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    蓬莱9-1潜山岩性组成及其对储层发育的控制

    李建平 周心怀 王国芝

    李建平, 周心怀, 王国芝, 2014. 蓬莱9-1潜山岩性组成及其对储层发育的控制. 地球科学, 39(10): 1421-1430. doi: 10.3799/dqkx.2014.134
    引用本文: 李建平, 周心怀, 王国芝, 2014. 蓬莱9-1潜山岩性组成及其对储层发育的控制. 地球科学, 39(10): 1421-1430. doi: 10.3799/dqkx.2014.134
    Li Jianping, Zhou Xinhuai, Wang Guozhi, 2014. Lithologic Constitution and Its Control on Reservoir Development on Penglai 9-1 Buried Hill, Bohai Sea Basin. Earth Science, 39(10): 1421-1430. doi: 10.3799/dqkx.2014.134
    Citation: Li Jianping, Zhou Xinhuai, Wang Guozhi, 2014. Lithologic Constitution and Its Control on Reservoir Development on Penglai 9-1 Buried Hill, Bohai Sea Basin. Earth Science, 39(10): 1421-1430. doi: 10.3799/dqkx.2014.134

    蓬莱9-1潜山岩性组成及其对储层发育的控制

    doi: 10.3799/dqkx.2014.134
    基金项目: 

    国家科技重大专项 2011ZX05023-006-002

    详细信息
      作者简介:

      李建平(1964-), 男, 高级工程师, 主要从事地层和沉积相研究.E-mail: lijp@cnooc.com.cn

    • 中图分类号: TE51

    Lithologic Constitution and Its Control on Reservoir Development on Penglai 9-1 Buried Hill, Bohai Sea Basin

    • 摘要: PL9-1潜山油藏是渤海湾盆地储量最大的古潜山油气藏之一,探明储量过亿吨.该油藏发育于庙西北凸起鞍部的中生界花岗岩侵入体顶部.凸起端部变质岩中没有油气发现.油气的分布受岩性控制明显.综合岩心观察、薄片鉴定、X粉晶衍射以及常量元素分析等技术手段,通过对比不同岩石类型的矿物组成、储集空间类型及发育程度,探讨了岩性组成对储层发育的控制作用.研究表明,变质岩中裂缝和孔隙均不发育,不能形成有效储层.花岗岩主要储集空间类型为孔隙-裂缝型,总体具有从砂质风化带→砾质风化带→裂缝带→基岩带,储集空间组合类型从孔隙→孔隙+裂缝→裂缝→不太发育的微裂缝的变化特征.储层厚度大,成层性强,可形成有效的规模性储层.花岗岩与变质岩的矿物组成差异控制了研究区优质储层的发育.变质岩中长石含量极低,不能形成溶蚀孔隙,较高含量(30%~50%)的片状矿物使其在应力作用下易发生塑性变形,不易产生裂缝.花岗岩具有很高的长石含量和含量很低的片状矿物,不仅容易被风化并产生溶蚀孔隙,而且易于发生脆性变形形成裂缝.

       

    • 图  1  研究区位置与地质要素

      a.研究区位置; b.研究区岩性、油藏与井位分布

      Fig.  1.  Location and geological elements of the study area

      图  2  PL9-1油藏剖面(剖面位置见图 1)

      Fig.  2.  Reservoir profile of the PL9-1 oil field

      图  3  13井花岗闪长岩岩心照片

      Fig.  3.  Core photos of the granodiorite in well 13

      图  4  PL9-1油藏典型岩石薄片镜下照片

      a.花岗闪长岩及其斜长石中的环带构造; b.二长花岗岩; c.钾长花岗岩; d.绢云千枚岩; e.变质砂岩和变余砂状结构; f.云母石英片岩.Q.石英; Kfs.钾长石; Pl.斜长石; Bio.黑云母; Ser.绢云母; Epi.绿帘石

      Fig.  4.  Microscopic photographs of typical rock in reservoir of the PL9-1 oil field

      图  5  潜山岩石的QAP图解

      1.富石英花岗岩;2.碱长花岗岩;3a.花岗岩;3b.花岗岩(二长花岗岩);4.花岗闪长岩;5.英云闪长岩、斜长花岗岩;6*.碱长石英正长岩;7*.石英正长岩;8*.石英二长岩;9*.石英二长闪长岩;10*.石英闪长岩、石英辉长岩、石英斜长岩

      Fig.  5.  QAP diagram of rocks from the buried hill

      图  6  2井二长花岗岩岩心照片

      Fig.  6.  Core photos of the monzogranite in well 2

      图  7  6井各种变质岩岩心照片

      a.石英片岩;b.黑云母片岩;c.糜棱岩

      Fig.  7.  Core photos of the metamorphic in well 6

      图  8  变质岩中的次生孔隙和裂缝

      a.变质砂岩中的次生生溶孔;b.片岩中的次生溶孔;c.石英岩中的显微裂缝;d.斜长石蚀变形成的次生溶孔, 斜长石蚀变成高岭土和绢云母、蚀变强烈部位形成溶孔

      Fig.  8.  Secondary pores and fissures developing in the metamorphic rocks

      图  9  各风化壳亚带储层孔隙度分布直方图

      Fig.  9.  Distribution histogram of reservoir porosity in different sub-zone of weathering crust

      图  10  花岗岩基岩储层厚度平面分布

      a.砂质带储层厚度;b.砾质带储层厚度;c.裂缝带储层厚度;d.砂质带+砾质带+裂缝带储层厚度

      Fig.  10.  Isopach map of the reservoir thickness in the granite basement rocks

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