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    鄂尔多斯盆地西部志丹-吴起地区延长组裂缝特征及其控藏作用

    尹帅 丁文龙 林利飞 刘翰林 李爱荣

    尹帅, 丁文龙, 林利飞, 刘翰林, 李爱荣, 2023. 鄂尔多斯盆地西部志丹-吴起地区延长组裂缝特征及其控藏作用. 地球科学, 48(7): 2614-2629. doi: 10.3799/dqkx.2022.217
    引用本文: 尹帅, 丁文龙, 林利飞, 刘翰林, 李爱荣, 2023. 鄂尔多斯盆地西部志丹-吴起地区延长组裂缝特征及其控藏作用. 地球科学, 48(7): 2614-2629. doi: 10.3799/dqkx.2022.217
    Yin Shuai, Ding Wenlong, Lin Lifei, Liu Hanlin, Li Airong, 2023. Characteristics and Controlling Effect on Hydrocarbon Accumulation of Fractures in Yanchang Formation in Zhidan-Wuqi Area, Western Ordos Basin. Earth Science, 48(7): 2614-2629. doi: 10.3799/dqkx.2022.217
    Citation: Yin Shuai, Ding Wenlong, Lin Lifei, Liu Hanlin, Li Airong, 2023. Characteristics and Controlling Effect on Hydrocarbon Accumulation of Fractures in Yanchang Formation in Zhidan-Wuqi Area, Western Ordos Basin. Earth Science, 48(7): 2614-2629. doi: 10.3799/dqkx.2022.217

    鄂尔多斯盆地西部志丹-吴起地区延长组裂缝特征及其控藏作用

    doi: 10.3799/dqkx.2022.217
    基金项目: 

    延长油田开发部项目 ycsy2018ky-B-04

    国家自然科学基金面上项目 42072173

    详细信息
      作者简介:

      尹帅(1989-),男,博士,讲师,硕士生导师,从事非常规油气地质理论及应用技术研究.ORCID:0000-0002-8207-7751.E-mail:speedysys@163.com

      通讯作者:

      丁文龙, E-mail: dingwenlong2006@126.com

    • 中图分类号: P618.13

    Characteristics and Controlling Effect on Hydrocarbon Accumulation of Fractures in Yanchang Formation in Zhidan-Wuqi Area, Western Ordos Basin

    • 摘要: 鄂尔多斯盆地西部延长组发育大量裂缝,裂缝的存在对致密油甜点具有良好的指示作用.以鄂尔多斯盆地西部志丹-吴起地区延长组致密油储层为例,利用大量岩心、薄片、古地磁、测井、产能数据及数值模拟方法,系统研究了致密油储层裂缝发育特征及其控藏模式.结果表明,延长组主要发育垂直裂缝,根据裂缝砂岩厚度制定了裂缝发育程度分类标准;同时,结合裂缝与砂体、构造、油藏的耦合关系及油藏生产现状,系统总结了裂缝对油藏的控制作用.裂缝为延长组致密油藏运聚中良好的疏导体系;河道交汇或转向区域水流能量相对增强,砂岩分选好、脆性大,裂缝发育且利于成藏;低幅构造高点及鼻状隆起区裂缝发育且利于成藏;裂缝带与砂体走向关系耦合形成“平行砂体疏导”裂缝甜点区;裂缝主要发育于中小厚度细砂岩中,累积砂体厚度主要分布在5~15 m范围内;从砂体部位来看,裂缝主要发育于主河道翼部,其与翼部砂体粒度、颗粒可压实空间及厚度变小有关.

       

    • 图  1  研究区位置及地层综合柱状图

      Fig.  1.  Location and comprehensive histogram of the study area

      图  2  研究区延长组露头及岩心裂缝发育特征

      a.安沟延长组油苗,垂直裂缝,裂缝面上有大量油迹,坐标N36.51°、E110.22°;b.Y699井,1 833.6 m,高角度裂缝,长6;c.J41井,1 705.6 m,垂直裂缝,长6;d.T338井,615.2 m,垂直裂缝,长6;e. 4548-3井成像测井裂缝,长8

      Fig.  2.  Development characteristics of outcrops and core fractures of Yanchang Formation in the study area

      图  3  F899井长6段测井曲线与岩心识别裂缝之间的关系

      R0.5、R2.5及R4.0为不同测深的视电阻率测井;RILDRILM分别为深感应及中感应测井

      Fig.  3.  Relationship between logging curves and developed core fractures in the Chang 6 Member of Well F899

      图  4  研究区延长组致密砂岩微裂缝发育特征

      a.Y491井,1 731.46 m,粒间孔及粒间溶蚀孔;b.Y669井,1 839.71 m,长石溶孔;c.F808井,1 954.15 m,粒间孔及填隙物溶蚀孔;d.F668井,1 857.87 m,微裂缝;e.D4578井,2 244.80 m,微裂缝;f.Y491井,1 731.76 m,粒间孔、长石溶孔及微裂缝

      Fig.  4.  Development characteristics of microfractures in tight sandstone of Yanchang Formation in the study area

      图  5  D4578井古地磁定向实验结果

      a、b. Lc12及Lc13样品的退磁曲线;c.古地磁定向裂缝方位

      Fig.  5.  Test results of paleomagnetic orientation experiments in Well D4578

      图  6  S326井延长组热演化史及裂缝形成期次分析结果(改自何晓波,2017)

      Fig.  6.  Thermal evolution history of Yanchang Formation in Well S326 and analysis results of fracture formation stages (modified after He, 2017)

      图  7  F758井测井参数垂向分布特征

      Fig.  7.  The vertical distribution characteristics of logging parameters in Well F758

      图  8  研究区长8段裂缝型及基质型(裂缝不发育)致密砂岩储层的物性特征

      Fig.  8.  Petrophysical properties of fracture-type and matrix-type (no fractures) tight sandstone reservoirs in Chang 8 Member in the study area

      图  9  裂缝空间展布与油井产能的匹配关系

      Fig.  9.  Matching relationship between the spatial distribution of fractures and the productivity of oil wells

      图  10  W区块长81砂体展布、裂缝砂岩厚度及油藏关系图

      Fig.  10.  Relationship diagram of Chang 81 sandbody, fracture and oil reservoir in W Block

      图  11  W区块长81顶面低幅构造、裂缝砂岩厚度及油藏关系图

      Fig.  11.  Relationship among low-amplitude structures, fractures and reservoirs on the top of Chang 81 in Block W

      图  12  W区块长81裂缝平面分布及裂缝“甜点区”预测

      Fig.  12.  Plane distribution of fractures in Chang 81 and the prediction of fracture "sweet spots" in Block W

      图  13  研究区延长组致密油储层裂缝控藏模式(改自肖承钰等,2015)

      Fig.  13.  Hydrocarbon accumulation mode of fractures in tight oil reservoirs of the Yanchang Formation in the study area (modified after Xiao et al., 2015)

      图  14  研究区延长组裂缝发育规模与层厚关系

      Fig.  14.  Relationship between fracture development strength and layer thickness of Yanchang Formation in the study area

      表  1  致密砂岩微尺度裂缝类型划分方案(据Laubach, 1997)

      Table  1.   Classification scheme of microfractures in tight sandstone (Laubach, 1997)

      类型 特征 长度 形态 分布 范围
      Ⅰ型(延伸型) 孤立的;较为平直(剪性)或扭曲(张性);
      局部可有多组平行集
      μm~mm,可穿过多个颗粒 纵横比约为10‒3~10‒4
      透镜状
      所有
      地层
      区域性
      Ⅱ型(网络型) 曲线形态;相交;辐射状 与颗粒尺寸相当或
      小于颗粒尺寸
      透镜状或角状或不规则状 所有
      地层
      局部
      Ⅲ型(继承型) 颗粒内部较为孤立;尖灭于颗粒内部或颗粒边缘 与颗粒尺寸相当或小于
      颗粒尺寸
      扁平状或没有固定形态 所有
      地层
      局部
      下载: 导出CSV

      表  2  研究区延长组裂缝发育程度标准

      Table  2.   Fracture development standard of Yanchang Formation in the study area

      裂缝等级 裂缝砂岩厚度 主要裂缝类型 裂缝形态
      Ⅰ类裂缝 > 1.5 m 小尺度裂缝 垂直裂缝
      Ⅱ类裂缝 0.5~1.5 m
      Ⅲ类裂缝 0~0.5 m 微尺度裂缝 延伸型微裂缝
      非裂缝 0 m
      下载: 导出CSV
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    • 收稿日期:  2021-09-02
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