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塔北隆起哈拉哈塘-哈得地区中生界次生油气藏形成条件分析

石放 王铸坤 李建浪 孙琦 易珍丽 李斌 刘柳 尹太举

王翠丽, 李红波, 陈 东, 陈宝新, 刘 磊, 罗明高. 克深气田巴什基奇克组致密砂岩储层孔隙结构特征及影响因素分析[J]. 地质科技通报, 2018, 37(5): 70-77.
引用本文: 石放, 王铸坤, 李建浪, 孙琦, 易珍丽, 李斌, 刘柳, 尹太举. 塔北隆起哈拉哈塘-哈得地区中生界次生油气藏形成条件分析[J]. 地质科技通报, 2024, 43(4): 15-26. doi: 10.19509/j.cnki.dzkq.tb20230449
Wang Cuili, Li Hongbo, Chen Baoxin, Luo Minggao. Porosity Structure Characteristics and Influencing Factors Analysis of Basijiqike Tight Sandstone Reservoir in Keshen Gasfield[J]. Bulletin of Geological Science and Technology, 2018, 37(5): 70-77.
Citation: SHI Fang, WANG Zhukun, LI Jianlang, SUN Qi, YI Zhenli, LI Bin, LIU Liu, YIN Taiju. Analysis of the formation conditions of Mesozoic secondary oil and gas reservoirs in Halahatang-Hade area of the Tabei Uplift[J]. Bulletin of Geological Science and Technology, 2024, 43(4): 15-26. doi: 10.19509/j.cnki.dzkq.tb20230449

塔北隆起哈拉哈塘-哈得地区中生界次生油气藏形成条件分析

doi: 10.19509/j.cnki.dzkq.tb20230449
基金项目: 

国家自然科学基金项目 42072119

中国石油天然气股份有限公司塔里木油田分公司科技项目 041021120183

详细信息
    作者简介:

    石放, E-mail: sfang-tlm@petrochina.com.cn

    通讯作者:

    尹太举,E-mail:yintaij@yangtzeu.edu.cn

  • 中图分类号: P534.5;P618.130.2

Analysis of the formation conditions of Mesozoic secondary oil and gas reservoirs in Halahatang-Hade area of the Tabei Uplift

More Information
  • 摘要:

    塔里木盆地塔北隆起带哈拉哈塘-哈得地区中生界面积超3万km2, 处于大型单斜背景, 油气显示活跃, 具有较大的勘探潜力, 但多年来未有勘探突破。邻区中石化矿区的发现使得该区的勘探再次提上了日程。基于新处理的三维地震资料, 在分析区域地质概况的基础上, 系统分析了油源条件、走滑断裂的构造及演化特征和岩性圈闭的形成及封堵条件, 明确了该区的成藏模式及有利勘探方向。研究区中生界发育河流-三角洲沉积体系, 其中三叠系发育NE-SW向条带状三角洲砂体, 侏罗系和白垩系下部发育SE-NW向展布的叠覆浅水三角洲砂体, 白垩系上部发育大面积连片状的辫状河砂体。该区经历了3期隆升, 发育5期断层, 其中中生界的三叠系-侏罗系断层是古生界断层的伴生断层, 受古生界断层的发育控制, 雁列状NE-SW向展布。白垩系和侏罗系浅水三角洲前缘单一朵体或多个朵体披覆泥岩拼接形成了侧向遮挡, 与上倾方向断层联合形成岩性-断层圈闭, 三叠系条带状SE方向展布的三角洲砂体和大型河道弯曲部位河道外泥岩遮挡形成岩性圈闭。油气源于古生界古油藏, 通过古生界奥陶系断层泄漏后, 经中生界伴生断层直接进入中生界圈闭或经中生界断层接替输运进入圈闭而成藏。基于此, 认为本区勘探潜力区主要有北部走滑带的侏罗系-白垩系舒善河组三角洲前缘岩性油气藏、三叠系北侧的三角洲前缘砂体和南部河道砂体岩性油气藏和三叠系北部隆起区披覆小型扇体岩性油气藏。断裂组合、砂体展布及披覆泥岩遮挡3个关键控藏要素及其有效配置是塔北隆起带大型斜坡区形成有利岩性、岩性-断层复合圈闭油气藏的重要前提, 该认识为该区油气的深化勘探指明了方向, 对其他地区岩性、岩性-断层复合圈闭油气藏勘探具有借鉴意义。

     

  • 所有作者声明不存在利益冲突。
  • 图 1  塔北隆起构造单元划分及研究区位置图(据文献[12]修改)

    Figure 1.  Subdivision of tectonic units in the Tabei Uplift and location of the study area

    图 2  塔北隆起中生代地层及沉积发育综合柱状图(据文献[10,12-13,22]修改)

    Figure 2.  Comprehensive diagram of Mesozoic stratigraphy and sedimentary characteristics in the Tabei Uplift

    图 3  塔北地区不同地层中原油色谱及特征

    Figure 3.  Chromatography characteristics of crude oil in different formations in the Tabei area

    图 4  塔北地区沥青砂岩中的固体沥青的显微照片

    a.H1井,6 230 m, 透射光下的沥青(固体沥青分布在岩石颗粒之间的孔隙中);b.HD17井,5 591 m,沥青周围液态石油;c.X3井, 5 682 m,沥青周围液态石油

    Figure 4.  Micrograph of the solid bitumen in the bituminous sandstone of the Tabei area

    图 5  哈拉哈塘-哈得地区侏罗系顶面构造图(a)及典型剖面特征(b) (剖面位置见图 1)

    Figure 5.  Structural map of the Jurassic top interface (a) and typical profile characteristics (b) in the Halahatang-Hade area

    图 6  哈拉哈塘-哈得地区不同时期断层发育特征(剖面位置见图 1)

    a.地层及断层解释;b.不同时期断层

    Figure 6.  Characteristics of fault development during different periods in the Halahatang-Hade area

    图 7  哈拉哈塘-哈得地区构造演化恢复(剖面位置见图 1)

    Figure 7.  Restoration of tectonic evolution in the Halahatang-Hade area

    图 8  哈拉哈塘-哈得地区中生界(a)和古生界(b)断层平面分布及油气显示图

    Figure 8.  Distribution of fault planes and hydrocarabon display maps in the Mesozoic(a) and Paleozoic strata(b) of the Halahatang-Hade area

    图 9  哈拉哈塘-哈得地区中生界3类沉积体系砂体发育特征

    Figure 9.  Development characteristics of Mesozoic sand-bodies in three types of sedimentary systems in the Halahatang-Hade area

    图 10  哈拉哈塘-哈得地区中生界RP1402井岩性圈闭形成示意图

    a.侏罗系含油砂体伽马属性;b.侏罗系伽马属性反演剖面(剖面位置见图 10a);c.侏罗系顶界面构造图;d.侏罗系顶界面相干体切片;e.典型剖面断层解释(剖面位置见图 10d)

    Figure 10.  Illustration of the lithologic traps generation in the Mesozoic Well RP1402 of the Halahatang-Hade area

    图 11  哈拉哈塘-哈得地区中生界成藏模式图

    Figure 11.  Accumulation model of Mesozoic hydrocarbon in the Halahatang-Hade area

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出版历程
  • 收稿日期:  2023-08-02
  • 录用日期:  2023-12-25
  • 修回日期:  2023-12-22

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