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    玄武岩发育区砂岩储层特征及控制因素:渤海南部BZ34-9区与KL6区块对比

    王维 杨香华 叶加仁 王清斌 朱红涛 李欢

    王维, 杨香华, 叶加仁, 王清斌, 朱红涛, 李欢, 2017. 玄武岩发育区砂岩储层特征及控制因素:渤海南部BZ34-9区与KL6区块对比. 地球科学, 42(4): 570-586. doi: 10.3799/dqkx.2017.045
    引用本文: 王维, 杨香华, 叶加仁, 王清斌, 朱红涛, 李欢, 2017. 玄武岩发育区砂岩储层特征及控制因素:渤海南部BZ34-9区与KL6区块对比. 地球科学, 42(4): 570-586. doi: 10.3799/dqkx.2017.045
    Wang Wei, Yang Xianghua, Ye Jiaren, Wang Qingbin, Zhu Hongtao, Li Huan, 2017. Characterization and Controlling Factors of Sandstone Reservoirs in Basalt Development Areas: An Example from Comparison between BZ34-9 and KL6 Areas in South of Bohai Sea. Earth Science, 42(4): 570-586. doi: 10.3799/dqkx.2017.045
    Citation: Wang Wei, Yang Xianghua, Ye Jiaren, Wang Qingbin, Zhu Hongtao, Li Huan, 2017. Characterization and Controlling Factors of Sandstone Reservoirs in Basalt Development Areas: An Example from Comparison between BZ34-9 and KL6 Areas in South of Bohai Sea. Earth Science, 42(4): 570-586. doi: 10.3799/dqkx.2017.045

    玄武岩发育区砂岩储层特征及控制因素:渤海南部BZ34-9区与KL6区块对比

    doi: 10.3799/dqkx.2017.045
    基金项目: 

    国家重大油气专项课题 2011ZX05023-001-001

    国家重大油气专项课题 2011ZX05023-001-015

    详细信息
      作者简介:

      王维 (1988-),男,博士研究生,主要从事储层地质学与层序地层学研究.ORCID:0000-0003-3594-643X.E-mail: wangweiylcug@163.com

      通讯作者:

      杨香华,ORCID:0000-0001-5699-8074.E-mail: xhyang111@vip.sina.com

    • 中图分类号: P618.13

    Characterization and Controlling Factors of Sandstone Reservoirs in Basalt Development Areas: An Example from Comparison between BZ34-9 and KL6 Areas in South of Bohai Sea

    • 摘要: 渤海南部BZ34-9区与KL6区块位于莱北低凸起南北两侧,均发育新生代玄武岩并得到钻井证实,但储层特征差异明显.以三维地震、薄片、SEM以及X衍射等技术手段对两个区块玄武岩时空展布,沉积体系以及储层特征进行对比.研究表明,BZ34-9区构造位于缓坡带,供源速率中等.渐新世玄武岩为沉积期及准同生期喷发且位于砂体主体部位,优质层段形成白云石包壳、沸石胶结溶蚀、混层粘土包膜等成岩响应,整体对储层发育发挥积极作用;KL6区构造近物源,供源强烈,渐新世玄武岩发育在凹陷内部,对砂体影响有限,储层以高岭石及碳酸盐胶结充填为特征,在成岩期受郯庐断裂带岩浆热液影响,绢云母、菱铁矿重结晶等现象普遍.对比分析表明玄武岩对储层的影响受控于火山喷发时机、物源供给速率、砂体及火山岩配置关系等因素.

       

    • 图  1  BZ34-9区与KL6区块区域地质简图

      Fig.  1.  Regional geological sketch of BZ34-9 and KL6 areas

      图  2  BZ34-9区与KL6区深度与孔隙度交会

      Fig.  2.  Porosity versus depths of BZ34-9 and KL6 areas

      图  3  火山岩溢流相-火山通道相地震相特征对比

      Fig.  3.  Seismic reflection characteristics of volcanic overflow faciesandvolcanic channel facies

      图  4  BZ34-9区火山岩三维时空展布

      a为BZ34-9区溢流相与火山通道相火山岩三维显示 (粉红色为沙一二段溢流相火山岩,黄色为沙一二段火山通道;红色为东一二段溢流相火山岩,绿色为东一二段火山通道);b、c分别为沙一二段、东一二段火山岩俯视图;d、e分别为沙一二段、东一二段火山岩侧视图 (b~e中红色为溢流相,绿色为火山通道);f.过井地震剖面,蓝色阴影为溢流相,红色阴影为火山通道;据朱红涛等 (2014)

      Fig.  4.  Spatial and temporal distribution of volcanic eruption phases in the BZ34-9 area

      图  5  KL6区玄武岩三维刻画

      a.火山岩溢流相与通道相三维显示;b、c、d.沙一二段、东一二段以及馆陶组火山岩俯视图;e、f、g.沙一二段、东一二段以及馆陶组火山岩侧视图 (橙色代表东营组溢流相,粉红色代表东一二段溢流相,红色代表馆陶组溢流相,绿色为火山通道);h.过井地震剖面,蓝色阴影代表溢流相,红色阴影代表火山通道相

      Fig.  5.  Spatial and temporal distribution of volcanic eruption phases in the KL6 area

      图  6  BZ34-9区块 (a) 与KL6区块 (b) 沉积相与火山相叠合

      a1.BZ34-9区块沙一二段;a2.BZ34-9区块东三段;a3.BZ34-9区块东一二段;b1.KL6区块沙一二段;b2.KL6区块东三段;b3.KL6区块东一二段

      Fig.  6.  Distribution of basalt and sedimentary facies of BZ34-9 and KL6 areas

      图  7  典型钻井玄武岩与泥岩黏土矿物分布

      a.BZ34-A; b.KL6-D

      Fig.  7.  Basalt development and clay mineral characteristics of typical wells of BZ34-A and KL6-D

      图  8  典型成岩矿物微观特征及能谱

      I/S.伊蒙混层;C.绿泥石;Zeo.沸石;K.高岭石

      Fig.  8.  Typical diagenetic minerals and EDX characteristics

      图  9  BZ34-9区与KL6区沙一二段储层成岩特征

      a.碎屑颗粒表面白云石包壳 (dol),BZ34-A,3 037 m,沙一段,扫描电镜照片;b.碎屑颗粒表面菱形体白云石晶体,A视域局部放大,扫描电镜照片;c.颗粒表面及粒间孔 (IP) 内栉壳状白云石及晶间孔,BZ34-A,3 084 m,沙二段,电子背散射照片;d.多期碳酸盐胶结充填,早期方解石胶结 (红色),晚期铁白云石充填 (蓝色),KL6-B,2 568 m,沙二段,单偏光;e.铁白云石充填交代石英颗粒,KL6-B,2 535 m,沙一段,单偏光;f.鳞片状高岭石等基质充填,压实,KL6-A,3 073 m,沙二段,正交光

      Fig.  9.  The features and diagenesis of reservoirs from Es1+2, BZ34-9 and KL6 areas

      图  10  BZ34-9区与KL6区东三段控制性成岩作用

      a.沸石充填粒间孔 (Z) 并次生溶蚀,BZ34-A,2 944 m,Ed3,单偏光;b.石英溶蚀呈现港湾状,BZ34-A,2 944 m,东三段,单偏光;c.混层粘土包膜,抑制石英加大,BZ34-A,2 944 m,Ed3,扫描电镜照片;d.方解石胶结 (Cal) 及钠长石化 (红色箭头),BZ34-A,2 944 m,东三段,电子背散射照片;e.菱铁矿 (S) 致密胶结交代颗粒,KL6-D,2 928.68 m,东三段,正交光;f.方解石 (红)+菱铁矿 (S) 铁白云石 (Ank) 胶结,KL6-D,3 096.61 m,东三段,单偏光;g.高岭石 (K) 致密胶结及铁白云石充填孔隙 (Ank),KL6-D,3 035 m,东三段,电子背散射照片;h.岩屑沿变质岩颗粒缝合线 (红色箭头) 溶蚀,KL6-D,2 928 m,东三段,电子背散射照片

      Fig.  10.  The features and diagenesis of reservoirs from Ed3, BZ34-9 and KL6 areas

      图  11  BZ34-9区与KL6区东三段控制性成岩作用

      a.沸石胶结 (Z) 全貌,BZ34-A,2 280 m,东二段,单偏光;b.粒间见沸石 (Z) 溶蚀,点状分布,蓝色铸体,BZ34-A,2 265 m,东二段,单偏光;c.多期沸石充填,伴生绿泥石环边 (C),BZ34-A,2 351 m,东二段,单偏光;d.储层分选差,大小混杂,压实强度大,KL6-D,2 389 m,东二段,电子背散射照片;e.长石钠长石化与溶蚀,KL6-D,2 389 m东二段,电子背散射照片;f.高岭石胶结与充填 (K),KL6-D,2 389 m,东二段,电子背散射照片

      Fig.  11.  The features and diagenesis of reservoirs from Ed1+2, BZ34-9 and KL6 areas

      图  12  KL6区热液作用矿物特征

      a.KL6-A井2 543.00 m,长石绢云母化,正交光;b.KL6-A井2 492.50 m,长石绢云母化,正交光;c.KL6-B井,2 600.00 m,长石绢云母化,正交光;d.KL6-D井,2 925.98 m,块状菱铁矿 (黑色块状),单偏光;e.KL6-D井,2 926.78 m,菱铁矿铁白云石化,单偏光;f.KL6-D,3 098.55 m,菱形体菱铁矿,扫描电镜照片

      Fig.  12.  The reservoir characteristics of KL6 area influenced by hydrothermal activities

      图  13  BZ34-A井与KL6-A井泥岩Ro

      Fig.  13.  Reflectance of vitrinite (Ro) of mudstones from KL6-A and BZ34-A

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