浅海重力流低渗细粒沉积砂岩储层质量评价与预测

朱绍鹏, 张冲, 周伟, 孟迪, 汤晓宇. 浅海重力流低渗细粒沉积砂岩储层质量评价与预测——以莺歌海盆地东方A区黄流组一段为例[J]. 海洋地质前沿, 2025, 41(6): 1-13. doi: 10.16028/j.1009-2722.2024.189
引用本文: 朱绍鹏, 张冲, 周伟, 孟迪, 汤晓宇. 浅海重力流低渗细粒沉积砂岩储层质量评价与预测——以莺歌海盆地东方A区黄流组一段为例[J]. 海洋地质前沿, 2025, 41(6): 1-13. doi: 10.16028/j.1009-2722.2024.189
ZHU Shaopeng, ZHANG Chong, ZHOU Wei, MENG Di, TANG Xiaoyu. Quality evaluation and prediction of low permeability fine-grained sandstone reservoir of shallow marine gravity flow: a case study of the First Member of Huangliu Formation in Dongfang A area of Yinggehai Basin[J]. Marine Geology Frontiers, 2025, 41(6): 1-13. doi: 10.16028/j.1009-2722.2024.189
Citation: ZHU Shaopeng, ZHANG Chong, ZHOU Wei, MENG Di, TANG Xiaoyu. Quality evaluation and prediction of low permeability fine-grained sandstone reservoir of shallow marine gravity flow: a case study of the First Member of Huangliu Formation in Dongfang A area of Yinggehai Basin[J]. Marine Geology Frontiers, 2025, 41(6): 1-13. doi: 10.16028/j.1009-2722.2024.189

浅海重力流低渗细粒沉积砂岩储层质量评价与预测

  • 基金项目: 海南省“南海新星”科技创新人才平台项目“东方1-1气田高温高压低渗气藏成因机制与精细表征研究”(NHXXRCXM202368)
详细信息
    作者简介: 朱绍鹏(1980—),男,硕士,高级工程师,主要从事油气田开发方面的研究工作. E-mail:zhushp@cnooc.com.cn
    通讯作者: 张冲(1988—),男,博士,高级工程师,主要从事复杂油气储层地质方面的研究工作. E-mail:zhangchong16@cnooc.com.cn
  • 中图分类号: TE122.1

Quality evaluation and prediction of low permeability fine-grained sandstone reservoir of shallow marine gravity flow: a case study of the First Member of Huangliu Formation in Dongfang A area of Yinggehai Basin

More Information
  • 莺歌海盆地东方A区高温高压低渗气藏尚未实现规模有效开发,寻找有利储层至关重要。通过激光粒度、铸体薄片、扫描电镜、高压压汞等岩芯测试分析手段,首先研究了储层微观差异特征,并对储层质量差异进行分类评价,然后通过分析储层质量差异与测井曲线间的响应关系,筛选能用于评价储层质量的测井曲线,利用主成分分析法构建了可反映储层质量好坏的敏感因子曲线,最后基于敏感因子曲线协同波形指示模拟方法对储层质量进行预测。结果表明,储层质量主要由泥质产出特征决定,当储层物性差异较大,但泥质含量与沉积粒度特征相近时,可根据其泥质产状特征将研究区低渗储层质量划分为3个级次:Ⅰ级储层的泥质产状以有序分布的泥质条带为主,发育粗粒粉砂岩,溶蚀作用强烈;Ⅱ级储层主要特征为泥质混杂分布,发育中—粗粒粉砂岩,溶蚀强度中—强;Ⅲ级储层的泥质产状呈杂基分散状态,沉积细粒粉砂岩,溶蚀发育较弱。其中,Ⅰ级与Ⅱ级储层属于优质储层。建立的储层质量分级评价模型累计方差贡献率可达98.1%,能够反映研究区储层质量差异;提出了基于储层质量敏感因子和地震波形指示模拟相协同的储层质量预测方法,预测结果与实钻资料吻合率高,能揭示有利储层的空间展布,对气田的开发决策和井位部署具有指导意义。

  • 加载中
  • 图 1  莺歌海盆地构造划分、研究区位置和地层分布

    Figure 1. 

    图 2  莺歌海盆地东方A区黄一段储层岩芯沉积构造特征

    Figure 2. 

    图 3  莺歌海盆地东方A区黄一段储层孔渗关系

    Figure 3. 

    图 4  莺歌海盆地东方A区黄一段储层镜下成岩作用与孔喉结构特征

    Figure 4. 

    图 5  莺歌海盆地东方A区黄一段储层压汞曲线特征

    Figure 5. 

    图 6  莺歌海盆地东方A区黄一段储层泥质产状

    Figure 6. 

    图 7  泥质含量、泥质产状与渗透率关系

    Figure 7. 

    图 8  莺歌海盆地东方A区黄一段储层质量分级的常规测井曲线交会图

    Figure 8. 

    图 9  莺歌海盆地东方A区黄一段储层质量分级判别主因子与次因子交会图

    Figure 9. 

    图 10  莺歌海盆地东方A区D13井储层质量分级测井识别结果

    Figure 10. 

    图 11  地震波形指示模拟反演成果频率构成

    Figure 11. 

    图 12  莺歌海盆地东方A区黄一段储层质量分级过井模拟剖面

    Figure 12. 

    图 13  莺歌海盆地东方A区黄一段储层质量分级反演切片

    Figure 13. 

    表 1  莺歌海盆地东方A区黄一段储层质量分级特征

    Table 1.  The reservoirs quality grading based on mainly the mudstone texture of the First Member of Huangliu Formation in Dongfang A area, Yinggehai Basin

    储层质量级次 粒度
    泥质含量/% 泥质
    产状
    孔隙度/% 渗透率/10−3 μm2 薄片照片 测井曲线响应
    测井曲线特征描述
    宏观 微观
    6.15 4~15 条带状 >16 >0.5 GR曲线呈高幅度箱形、钟形
    6.18 10~20 混杂分布 14~16 0.2~0.5 GR曲线呈中幅度箱形、钟形
    6.25 >15 杂基分散 <14 <0.2 GR曲线呈较为平直的微齿形
    下载: 导出CSV

    表 2  莺歌海盆地东方A区黄一段储层质量分级判别函数特征值信息统计

    Table 2.  Statistics of discriminant function eigenvalues for reservoir quality grading of the First Member of Huangliu Formation in Dongfang A area, Yinggehai Basin

    判别函数 特征值 方差贡献率/% 累积方差百分比/% 典型相关性
    1 7.325 98.1 98.1 0.938
    2 0.142 1.9 100 0.353
    下载: 导出CSV
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出版历程
收稿日期:  2024-07-30
刊出日期:  2025-06-28

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