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    涠西南凹陷西北陡坡带流三段砂砾岩储层特征与主控因素

    徐燕红 杨香华 梅廉夫

    徐燕红, 杨香华, 梅廉夫, 2020. 涠西南凹陷西北陡坡带流三段砂砾岩储层特征与主控因素. 地球科学, 45(5): 1706-1721. doi: 10.3799/dqkx.2019.174
    引用本文: 徐燕红, 杨香华, 梅廉夫, 2020. 涠西南凹陷西北陡坡带流三段砂砾岩储层特征与主控因素. 地球科学, 45(5): 1706-1721. doi: 10.3799/dqkx.2019.174
    Xu Yanhong, Yang Xianghua, Mei Lianfu, 2020. Reservoir Characteristics and Main Control Factors of Conglomerate Reservoir of El3 in the Northwest Steep Slope Zone of Weixinan Depression. Earth Science, 45(5): 1706-1721. doi: 10.3799/dqkx.2019.174
    Citation: Xu Yanhong, Yang Xianghua, Mei Lianfu, 2020. Reservoir Characteristics and Main Control Factors of Conglomerate Reservoir of El3 in the Northwest Steep Slope Zone of Weixinan Depression. Earth Science, 45(5): 1706-1721. doi: 10.3799/dqkx.2019.174

    涠西南凹陷西北陡坡带流三段砂砾岩储层特征与主控因素

    doi: 10.3799/dqkx.2019.174
    基金项目: 

    国家“十三五”油气重大专项 2016ZX05024-006

    详细信息
      作者简介:

      徐燕红(1991-), 女, 博士研究生, 主要从事储层地质研究工作.ORCID:0000-0002-8595-3163.E-mail:18062796419@163.com

      通讯作者:

      杨香华, ORCID:0000-0002-0567-6590.E-mail:xhyang@cug.edu.cn

    • 中图分类号: P618

    Reservoir Characteristics and Main Control Factors of Conglomerate Reservoir of El3 in the Northwest Steep Slope Zone of Weixinan Depression

    • 摘要: 通过岩心观察、薄片鉴定、扫描电镜、X射线衍射分析等实验手段,结合物性、有机质演化、埋藏史、测录井等资料,研究涠西南凹陷西北陡坡带流三段砂砾岩储层储集性能、成岩特征及物性主控因素.结果表明:(1)流三段储层岩石类型以岩屑砂岩为主,岩性以粗粒级砂砾岩、含砾粗砂岩为主,储集空间以粒内溶孔、残余粒间孔、铸模孔等为主,物性变化大,以低孔特低渗、中孔低渗、中孔中渗、高孔高渗为特征,非均质性强.(2)持续的压实作用是物性变差的主要原因,碳酸盐胶结和自生粘土矿物充填使部分原生孔隙丧失,高泥质含量部位表现为早期强压实;粗粒级砂岩的中-强溶蚀作用有利于次生孔隙的发育,而微裂缝是深层砂砾岩储层的重要渗流通道之一.西北斜坡带流三段扇三角洲水下分流河道发育厚层的砂砾岩、含砾粗砂岩,杂基含量低,压实作用较弱,是研究区的优质储层发育带;湖底扇压实作用强,微裂缝提供了有机酸性流体活动的渗流通道,砂砾岩储层发生次生溶蚀使储集性能得以改善,为深层相对有利储层.

       

    • 图  1  涠西南凹陷位置、区域构造格架(a)及地层系统(b)

      Fig.  1.  Location, regional tectonic framework (a) and stratum system (b) of Weixinan depression

      图  2  涠西南凹陷西北陡坡带流三段砂岩组分三角图

      Fig.  2.  The Q-F-R diagram of El3 sandstone in the northwest steep slope zone of Weixinan depression

      图  3  研究区砂砾岩储层孔、渗分布直方图及物性交会图

      Fig.  3.  Porosity and permeability distribution histogram(a, b)and physical property crossplot(c)of conglomerate reservoir in the study area

      图  4  涠西南西北部砂岩储层储集空间类型

      a.WZ10-3W-1井,2 152.41 m(-),原生粒间孔(Pp)、次生溶孔(Sp)均发育;b. WZ10-3W-1井,2 041.89 m(-),孔隙不发育,构造作用形成的穿粒缝被沥青等充填;c. WZ11-2-2井,3 306.45 m(-),长石粒内溶孔(Sp),贴粒缝(箭头指示);d. WZ11-2-2井,3 303.91 m(-),长石、岩屑溶蚀作用强烈,形成粒内溶孔、铸模孔(Mh),发育构造微裂缝(箭头指示);e. WZ11-2-2井,3 250.27 m(-),粒内成岩缝;f. WZ10-3W-1井,2 547.61 m(-),红线左边粗粒部分发育次生溶孔、粒内缝,右边细粒部分被暗色基质充填

      Fig.  4.  Storage space types of sandstone reservoir in the northwestern Weixinan depression

      图  5  涠西南西北部砂岩储层主要成岩作用

      a.WZ11-2-2井,3 306.45 m(+),砂砾岩,强压实压溶作用,颗粒间凹凸-缝合线接触(Q代表石英,F代表长石,R代表岩屑),发育长石粒内溶蚀孔;b. WZ10-3W-1井,2 048.29 m(+),粗砂岩,方解石(Cal)不均匀充填粒间,并沿颗粒边缘交代颗粒;c. WZ10-3W-1井,2 061.24 m(-),中砂岩,紫红色铁方解石胶结作用;d. WZ10-3W-1井,2 058.39 m(+),中-细砂岩,放射状菱铁矿(Sd)交代碎屑颗粒及泥质杂基;e. WZ11-2-3井,2 646.00 m(-),粉细砂岩,晶粒状菱铁矿胶结作用;f. WZ11-2-3井,2 958.00 m(-),中砂岩,细晶白云石(Dol)胶结、交代作用;g. WZ11-2-2井,3 158.63 m(SEM),砂砾岩,书页状高岭石(K)和丝片状伊利石(I);h. WZ11-2-3井,3 225.03 m(SEM),含砾粗砂岩,蜂窝状伊蒙混层(I/S)堵塞孔隙;i. WZ11-2-3井,3 229.13 m(SEM),含砾粗砂岩,叶片状、玫瑰花状绿泥石(Chl)充填次生孔隙;j. WZ11-2-2井,3 158.44 m(-),长石强烈溶蚀,形成暗色粘土矿物;k. WZ11-2-2井,3 303.91 m(-),砂砾岩,长石、岩屑强烈溶蚀形成次生孔隙,或粘土化(红色虚线圈定区域);l. WZ11-2-2井,3 307.15 m(-),砂砾岩,长石溶蚀,生成伊利石

      Fig.  5.  Major diagenesis of sandstone reservoir in the northwestern Weixinan depression

      图  6  涠西南凹陷西北带地层埋藏史

      a.扇三角洲; b.湖底扇

      Fig.  6.  Burial history of the northwest steep slope zone of Weixinan depression

      图  7  涠西南西北陡坡带流三段储层成岩演化

      Fig.  7.  Diagenetic evolution of El3 reservoir in the northwest steep slope zone of Weixinan depression

      图  8  研究区成岩相孔-渗分布交会图

      Fig.  8.  Porosity and permeability distribution crossplot for diagenetic facies in the study area

      图  9  研究区成岩相常规测井曲线交会图

      Fig.  9.  Conventional logging crossplots for diagenetic facies in the study area

      图  10  流三段砂岩储层孔渗-岩性对比

      Fig.  10.  Porosity-lithology comparison diagram of El3 sandstone reservoir

      图  11  涠西南西北陡坡带流三段储层综合分析

      Fig.  11.  Comprehensive analysis of El3 sandstone reservoir in the northwest steep slope zone of Weixinan depression

      表  1  研究区流三段砂岩储层碳酸盐胶结物含量统计

      Table  1.   Statistics on carbonate cement content of El3 sandstone in the study area

      井号 深度(m) 方解石(%) 铁方解石(%) 白云石(%) 铁白云石(%) 菱铁矿(%) 总孔隙度(%)
      WZ10-3-1 1 943.07 34 / / / 4 /
      1 946.56 / 14 0.2 / 0.2 3
      1 981.00 / / / / 30 /
      2 005.00 / / / / 22 /
      2 035.00 41 / 0.2 / / 1
      WZ10-3-2 2 023.15 / / / / 12 2
      2 083.00 / / / / 26 /
      2 095.00 20 / / / / /
      WZ10-3-3 2 052.00 38.5 / / / / 0.2
      2 054.05 30 / / / / 1
      2 054.90 22 / / / 28 /
      2 054.95 30 / / / / /
      2 108.60 / / 8 / 5 1
      WZ10-3W-1 2 040.05 / / 1 / 45 1.5
      2 049.29 / 16 / / 2 2
      2 050.44 / / 13.5 / 13.5 0.2
      2 058.39 / 0.2 / 6.5 10 3
      WZ11-1-1 2 687.80 15 / / / / 0.2
      2 700.00 / 12 / / 6 4.5
      2 716.00 34 / / / / 0.2
      下载: 导出CSV

      表  2  研究区流三段砂岩储层粘土矿物相对含量分析

      Table  2.   Relative content analysis of clay minerals of El3 sandstone in the study area

      沉积相 井号 深度范围(m) 蒙脱石(%) 伊蒙混层(%) 伊利石(%) 高岭石(%) 绿泥石(%) 样品个数
      扇三角洲平原 WZ10-3-1 1 936~1 950 / 5.43 22.88 71.69 / 9
      WZ10-3-3 2 055~2 178 / 26.43 31.97 39.27 2.33 9
      WZ10-3-13 1 957~2 106 6.77 20.01 29.72 34.04 9.46 21
      WZ10-3W-1 2 039~2 056 16.48 9.93 35.04 28.28 17.15 24
      扇三角洲前缘 WZ11-1-1 2 982~3 348 / 34.67 54.88 5.43 5.03 15
      湖底扇 WZ11-2-2 3 156~3 308 / 3.90 70.40 4.60 21.10 10
      WZ11-2-3 3 225~3 234 / 4.50 75.42 17.17 2.92 12
      下载: 导出CSV

      表  3  流三段砂岩储层成岩相类型

      Table  3.   The types of diagenetic facies of El3 reservoir

      成岩相类型 成岩相定量参数 成岩特征 岩性 面孔率(%)
      压实率(%) 胶结率(%) 溶蚀率(%)
      弱压实-弱胶结相 < 30 < 30 < 30 颗粒不接触或点接触,原生粒间孔为主,少量溶蚀孔隙,孔隙连通性好 含砾粗砂岩、砂砾岩 20~30
      中压实-中溶蚀相 30~70 < 30 30~60 颗粒点-线接触,长石、岩屑溶蚀较强烈,部分粘土化,孔隙以粒内溶孔、剩余粒间孔为主,连通性中等 含砾粗砂岩、砂砾岩 13~20
      强压实中-强溶蚀相 > 70 30~70 60~90 颗粒线接触为主,长石、岩屑强烈溶蚀形成粒内溶孔、铸模孔,孔隙发育中等,连通性较差 砂砾岩 5~15
      压实-充填相 > 70 30~70 < 30 基质含量高,以泥质和粘土矿物为主.孔隙不发育或仅发育少量长石溶孔、杂基微孔 粉-细砂岩 < 5
      碳酸盐致密胶结相 > 30 > 80 < 30 颗粒互不接触或点接触.方解石含量10%~30%,不发育孔隙,或仅发育少量孤立微溶孔 细-中砂岩 < 3
      下载: 导出CSV

      表  4  流三段砂岩储层成岩相测井识别参数

      Table  4.   Logging identification parameters of diagenetic facies of El3 sandstone reservoir

      成岩相 ACμs/ft) GR(API) RT(ohmm) CNCF(v/v) DEN(g/cm3
      弱压实弱胶结相成岩相 90~100 60~120 10~15 0.23~0.27 2.20~2.40
      中压实中溶蚀相 80~95 40~90 0~15 0.18~0.30 2.15~2.40
      强压实中-强溶蚀相 68~80 50~140 10~15 0.10~0.15 2.35~2.60
      压实-充填相 80~90 145~210 8~12 0.15~0.30 2.40~2.60
      碳酸盐致密胶结相 70~85 110~195 12~20 0.25~0.35 2.40~2.60
      下载: 导出CSV

      表  5  不同沉积相带砂岩孔隙度、渗透率分布统计

      Table  5.   Statistics of porosity and permeability distribution of sandstone in different sedimentary zones

      沉积相带 孔隙度(%) 渗透率(10-3 μm2
      分布 平均值 分布 平均值
      分流河道 3.54~28.20 13.10 0.035~1 761 68.76
      水下分流河道 6.34~28.45 17.98 0.010~4 481 388.59
      分流河道间 3.46~11.40 8.98 0.030~6.120 1.06
      越岸沉积 6.10~14.10 10.32 0.170~4.850 1.27
      席状砂 6.61~9.92 8.27 0.020~1.570 0.61
      湖底扇 3.20~19.10 11.81 0.069~29.400 4.81
      下载: 导出CSV
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