Advanced Search
Volume 41 Issue 6
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2019  >  41(6): 779-790
XU Xuhui, FANG Chengming, LIU Jinlian, ZHAO Li, LU Jianlin, HUANG Zeguang. Deformation zoning model of piedmont thrust, western China, and its petroleum response[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2019, 41(6): 779-790. doi: 10.11781/sysydz201906779
Citation: XU Xuhui, FANG Chengming, LIU Jinlian, ZHAO Li, LU Jianlin, HUANG Zeguang. Deformation zoning model of piedmont thrust, western China, and its petroleum response[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2019, 41(6): 779-790. doi: 10.11781/sysydz201906779
shu

Deformation zoning model of piedmont thrust, western China, and its petroleum response

doi: 10.11781/sysydz201906779

  • 1. SINOPEC Petroleum Exploration & Production Research Institute, Beijing 100083, China;

  • 2. Wuxi Research Institute of Petroleum Geology, SINOPEC Petroleum Exploration & Production Research Institute, Jiangsu 214126, China;

  • 3. Oil & Gas Exploration Department, SINOPEC, Beijing 100000, China;

  • 4. College of Resources and Environment, Shandong Agricultural University, Tai'an, Shangdong 271018, China

  • Received Date: 2019-06-25
  • Rev Recd Date: 2019-09-20
  • Publish Date: 2019-11-28
    Abstract
  • The deformation structure and zonation model of piedmont thrust in an intra-continental composite system is an effective method of studying hydrocarbon accumulation regularity. The conjoint analysis of the characteristics of deep geological structures and sedimentary cover in the main piedmont thrust belt, western China indicate that the deformation of the intra-continental piedmont thrust belts is controlled by the different detachments and also by the geometric form and location of the compound land mass. The intra-continental composite piedmont thrust belt is essentially a deformation system formed by an orogenic wedge step sliding along different levels of soft strata from the orogenic wedge to the basin. Four zonation models divide the intra-continental piedmont thrust belt using the depth of main detachment as a key factor combined with deformation style. The models include a thick belt, a transition belt and a thin belt from the orogenic region to the basin, and a transition belt is further divided into transition Ⅰ belt and transition Ⅱ belt. Each belt has its unique characteristics with respect to deformation strata, deformation styles, fault-rupture mechanism, folding styles, fault-related fold principles and geometric theory. The deformation style of the intracontinental thrust belt clearly influences hydrocarbon accumulation regularity. The industrial oil and gas is mainly distributed in the transition zone. During accumulation, oil and gas in transition Ⅰ belt also adjusted, so the present petroleum reservoirs are mainly residual and always in the front part of the belt. Oil and gas in the transition Ⅱ belt mainly accumulated at the late stage and in the center of the belt. Therefore, the key factor for accumulation is the matching style of fault shape and seal. The transition from thick belt to thin belt in the central and western piedmont thrust belt is the key area for seismic technology development and exploration deployment.

     

    • FullText(HTML)
  • loading
    • References(50)
  • [1]
    贾承造,宋岩,魏国齐,等.中国中西部前陆盆地的地质特征及油气聚集[J].地学前缘,2005,12(3):3-13.

    JIA Chengzao,SONG Yan,WEI Guoqi,et al.Geological features and petroleum accumulation in the foreland basins in central and western China[J].Earth Science Frontiers,2005,12(3):3-13.
    [2]
    魏国齐,贾承造,李本亮.我国中西部前陆盆地的特殊性和多样性及其天然气勘探[J].高校地质学报,2005,11(4):552-557.

    WEI Guoqi,JIA Chengzao,LI Benliang.Particularity and diversity of the foreland basins in the central and western China and the natural gas exploration in the foreland basins[J].Geological Journal of China Universities,2005,11(4):552-557.
    [3]
    李本亮,贾承造,庞雄奇,等.环青藏高原盆山体系内前陆冲断构造变形的空间变化规律[J].地质学报,2007,81(9):1200-1207.

    LI Benliang,JIA Chengzao,PANG Xiongqi,et al.The spatial distribution of the foreland thrust tectonic deformation in the Circum-Tibetan Plateau Basin and range system[J].Acta Geologica Sinica,2007,81(9):1200-1207.
    [4]
    李本亮,魏国齐,贾承造.中国前陆盆地构造地质特征综述与油气勘探[J].地学前缘,2009,16(4):190-202.

    LI Benliang,WEI Guoqi,JIA Chengzao.Some key tectonics characteristics of Chinese foreland basins and their petroleum exploration[J].Earth Science Frontiers,2009,16(4):190-202.
    [5]
    贾承造,李本亮,雷永良,等.环青藏高原盆山体系构造与中国中西部天然气大气区[J].中国科学(地球科学),2013,43(10):1621-1631. JIA Chengzao,LI Benliang,LEI Yongliang,et al.The structure of circum-Tibetan plateau basin-range system and the large gas provinces[J].Science China(Earth Sciences),2013,56(11):1853-1863.
    [6]
    罗志立,刘树根,赵锡奎,等.试论C-型俯冲带及对中国中西部造山带形成的作用[C]//罗志立.龙门山造山带的崛起和四川盆地的形成与演化.成都:成都科技大学出版社,1994:288-316. LUO Zhili,LIU Shugen,ZHAO Xikui,et al.Discussion on the C-type subduction zone and its effect on the formation of orogenic belts in the central and western China[C]//LUO Zhili.The rise of the Longmenshan Orogenic Belt and the formation and evolution of the Sichuan Basin.Chengdu:Press of Chengdu University of Science and Technology,1994:288-316.
    [7]
    李德威,夏义平,徐礼贵.大陆板内盆山耦合及盆山成因:以青藏高原及周边盆地为例[J].地学前缘,2009,16(3):110-119.

    LI Dewei,XIA Yiping,XU Ligui.Coupling and formation mechanism of continental intraplate basin and orogeny:examples from the Qinghai-Tibet Plateau and adjacent basins[J].Earth Science Frontiers,2009,16(3):110-119.
    [8]
    周新源,苗继军.塔里木盆地西北缘前陆冲断带构造分段特征及勘探方向[J].大地构造与成矿学,2009,33(1):10-18.

    ZHOU Xinyuan,MIAO Jijun.The tectonic segmentation and hydrocarbon exploration of the foreland thrust belt in the northwestern Tarim Basin[J].Geotectonica et Metallogenia,2009,33(1):10-18.
    [9]
    李艳友,漆家福.库车坳陷克拉苏构造带分层收缩构造变形及其主控因素[J].地质科学,2012,47(3):607-617.

    LI Yanyou,QI Jiafu.Delamination contractional deformation and it main controlled factors of Kelasu Structural Zone in Kuqa Depression[J].Chinese Journal of Geology,2012,47(3):607-617.
    [10]
    汪新,贾承造,杨树锋.南天山库车褶皱冲断带构造几何学和运动学[J].地质科学,2002,37(3):372-384.

    WANG Xin,JIA Chengzao,YANG Shufeng.Geometry and kinematics of the Kuqa Fold-and-Thrust Belt in the southern Tianshan[J].Chinese Journal of Geology,2002,37(3):372-384.
    [11]
    汤良杰,金之钧,贾承造,等.库车前陆褶皱-冲断带前缘大型盐推覆构造[J].地质学报,2004,78(1):17-25.

    TANG Liangjie,JIN Zhijun,JIA Chengzao,et al.A large-scale salt nappe complex in the leading edge of the Kuqa Foreland Fold-Thrust Belt,Tarim Basin,Northwest China[J].Acta Geologica Sinica,2004,78(1):17-25.
    [12]
    孙晓猛,杜继宇,单玄龙,等.龙门山冲断带北段前山带构造分带性及山前带变形特征[J].吉林大学学报(地球科学版),2010,40(6):1323-1332. SUN Xiaomeng,DU Jiyu,SHAN Xuanlong,et al.Tectonic zonation of front range and deformation features of foreland in northern Longmen Mountain Thrust Zone[J].Journal of Jilin University (Earth Science Edition),2010,40(6):1323-1332.
    [13]
    金文正,汤良杰,杨克明,等.川西龙门山褶皱冲断带分带性变形特征[J].地质学报,2007,81(8):1072-1080.

    JIN Wenzheng,TANG Liangjie,YANG Keming,et al.Deformation and zonation of the Longmenshan Fold and Thrust Zone in the western Sichuan Basin[J].Acta Geologica Sinica,2007,81(8):1072-1080.
    [14]
    贾承造,何登发,雷振宇,等.前陆冲断带油气勘探[M].北京:石油工业出版社,2000. JIA Chengzao,HE Dengfa,LEI Zhenyu,et al.Exploration of thrust belt in foreland basin[M].Beijing:Petroleum Industry Press,2000.
    [15]
    金文正,汤良杰,杨克明,等.龙门山冲断带构造特征研究主要进展及存在问题探讨[J].地质论评,2008,54(1):37-46.

    JIN Wenzheng,TANG Liangjie,YANG Keming,et al.Progress and problem of study on characters of the Longmen Mountain Thrust Belt[J].Geological Review,2008,54(1):37-46.
    [16]
    卢华复,邓锡秧,胡德昭,等.四川盆地龙门山前破裂构造时空分布研究[D].南京:南京大学,1989. LU Huafu,DENG Xiyang,HU Dezhao,et al.Temporal and spatial distribution of the Longmenshan Faulted Structure in the Sichuan Basin[D].Nanjing:Nanjing University,1989.
    [17]
    李书兵,陈伟,简高明,等.龙门山前中段地震剖面的构造分析[J].西南石油学院学报,2006,28(2):20-24.

    LI Shubing,CHEN Wei,JIAN Gaoming,et al.The structure analysis of two-dimensional seismic profile to the middle section of Longmen Mountain anterior margin[J].Journal of Southwest Petroleum Institute,2006,28(2):20-24.
    [18]
    李坤,赵锡奎,王国芝,等.龙门山中段前山带构造特征及油气赋存研究[J].太原理工大学学报,2005,36(S1):23-26.

    LI Kun,ZHAO Xikui,WANG Guozhi,et al.Study on structural characteristics and hydrocarbon accumulation in piedmont of central Longmen Mountains[J].Journal of Taiyuan University of Technology,2005,36(S1):23-26.
    [19]
    刘和甫,梁慧社,蔡立国,等.川西龙门山冲断系构造样式与前陆盆地演化[J].地质学报,1994,68(2):101-118.

    LIU Hefu,LIANG Huishe,CAI Liguo,et al.Structural styles of the Longmenshan Thrust Belt and evolution of the foreland basin in western Sichuan province,China[J].Acta Geologica Sinica,1994,68(2):101-118.
    [20]
    周建文,曾庆,徐世琦,等.龙门山北段推覆构造带变形特征研究[J].天然气工业,2005,25(S1):66-71.

    ZHOU Jianwen,ZENG Qing,XU Shiqi,et al.Research on deformation characteristics of the nappe structural belt in the north section of Longmen mountains[J].Natural Gas Industry,2005,25(S1):66-71.
    [21]
    马永旺,杨尽.龙门山中段推覆构造的变形特征[J].成都理工学院学报,2001,28(3):236-240.

    MA Yongwang,YANG Jin.Tectonic deformation of the nappe tectonic in the middle Longmen mountains[J].Journal of Chengdu University of Technology,2001,28(3):236-240.
    [22]
    刘绍文,王良书,贾承造,等.中国中西部盆地区岩石圈热-流变学结构及其对前陆盆地成因演化的意义[J].地学前缘,2008,15(3):113-122.

    LIU Shaowen,WANG Liangshu,JIA Chengzao,et al.Thermo-rheological structure of continental lithosphere beneath major basins in central-western China:implications for foreland basin formation[J].Earth Science Frontiers,2008,15(3):113-122.
    [23]
    魏荣强,臧绍先.大陆岩石圈流变结构研究进展及存在问题[J].地球物理学进展,2007,22(2):359-364.

    WEI Rongqiang,ZANG Shaoxian.Progresses and problems in the study of the rheological structure of the continental lithosphere[J].Progress in Geophysics,2007,22(2):359-364.
    [24]
    汪洋,程素华.中国西部及邻区岩石圈热状态与流变学强度特征[J].地学前缘,2013,20(1):182-189.

    WANG Yang,CHENG Suhua.Thermal state and rheological strength of the lithosphere beneath western part of China and its adjacent region[J].Earth Science Frontiers,2013,20(1):182-189.
    [25]
    徐旭辉,高长林,黄泽光,等.中国盆地形成的三大活动构造历史阶段[J].石油与天然气地质,2005,26(2):155-162.

    XU Xuhui,GAO Changlin,HUANG Zeguang,et al.Three stages of tectonic movements in formation of petroliferous basins in China[J].Oil & Gas Geology,2005,26(2):155-162.
    [26]
    方成名,黄泽光.中国中西部大型盆地差异演化与碎屑岩油气响应[J].石油实验地质,2016,38(6):703-712.

    FANG Chengming,HUANG Zeguang.Differential characteristics of large-scale basin evolution and hydrocarbon response of clastic strata in central-western China[J].Petroleum Geology & Experiment,2016,38(6):703-712.
    [27]
    徐旭辉,黄泽光,高长林,等.中国大陆中新生代变格运动及第一变格期盆地[J].石油实验地质,2009,31(2):119-127.

    XU Xuhui,HUANG Zeguang,GAO Changlin,et al.Diktyogenese and basins in China continent during the Mesozoic-Cenozoic[J].Petroleum Geology & Experiment,2009,31(2):119-127.
    [28]
    孙肇才,邱蕴玉,郭正吾.板内形变与晚期次生成藏:扬子区海相油气总体形成规律[J].石油实验地质,1991,13(2):107-142.

    SUN Zhaocai,QIU Yunyu,GUO Zhengwu.On the relationship of the intraplate deformation and the secondary formation of oil/gas pools:the general regularities of the oil/gas formation in marine environment of the Yangtze area[J].Petroleum Geology & Experiment,1991,13(2):107-142.
    [29]
    贾承造.中国中西部前陆盆地与天然气勘探[C]//中国石油天然气股份公司前陆盆地冲断带勘探技术研讨会论文集.北京:石油工业出版社,2002:210-228. JIA Chengzao.Foreland basin and natural gas exploration in Midwest China[C]//Proceedings of Foreland Basin Thrust Belt Exploration Technology Seminar,CNPC.Beijing:Petroleum Industry Press,2002:210-228.
    [30]
    何登发,吕修祥,林永汉,等.前陆盆地分析[M].北京:石油工业出版社,1996:203-210. HE Dengfa,LÜ Xiuxiang,LIN Yonghan,et al.Analysis of foreland basins[M].Petroleum Industry Press,1996:203-210.
    [31]
    罗志立.试论中国型(C-型)冲断带及其油气勘探问题[J].石油与天然气地质,1984,5(4):315-324.

    LUO Zhili.A preliminary approach on C-subduction and its hydrocarbon prospecting[J].Oil & Gas Geology,1984,5(4):315-324.
    [32]
    刘和甫.沉积盆地地球动力学分类及构造样式分析[J].地球科学(中国地质大学学报),1993,18(6):699-724. LIU Hefu.Dynamic classification of sedimentary basins and their structural styles[J].Earth Science(Journal of China University of Geosciences),1993,18(6):699-724.
    [33]
    刘树根,李智武,曹俊兴,等.龙门山陆内复合造山带的四维结构构造特征[J].地质科学,2009,44(4):1151-1180.

    LIU Shugen,LI Zhiwu,CAO Junxing,et al.4-D textural and structural characteristics of Longmen Intracontinental Composite Orogenic Belt,Southwest China[J].Chinese Journal of Geology,2009,44(4):1151-1180.
    [34]
    JIA Dong,WEI Guoqi,CHEN Zhuxin,et al.Longmen Shan Fold-Thrust Belt and its relation to the western Sichuan Basin in central China:new insights from hydrocarbon exploration[J].AAPG Bulletin,2006,90(9):1425-1447.
    [35]
    李岩峰,曲国胜,刘殊,等.米仓山、南大巴山前缘构造特征及其形成机制[J].大地构造与成矿学,2008,32(3):285-292.

    LI Yanfeng,QU Guosheng,LIU Shu,et al.Structural characters and mechanism in the Micang Shan and southern Daba Shan mountains front[J].Geotectonica et Metallogenia,2008,32(3):285-292.
    [36]
    吴磊,钱俊锋,肖安成,等.扬子地块西侧米仓山基底卷入式冲断带的结构分析[J].岩石学报,2011,27(3):681-688.

    WU Lei,QIAN Junfeng,XIAO Ancheng,et al.Structural analysis of the Micang Shan Basement-Involved Thrust Belt in the western edge of the Yangtze Block[J].Acta Petrologica Sinica,2011,27(3):681-688.
    [37]
    吴世祥,马永生,金之钧,等.米仓山前陆盆地东段构造演化模式与油气聚集[J].石油勘探与开发,2006,33(1):14-16.

    WU Shixiang,MA Yongsheng,JIN Zhijun,et al.Tectonic evolution and oil and gas accumulation in the east Micangshan Foreland Basin,Sichuan[J].Petroleum Exploration and Development,2006,33(1):14-16.
    [38]
    邓宾.四川盆地中-新生代盆-山结构与油气分布[D].成都:成都理工大学,2013:1-56. DENG Bin.Meso-Cenozoic architecture of basin-mountain system in the Sichuan Basin and its gas distribution[D].Chengdu:Chengdu University of Technology,2013:1-56.
    [39]
    张国伟,张本仁,袁学诚,等.秦岭造山带与大陆动力学[M].北京:科学出版社,2001:855-860. ZHANG Guowei,ZHANG Benren,YUAN Xuecheng,et al.Qinling Orogenic Belt and continental dynamics[M].Beijing:Science Press,2001:855-860.
    [40]
    朱国胜.六盘山盆地中新生代构造特征分析及有利油气区预测[D].西安:长安大学,2015:1-78. ZHU Guosheng.Analysis of Meso-Cenozic structural characteris-tics and prediction of favorable oil and gas zone in Liupanshan Basin[D].Xi'an:Chang'an University,2015:1-78.
    [41]
    杨树锋,陈汉林,程晓敢,等.祁连山北缘冲断带的特征与空间变化规律[J].地学前缘,2007,14(5):211-221.

    YANG Shufeng,CHEN Hanlin,CHENG Xiaogan,et al.Deformation characteristics and rules of spatial change for the Northern Qilianshan Thrust Belt[J].Earth Science Frontiers,2007,14(5):211-221.
    [42]
    ZHAO Junmeng,LIU Guodong,LU Zaoxun,et al.Lithospheric structure and dynamic processes of the Tianshan Orogenic Belt and the Junggar Basin[J].Tectonophysics,2003,376(3/4):199-239.
    [43]
    漆家福,李勇,吴超,等.塔里木盆地库车坳陷收缩构造变形模型若干问题的讨论[J].中国地质,2013,40(1):106-120.

    QI Jiafu,LI Yong,WU Chao,et al.The interpretation models and discussion on the contractive structure deformation of Kuqa Depression,Tarim Basin[J].Geology in China,2013,40(1):106-120.
    [44]
    王招明.试论库车前陆冲断带构造顶蓬效应[J].天然气地球科学,2013,24(4):671-677.

    WANG Zhaoming.Discussion of ceiling effect in foreland thrust belt of Kuqa Depression[J].Natural Gas Geoscience,2013,24(4):671-677.
    [45]
    谢会文,尹宏伟,唐雁刚,等.基于面积深度法对克拉苏构造带中部盐下构造的研究[J].大地构造与成矿学,2015,39(6):1033-1040.

    XIE Huiwen,YIN Hongwei,TANG Yangang,et al.Research on subsalt structure in the central Kelasu Structure Belt based on the area-depth technique[J].Geotectonica et Metallogenia,2015,39(6):1033-1040.
    [46]
    曲国胜,李亦纲,张宁,等.塔里木西南缘(齐姆根弧)前陆构造及形成机理[J].地质论评,2004,50(6):567-576.

    QU Guosheng,LI Yigang,ZHANG Ning,et al.A study on the foreland structure of the Qimugen Arc in southwest Tarim and its genetic mechanism[J].Geological Review,2004,50(6):567-576.
    [47]
    伍秀芳,刘胜,汪新,等.帕米尔-西昆仑北麓新生代前陆褶皱冲断带构造剖面分析[J].地质科学,2004,39(2):260-271.

    WU Xiufang,LIU Sheng,WANG Xin,et al.Analysis on structural sections in the Cenozoic Pamir-Western Kunlun Foreland Fold-and-Thrust Belt[J].Chinese Journal of Geology,2004,39(2):260-271.
    [48]
    隋风贵.准噶尔盆地西北缘构造演化及其与油气成藏的关系[J].地质学报,2015,89(4):779-793.

    SUI Fenggui.Tectonic evolution and its relationship with hydrocarbon accumulation in the northwest margin of Junggar Basin[J].Acta Geologica Sinica,2015,89(4):779-793.
    [49]
    方成名,赵利.复合陆内山前冲断构造转换类型及其成因[J].石油实验地质,2019,41(6):791-799.

    FANG Chengming,ZHAO Li.Compound intracontinental piedmont thrust structure transformation and its formation mechanisms[J].Petroleum Geology & Experiment,2019,41(6):791-799
    [50]
    李书兵,许国明,宋晓波.川西龙门山前构造带彭州雷口坡组大型气田的形成条件[J].中国石油勘探,2016,21(3):74-82.

    LI Shubing,XU Guoming,SONG Xiaobo.Forming conditions of Pengzhou large gas field of Leikoupo Formation in Longmenshan Piedmont Tectonic Belt,western Sichuan Basin[J].China Petroleum Exploration,2016,21(3):74-82.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (633) PDF downloads(170) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return