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准噶尔盆地东道海子凹陷二叠系下乌尔禾组陆相页岩气形成富集条件及主控因素

王大兴 胡海燕 邹佳群 王涛 朱根根 陈笑宇 梁烁

王大兴, 胡海燕, 邹佳群, 王涛, 朱根根, 陈笑宇, 梁烁. 准噶尔盆地东道海子凹陷二叠系下乌尔禾组陆相页岩气形成富集条件及主控因素[J]. 地质科技通报, 2024, 43(4): 98-112. doi: 10.19509/j.cnki.dzkq.tb20230184
引用本文: 王大兴, 胡海燕, 邹佳群, 王涛, 朱根根, 陈笑宇, 梁烁. 准噶尔盆地东道海子凹陷二叠系下乌尔禾组陆相页岩气形成富集条件及主控因素[J]. 地质科技通报, 2024, 43(4): 98-112. doi: 10.19509/j.cnki.dzkq.tb20230184
WANG Daxing, HU Haiyan, ZOU Jiaqun, WANG Tao, ZHU Gengen, CHEN Xiaoyu, LIANG Shuo. Enrichment conditions and main controlling factors of continental shale gas in the Permian Lower Wuerhe Formation in the Dongdaohaizi Sag, Junggar Basin[J]. Bulletin of Geological Science and Technology, 2024, 43(4): 98-112. doi: 10.19509/j.cnki.dzkq.tb20230184
Citation: WANG Daxing, HU Haiyan, ZOU Jiaqun, WANG Tao, ZHU Gengen, CHEN Xiaoyu, LIANG Shuo. Enrichment conditions and main controlling factors of continental shale gas in the Permian Lower Wuerhe Formation in the Dongdaohaizi Sag, Junggar Basin[J]. Bulletin of Geological Science and Technology, 2024, 43(4): 98-112. doi: 10.19509/j.cnki.dzkq.tb20230184

准噶尔盆地东道海子凹陷二叠系下乌尔禾组陆相页岩气形成富集条件及主控因素

doi: 10.19509/j.cnki.dzkq.tb20230184
基金项目: 

中国石油化工股份有限公司重大科技资助项目“准噶尔盆地及周缘矿权战略选区及评价研究” P21086-4

详细信息
    作者简介:

    王大兴, E-mail: dax_wang@163.com

    通讯作者:

    胡海燕, E-mail: hyhucom@163.com

  • 中图分类号: P618.13

Enrichment conditions and main controlling factors of continental shale gas in the Permian Lower Wuerhe Formation in the Dongdaohaizi Sag, Junggar Basin

More Information
  • 摘要:

    为探明准噶尔盆地二叠系下乌尔禾组页岩气富集条件及主控因素, 以东道海子凹陷下乌尔禾组为研究对象, 通过野外地质观察、录井、测井、地震等资料的收集, 结合总有机碳含量测定、X衍射全岩分析、岩心观察、气体吸附(N2、CO2)等手段, 对下乌尔禾组页岩的分布特征、有机质发育特征、储层特征及含气性特征进行了研究。结果表明: (1)下乌尔禾组页岩总有机碳含量(w(TOC))较高, 平均1.58%;有机质类型以Ⅱ2型和Ⅲ型为主; 镜质体反射率Ro平均1.46%, 处于成熟阶段; 烃源岩厚度平均75 m, 烃源岩较好, 生气潜力大。盆地模拟结果表明下乌尔禾组页岩含气量较好, 平均1.89 m3/t。(2)页岩储集层粒内孔和微裂缝较为发育; 气体主要吸附于微孔和介孔; 孔隙度均值6.10%, 渗透率均值为0.27×10-3 μm2, 有利于页岩气的聚集。(3)页岩黏土矿物体积分数较高, 均值29.6%, 能提供较高的比表面积, 增加页岩的气体吸附能力; 脆性矿物体积分数均值50.9%, 压裂改造性良好。(4)页岩储层压力系数较大, 均值为1.58, 具有良好的保存条件。结合区域构造—沉积环境以及地化参数的分析表明, 东道海子凹陷下乌尔禾组页岩气成藏的主控因素包括地化参数和保存条件, 其中有机质热演化成熟度高、页岩厚度大、w(TOC)高、良好的保存条件等是影响页岩气富集的关键因素。基于上述条件, 提出东道海子凹陷页岩气勘探开发有利区位于凹陷的腹部偏东北斜坡地区。该研究成果揭示了东道海子凹陷下乌尔禾组页岩气富集条件及主控因素, 对准噶尔盆地腹部地区深层油气勘探具有借鉴意义。

     

  • 图 1  东道海子凹陷地质构造图(a)、沉积相图(b)和二叠系综合柱状图(c)

    Figure 1.  Geological structure map of the Dongdaohaizi Sag(a), sedimentary facies map(b) and composite column chart of the Permian System(c)

    图 2  东道海子凹陷下乌尔禾组连井剖面图(剖面位置见图 1a)

    Figure 2.  Well cross-section of the Lower Wuerhe Formation in the Dongdaohaizi Sag

    图 3  研究区下乌尔禾组页岩有机碳质量分数频率直方图(a)和平面展布图(b)

    Figure 3.  Frequency histogram(a) and plane distribution(b) of organic carbon content in shale of the Lower Wuerhe Formation in the study area

    图 4  研究区页岩Ro平面展布图

    Figure 4.  Ro plane distribution of shale in the study area

    图 5  东道海子凹陷下乌尔禾组烃源岩厚度展布图

    Figure 5.  Distribution map of source rock thickness of the Lower Wuerhe Formation in the Dongdaohaizi Sag

    图 6  下乌尔禾组陆相页岩与龙马溪组典型海相页岩矿物组成对比图(龙马溪组海相页岩数据来自文献[26])

    Figure 6.  Comparison of mineral composition between continental shales of the Lower Wuerhe Formation and typical marine shales of Longmaxi Formation

    图 7  下乌尔禾组页岩w(TOC)与矿物组分的关系

    Figure 7.  Relationships between the TOC content and mineral components content in the Lower Wuerhe Formation shale

    图 8  东道海子凹陷下乌尔禾组页岩扫描电镜图

    a.黄铁矿晶间孔,成6井,6 494.20 m;b.粒内孔,成6井,6 495.10 m;c.有机质孔,成6井,6 494.80 m;d.黏土矿物层间缝,成6井,6 499.10 m;e.微裂缝,成6井,6 495.95 m;f.粒间孔,成6井,6 497.60 m

    Figure 8.  Scanning electron microscope image of the Lower Wuerhe Formation shale in the Dongdaohaizi Sag

    图 9  下乌尔禾组页岩成6井全孔径分布图

    Figure 9.  Pore size distribution of shale in Well C6 in the Lower Wuerhe Formation

    图 10  下乌尔禾组页岩孔隙度频率分布直方图

    Figure 10.  Histogram of frequency distribution of shale porosity in the Lower Wuerhe Formation

    图 11  东道海子凹陷下乌尔禾组页岩孔隙度与石英体积分数以及渗透率与孔隙度的关系图(图b部分数据源于文献[19])

    Figure 11.  Relationship between porosity and quartz content, permeability and porosity of shale in the Lower Wuerhe Formation in Dongdaohaizi Sag

    图 12  东道海子凹陷压力系数与埋深、日产气量与压力系数关系图(部分数据来源于文献[3, 33])

    Figure 12.  Relationship between buried depth, total output and pressure coefficient in the Dongdaohaizi Sag

    图 13  研究区下乌尔禾组页岩热模拟气体产率图(a)和盆地模拟含气量变化图(b)

    Figure 13.  Thermal gas yield map(a) and gas content change map(b) of the Lower Wuerhe Formation shale in the study area

    图 14  典型盆地陆相页岩井与产气量的关系(部分数据来源于文献[3, 46])

    Figure 14.  Relationships between the continental shale wells and gas production in typical basins

    图 15  模拟含气量与w(TOC)关系图

    Figure 15.  Relationships between the gas content and TOC content

    图 16  东道海子凹陷下乌尔禾组页岩气富集区预测图

    Figure 16.  Prediction of shale gas enrichment area of the Lower Wuerhe Formation in the Dongdaohaizi Sag

    表  1  准噶尔盆地下乌尔禾组陆相页岩气组分与四川盆地龙马溪组典型海相页岩气组分分析对比

    Table  1.   Comparison of shale gas components between continental shale of the Lower Wuerhe Formation in Junggar Basin and typical marine shale of the Longmaxi Formation in Sichuan Basin

    盆地名称 井号 层位 气体组成/%
    CH4 C2H6 C3H8 CO2 N2
    四川盆地 W201井 龙马溪组 98.54 0.52 0.03 0.30 0.56
    W203井 龙马溪组 97.93 0.54 0.04 0.92 0.54
    准噶尔盆地 成6井 下乌尔禾组 96.43 0.34 0.02 1.60 1.58
    注:四川盆地龙马溪组海相页岩气组分资料来自于参考文献[26]
    下载: 导出CSV

    表  2  东道海子凹陷及邻区勘探井试气成果

    Table  2.   Gas test results of exploration wells in the Dongdaohaizi Sag and its adjacent areas

    地区 井号 层位 井深/m 日产气量/104 m3
    东道海子凹陷 成6井 P2w 6 400 3.429
    滴南8井 P2p 3 956~3 972 0.261
    克拉美丽气田 滴西5井 P2w 3 568~3 590 2.380
    滴西17井 P2w 3 519 2.255
    下载: 导出CSV
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  • 收稿日期:  2023-04-10
  • 录用日期:  2023-07-26
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