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    莺歌海盆地乐东区碳酸盐胶结物成因及地质意义

    吴仕玖 范彩伟 招湛杰 代龙 邓孝亮 钟佳

    吴仕玖, 范彩伟, 招湛杰, 代龙, 邓孝亮, 钟佳, 2019. 莺歌海盆地乐东区碳酸盐胶结物成因及地质意义. 地球科学, 44(8): 2686-2694. doi: 10.3799/dqkx.2019.154
    引用本文: 吴仕玖, 范彩伟, 招湛杰, 代龙, 邓孝亮, 钟佳, 2019. 莺歌海盆地乐东区碳酸盐胶结物成因及地质意义. 地球科学, 44(8): 2686-2694. doi: 10.3799/dqkx.2019.154
    Wu Shijiu, Fan Caiwei, Zhao Zhanjie, Dai Long, Deng Xiaoliang, Zhong Jia, 2019. Origin of Carbonate Cement in Reservoirs of Ledong Area, Yinggehai Basin and Its Geological Significance. Earth Science, 44(8): 2686-2694. doi: 10.3799/dqkx.2019.154
    Citation: Wu Shijiu, Fan Caiwei, Zhao Zhanjie, Dai Long, Deng Xiaoliang, Zhong Jia, 2019. Origin of Carbonate Cement in Reservoirs of Ledong Area, Yinggehai Basin and Its Geological Significance. Earth Science, 44(8): 2686-2694. doi: 10.3799/dqkx.2019.154

    莺歌海盆地乐东区碳酸盐胶结物成因及地质意义

    doi: 10.3799/dqkx.2019.154
    基金项目: 

    “十三五”国家重大专项《莺琼盆地高温高压天然气富集规律与勘探开发关键技术(三期)》 2016ZX05024-005

    中海石油(中国)有限公司自主立项项目《差异岩-场耦合的储盖层联控机制与有效储盖分布研究》 ZYKY-2018-ZJ-01

    详细信息
      作者简介:

      吴仕玖(1986-), 男, 工程师, 硕士, 主要从事沉积储层方面的研究

    • 中图分类号: P581

    Origin of Carbonate Cement in Reservoirs of Ledong Area, Yinggehai Basin and Its Geological Significance

    • 摘要: 为探讨乐东区碳酸盐胶结物的分布规律、成因机制及其对储层质量的影响,应用铸体薄片、碳氧同位素、包裹体对碳酸盐胶结物岩石学、地球化学等特征进行综合分析.研究结果表明,从斜坡带往凹陷中心,碳酸盐含量由18.0%降至5.0%;其δ13C值分布在-4.78‰~+1.03‰,δ18O值分布在-10.99‰~-6.34‰,Z值分布在111.27~123.59,古海水温度分布在11.36~32.02℃,古盐度分布在3.24%~6.91%;碳酸盐胶结物的形成主要与碳酸盐岩或高钙质砂岩母岩的溶解再沉淀有关,其受控于水介质温度、成岩温度与盐度,由斜坡带往凹陷中心,水介质温度降低、盐度增高,胶结变弱.低含量的早期(铁)方解石与高温热流体溶解高含量早期(铁)方解产生的低或高含量的晚期(铁)白云石区均可发育中渗“甜点”储层.

       

    • 图  1  莺歌海盆地构造区划与研究区位置

      Fig.  1.  Structure background and study area of Yinggehai Basin

      图  2  莺歌海盆地乐东区储层典型显微照片

      a. L4-1井,N1h2,2 567.0 m,极细砂岩,方解石呈基底式胶结,含量为34.5%,,壁心(-);b. D1-5井,N1h2,3 994.5 m,不等粒砂岩,方解石呈基底式胶结,含量为29%,壁心(-);c. D2-1井,N1h2,3 895.0 m,中砂岩,铁方解石充填于粒间,含量约为11%,壁心(-);d. D1-13井,N1h2,4 070.0 m,中-粗砂岩,铁方解石充填于粒间,含量为2%,粒间孔发育,Ф=11.9%,K=25.3 mD,壁心(-);e. D1-13井,N1h2,4 252.9 m,中-粗砂岩,溶蚀发育,铁方解石2%,白云石16%,Ф=14.5%,K=33.7 mD,壁心(-);f. D1-6井,N1h2,4 310.5 m,中-粗砂岩,溶蚀发育,铁白云石3%,Ф=12.2%,K=8.1 mD,壁心(-)

      Fig.  2.  Typical micrographs of reservoir rocks in Ledong area of Yinggehai Basin

      图  3  莺歌海盆地乐东区碳酸盐胶结物含量与碳氧同位素关系

      Fig.  3.  Relationship between carbonate cement content and carbon and oxygen isotopes in Ledong area of Yinggehai Basin

      图  4  莺歌海盆地乐东区碳酸盐胶结物碳氧同位素相关性

      Fig.  4.  Carbon and oxygen isotope correlation of carbonate cement in Ledong area of Yinggehai Basin

      图  5  莺歌海盆地乐东区碳酸盐胶结物含量与古盐度、古温度关系

      Fig.  5.  Relationship between carbonate cement content and paleo-salt and paleotemperature in Ledong area of Yinggehai Basin

      图  6  莺歌海盆地乐东区储层物性与碳酸盐胶结物含量关系

      Fig.  6.  Relationship between reservoir physical property and carbonate cement content in Ledong area of Yinggehai Basin

      表  1  莺歌海盆地乐东区碳酸盐胶结物含量统计

      Table  1.   Contents statistics of carbonate cements in Ledong area of Yinggehai Basin

      层位 井号 深度(m) 平均含量(%) 碳酸盐总量(%) 样品总数(个)
      菱铁矿 方解石 白云石 铁方解石 铁白云石
      N1h1 T3-1 3 238~3 320 2.0 5.6 0.2 4.0 0.0 11.8 15
      T4-1 1 950~2 100 0.0 18.4 0.0 1.4 0.0 19.8 13
      D2-1 3 710~3 790 0.1 0.0 0.0 4.0 0.0 4.1 12
      D2-7 3 720~3 910 1.1 3.5 4.3 0.0 0.0 8.9 13
      D8-7 3 700~3 900 4.4 0.0 0.0 0.0 1.1 5.5 15
      N1h2 T3-1 3 330~3 600 1.4 1.0 3.9 2.4 0.2 8.9 48
      T4-1 3 580~3 600 0.0 32.0 0.0 0.0 0.0 32.0 3
      L1-1 3 400~3 550 0.8 0.0 0.0 15.9 0.6 17.3 10
      D2-1 3 850~3 900 0.0 0.0 0.0 7.4 0.1 7.5 34
      D1-6 4 100~4 300 0.2 0.0 0.0 5.9 1.3 7.4 35
      D1-13 4 000~4 300 0.0 0.1 0.6 7.6 0.3 8.6 90
      D2-7 4 000~4 050 1.3 1.5 1.8 0.0 0.0 4.6 3
      N1m1 D2-1 4 050~4 200 0.3 0.0 1.4 8.6 0.3 10.6 41
      下载: 导出CSV

      表  2  莺歌海盆地乐东区碳氧同位素含量数据统计

      Table  2.   Average contents of different carbonate cements in Ledong area of Yinggehai Basin

      井名 岩性 δ13CPDB(‰) δ18OPDB(‰) δ18O校正(‰) t(℃) Z
      T3-1 含钙质砂岩 -3.84~-3.55(-3.70) -8.61~-8.23(-8.44) -1.11~-0.73(-0.94) 19.06~20.73(20.00) 115.21~115.74(115.52)
      L1-1 灰岩 -4.78~-0.79(-2.79) -9.52~-6.34(-7.83) -2.02~1.16(-0.43) 11.36~24.90(18.13) 114.35~120.93(117.64)
      D3-1 灰质粉砂岩 -0.94~0.21(-0.37) -8.65~-7.71(-8.18) -1.15~-0.21(-0.70) 16.86~20.92(18.89) 121.54~123.42(122.48)
      D2-1 含钙质砂岩 -3.06~1.03(-0.34) -10.99~-7.62(-9.56) -3.49~-0.12(-2.06) 16.47~32.02(25.24) 117.23~125.15(121.85)
      D1-1 含钙质砂岩 -0.55~0.50(-0.03) -8.85~-7.28(-8.00) -1.35~0.22(-0.50) 15.10~21.83(18.13) 121.77~124.41(123.26)
      D1-6 砂岩 -0.87 -9.02 -1.52 22.50 121.03
      下载: 导出CSV

      表  3  莺歌海盆地乐东区碳酸盐胶结物包裹体测试数据统计

      Table  3.   Test data of carbonate cement inclusion in Ledong area of Yinggehai Basin

      层位 井名 深度(m) 均一温度(℃) 冰点温度(℃) 盐度(%) 碳酸盐胶结物含量(%)
      N1h1 D2-1 3 762.50 146.90 12.00
      N1h2 D2-1 3 892.32 150.70 20.00
      3 873.80 161.65 -2.95 4.87 25.50
      3 906.00 -2.00 3.40 20.00
      3 907.50 151.00 -4.35 6.94 16.00
      T3-1 3 484.29 145.30 12.00
      N1m1 D2-1 4 117.50 -1.92 3.24 23.00
      4 115.00 -4.34 6.91 8.00
      4 078.00 -2.95 4.87 11.00
      4 068.30 -2.75 4.49 18.00
      4 117.50 150.00 -1.92 3.24 23.00
      4 161.50 156.00 -2.90 4.79 25.00
      下载: 导出CSV
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    • 收稿日期:  2019-02-05
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