO Fei,FANG Yanguo,et al.Characteristic analysis of reservoir induced earthquakes nearby the Three Gorges Dam[J].Journal of Engineering Geology,2013,21(6):932-937.
    [10]
    夏金梧,李长安,周继颐.三峡库首区仙女山等断裂活动性同位素测年研究[J].水文地质工程地质,2005,32(1):7-12. XIA Jingwu,LI Chang'an,ZHOU Jiyi.Isotope age determination study on activity of Xiannüshan fault etc in the primary Three Gorges reservoir area[J].Hydrogeology and Engineering Geo-logy,2005,32(1):7-12.
    [11]
    邢灿飞,张燕,施顺英,等.三峡库区的蓄水效应及对仙女山断裂活动的影响[J].大地测量与地球动力学,2006,26(3):69-72. XING Canfei,ZHANG Yan,SHI Shunying,et al.Impoundment effect of Three Gorges reservoir and influence on Xiannüshan fault zone[J].Journal of Geodesy and Geodynamics,2006,26(3):69-72.
    [12]
    王秋良,张丽芬,廖武林,等.三峡库首区断裂构造与地震活动特征[J].大地测量与地球动力学,2013,33(5):29-33. WANG Qiuliang,ZHANG Lifen,LIAO Wulin,et al.Fault tectonics and seismic activity characteristics of Three Gorges reservoir[J].Journal of Geodesy and Geodynamics,2013,33(5):29-33.
    [13]
    周明礼,秦兴力,冯选朝.对鄂西仙女山断裂带的几点认识[J].地壳形变与地震,1984,4(1):82-89. ZHOU Mingling,QIN Xingli,FENG Xuanchao.Several views on Xiannüshan fault zone[J].Crustal Deformation and Earthquake,1984,4(1):82-89.
    [14]
    吴世泽.仙女山断层分段性的初步研究[J].地壳形变与地震,1991,11(3):84-91. WU Shize.A preliminary study on the segmental characteristics of Xiannüshan fault[J].Crustal Deformation and Earthquake,1991,11(3):84-91.
    [15]
    湖北省地质矿产局.湖北省区域地质志[M].北京:地质出版社,1990. Bureau of Hubei Geology and Mineral Resources. Regional geology of Hubei Province[M].Beijing:Geological Publishing House,1990.
    [16]
    SUPPE J.Geometry and kinematics of fault-bend folding[J].American Journal of Science,1983,283:684-721.
    [17]
    桂宝玲.正断层相关褶皱理论及其在我国东部沉积盆地的应用[D].北京:中国地质大学(北京),2014. GUI Baoling.Normal fault related fold theory and its application in eastern basins in China[D].Beijing:China University of Geoscience,2014.
    [18]
    梅廉夫,刘昭茜,汤济广,等.湘鄂西-川东中生代陆内递进扩展变形:来自裂变径迹和平衡剖面的证据[J].地球科学(中国地质大学学报),2010,35(2):161-174. MEI Lianfu,LIU Zhaoqian,TANG Jiguang,et al.Mesozoic intra-continental progressive deformation in western Hunan-Hubei-eastern Sichuan provinces of China:Evidence from apatite fission track and balanced cross-section[J].Earth Science(Journal of China University of Geosciences),2010,35(2):161-174.
    [19]
    胡晓凤.湘鄂西地区油气藏类型及勘探方向[J].石油与天然气地质,2002,23(3):300-302. HU Xiaofeng.Oil & gas reservoir types in the western region of Hunan and Hubei and exploration orientation[J].Oil & Gas Geo-logy,2002,23(3):300-302.
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