Liu Zhiwu, Bai Yong, Zhou Lifa. Basin structure and hydrocarbon accumulation conditions of the Weihe Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(5): 584-591. doi: 10.11781/sysydz201605584
Citation: Liu Zhiwu, Bai Yong, Zhou Lifa. Basin structure and hydrocarbon accumulation conditions of the Weihe Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(5): 584-591. doi: 10.11781/sysydz201605584

Basin structure and hydrocarbon accumulation conditions of the Weihe Basin

doi: 10.11781/sysydz201605584
  • Received Date: 2015-10-04
  • Rev Recd Date: 2016-08-25
  • Publish Date: 2016-09-28
  • The Weihe Basin, which is located in the southern margin of the Ordos massif, is a Cenozoic fault basin. Understanding the basement structure and tectonic characteristics of this basin are pivotal to guide hydrocarbon exploration and resource potential evaluation. In this paper, the basement and tectonic style of the Weihe Basin is studied using regional structural analysis, with comprehensively field geology, drilling, test and geophysical data such as gravity, aeromagnetic, seismic etc. In turn, the hydrocarbon accumulation conditions of this basin are also discussed. The research results show that the pre-Cenozoic basement of the Weihe Basin is mainly composed of four different physical partitions. The tectonic style of the Lower Paleozoic basement is mainly strong fold deformation, which is separated by Cenozoic normal faults. The Cenozoic tectonic style of this basin is a half graben, which is controlled by normal faults. Both the pre-Cenozoic and the Cenozoic of the Weihe Basin have good natural gas reservoir forming conditions.

     

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  • [1]
    彭建兵,张骏,苏生瑞,等.渭河盆地活动断裂与地质灾害[M].西安:西北大学出版社,1992:65-80. Peng Jianbing,Zhang Jun,Su Shengrui,et al.Active faults and geological hazards in Weihe Basin[M].Xi'an:Northwest University Press,1992:65-80.
    [2]
    韩恒悦,张逸,袁志祥.渭河断陷盆地带的形成演化及断块运动[J].地震研究,2002,25(4):362-368. Han Hengyue,Zhang Yi,Yuan Zhixiang.The evolution of Weihe down-faulted basin and the movement of the fault blocks[J].Journal of Seismological Research,2002,25(4):362-368.
    [3]
    冯希杰,戴王强.渭河盆地断层活动的横向迁移[J].地震学报,2004,26(2):174-182. Feng Xijie,Dai Wangqiang.Lateral migration of fault activity in Weihe Basin[J].Acta Seismologica Sinica,2004,26(2):174-182.
    [4]
    刘护军,薛祥煦.对渭河盆地新生界及其年代的讨论[J].地球科学与环境学报,2004,26(4):1-5. Liu Hujun,Xue Xiangxu.Discussion on the Cenozoic and its chronology in the Weihe River Basin[J].Journal of Earth Sciences and Environment,2004,26(4):1-5.
    [5]
    权新昌.渭河盆地断裂构造研究[J].中国煤田地质,2005,17(3):1-4. Quan Xinchang.Weihe basin faulted structure study[J].Coal Geology of China,2005,17(3):1-4.
    [6]
    刘志武,周立发.渭河盆地新生代构造—沉积格局与油气成藏潜力初探[J].福州大学学报(自然科学版),2015,43(5):708-714. Liu Zhiwu,Zhou Lifa.The Cenozoic tectonic and sedimentary framework and preliminary study on the hydrocarbon accumulation potential of the Weihe Basin[J].Journal of Fuzhou University (Natural Science Edition),2015,43(5):708-714.
    [7]
    赵西蓉.渭河断陷盆地地热资源赋存特征与热储分析[J].煤田地质与勘探,2006,34(2):51-54. Zhao Xirong.Occurrence features of geothermal resources and geothermal bearing analysis in Weihe Basin[J].Coal Geology & Exploration,2006,34(2):51-54.
    [8]
    刘建朝,李荣西,魏刚峰,等.渭河盆地地热水水溶氦气成因与来源研究[J].地质科技情报,2009,28(6):84-88. Liu Jianchao,Li Rongxi,Wei Gangfeng,et al.Origin and source of soluble helium gas in geothermal water,Weihe Basin[J].Geological Science and Technology Information,2009,28(6):84-88.
    [9]
    李玉宏,卢进才,李金超,等.渭河盆地富氦天然气井分布特征与氦气成因[J].吉林大学学报(地球科学版),2011,41(S1):47-53. Li Yuhong,Lu Jincai,Li Jinchao,et al.Distribution of the helium-rich wells and helium derivation in Weihe Basin[J].Journal of Jilin University (Earth Science Edition),2011,41(S1):47-53.
    [10]
    张福礼,孙启邦,王行运,等.渭河盆地水溶氦气资源评价[J].地质力学学报,2012,18(2):195-202. Zhang Fuli,Sun Qibang,Wang Xingyun,et al.Evaluation of water soluble helium resources in Weihe Basin[J].Journal of Geomechanics,2012,18(2):195-202.
    [11]
    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. Zhang Guowei,Zhang Benren,Yuan Xuecheng,et al.Qinling orogenic belt and continental dynamics[M].Beijing:Science Press,2001.
    [12]
    陆永德.东秦岭洛南—栾川断裂带的形成和演化[J].石油实验地质,2009,31(2):148-153. Lu Yongde.Formation and evolution of the Luonan-Luanchuan fault belt in the east Qinling region[J].Petroleum Geology & Experiment,2009,31(2):148-153.
    [13]
    张国伟,孟庆任,刘少峰,等.华北地块南部巨型陆内俯冲带与秦岭造山带岩石圈现今三维结构[J].高校地质学报,1997,3(2):129-143. Zhang Guowei,Meng Qingren,Liu Shaofeng,et al.Huge intracontinental subduction zone at south margin of north china block and present 3-D lithospheric framework of the Qinling orogenic belt[J].Geological Journal of China Universities,1997,3(2):129-143.
    [14]
    Wang Jingming.The Fenwei rift and its recent periodic activity[J].Tectonophysics,1987,133(3/4):257-275.
    [15]
    林 舸,王岳军,李自安.盆地基本构造样式与天然气成藏[J].大地构造与成矿学,1999,23(3):197-204. Lin Ge,Wang Yuejun,Li Zi'an.The structural patterns and gas reserviors-forming in sedimentary basins[J].Geotectonica et Metallogenia,1999,23(3):197-204.
    [16]
    陈刚,周鼎武.陕西淳化口镇—圣人桥地区地层变形特征及其地质意义[J].西北大学学报(自然科学版),1994,24(2):163-166. Chen Gang,Zhou Dingwu.Geological significance and characteristics of the covering strata deformation in Kouzhen-Shengrenqiao,Chunhua county,Shaanxi province[J].Journal of Northwest University (Natural Science Edition),1994,24(2):163-166.
    [17]
    刘宝宪,闫小雄,白海峰,等.鄂尔多斯盆地南缘中奥陶统平凉组成藏条件分析[J].天然气地球科学,2008,19(5):657-661. Liu Baoxian,Yan Xiaoxiong,Bai Haifeng,et al. Reservoir-forming conditions of Middle Ordovician Pingliang Formation, southern margin of Ordos Basin[J].Natural Gas Geoscience,2008,19(5):657-661.
    [18]
    池卫国.鄂尔多斯南缘逆冲推覆带古生界天然气藏的保存条件[J].断块油气田,1998,6(3):5-7. Chi Weiguo.Preservation conditions for Palaeozoic gas reservoir of upthrust nappe zone in southern Eerduosi Basin[J].Fault-Block Oil & Gas Field,1998,6(3):5-7.
    [19]
    左智峰,李荣西.鄂尔多斯盆地南缘古坳陷奥陶系烃源岩与天然气勘探潜力研究[J].中国地质,2008,35(2):279-285. Zuo Zhifeng,Li Rongxi.Ordovician source rocks and natural gas potential in the southern Ordos Basin marginal paleo-depression[J].Geology in China,2008,35(2):279-285.
    [20]
    夏明军,戴金星,邹才能,等.鄂尔多斯盆地南部加里东期岩溶古地貌与天然气成藏条件分析[J].石油勘探与开发,2007,34(3):291-298. Xia Mingjun,Dai Jinxing,Zou Caineng,et al.Caledonian karst palaeogeomorphology and the forming condition of gas pool,southern Ordos Basin[J].Petroleum Exploration and Development,2007,34(3):291-298.
    [21]
    李江涛.鄂尔多斯盆地南缘构造特征及下古生界天然气勘探前景[J].石油勘探与开发,1996,23(2):11-15. Li Jiangtao.Structural characteristics and natural gas potential of Lower Paleozoic in the south margin of Ordos Basin[J].Petro-leum Exploration and Development,1996,23(2):11-15.
    [22]
    陈孟晋,汪泽成,郭彦如,等.鄂尔多斯盆地南部晚古生代沉积特征与天然气勘探潜力[J].石油勘探与开发,2006,33(1):1-5. Chen Mengjin,Wang Zecheng,Guo Yanru,et al.Late Paleozoic se-dimentary systems and gas potential in the south Ordos Basin[J].Petroleum Exploration and Development,2006,33(1):1-5.
    [23]
    张祥,纪宗兰,杨银山,等.关于生物气源岩评价标准的讨论:以柴达木盆地第四系生物气为例[J].天然气地球科学,2004,15(5):465-470. Zhang Xiang,Ji Zonglan,Yang Yinshan,et al.Discussion of evaluation criterion for the source rock of biological gas:Taking quaternary biological gas in Qaidam Basin as the example[J].Natural Gas Geoscience,2004,15(5):465-470.
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