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东海陆架盆地西湖凹陷平北地区含煤地层岩性圈闭识别

牛华伟 刘苗 蒋涔 朱立新 陈茂根

牛华伟, 刘苗, 蒋涔, 朱立新, 陈茂根. 东海陆架盆地西湖凹陷平北地区含煤地层岩性圈闭识别[J]. 石油实验地质, 2022, 44(5): 755-760. doi: 10.11781/sysydz202205755
引用本文: 牛华伟, 刘苗, 蒋涔, 朱立新, 陈茂根. 东海陆架盆地西湖凹陷平北地区含煤地层岩性圈闭识别[J]. 石油实验地质, 2022, 44(5): 755-760. doi: 10.11781/sysydz202205755
NIU Huawei, LIU Miao, JIANG Cen, ZHU Lixin, CHEN Maogen. Identification of lithologic trap in coal-bearing stratum of Pingbei area, Xihu Sag, East China Sea Shelf Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2022, 44(5): 755-760. doi: 10.11781/sysydz202205755
Citation: NIU Huawei, LIU Miao, JIANG Cen, ZHU Lixin, CHEN Maogen. Identification of lithologic trap in coal-bearing stratum of Pingbei area, Xihu Sag, East China Sea Shelf Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2022, 44(5): 755-760. doi: 10.11781/sysydz202205755

东海陆架盆地西湖凹陷平北地区含煤地层岩性圈闭识别

doi: 10.11781/sysydz202205755
详细信息
    作者简介:

    牛华伟(1969-), 男, 教授级高级工程师, 从事海洋石油勘探研究及管理。E-mail: niuhw.shhy@sinopec.com

    通讯作者:

    刘苗(1983-), 男, 高级工程师, 从事石油物探研究。E-mail: liumiao.shhy@sinopec.com

  • 中图分类号: TE122.3

Identification of lithologic trap in coal-bearing stratum of Pingbei area, Xihu Sag, East China Sea Shelf Basin

  • 摘要: 东海陆架盆地西湖凹陷平北地区主要目的层始新统平湖组沉积受潮汐作用影响较大,薄砂体多层叠置、横向变化快,煤层发育。目的层埋深普遍超过3 500 m,储层物性相对较差。现有地震资料深层信噪比低、能量弱,砂泥阻抗特征差异小,储层预测及刻画难度大。在深层保幅宽频处理资料的基础上, 按照明确岩性圈闭发育类型、精细砂体描述、落实岩性圈闭目标的整体思路开展研究,明确了古地貌背景、砂体模式及岩性圈闭发育类型, 在这一格架约束下开展精细的砂体描述工作,应用地震波形、地震反射结构特征、叠前反演弹性属性相结合预测砂体,并利用叠后统计学反演预测煤层分布,提高了砂体描述的精度和可靠性。

     

  • 图  1  新、老处理资料频谱参数、信噪比对比

    Figure  1.  Spectrum parameters and signal-to-noise ratio of new and old processing data

    图  2  东海陆架盆地西湖凹陷平北地区西部平下段拉平地震剖面

    Figure  2.  Flattened seismic profile of lower section of Pinghu Formation in western Pingbei area, Xihu Sag, East China Sea Shelf Basin

    图  3  东海陆架盆地西湖凹陷平北地区平下段控砂模式

    Figure  3.  Sandstone-controlled model of lower section of Pinghu Formation in Pingbei area, Xihu Sag, East China Sea Shelf Basin

    图  4  东海陆架盆地西湖凹陷平北地区过W1-W3-W2井反演、波形剖面对比

    Figure  4.  Inversion and waveform comparison among wells W1, W3 and W2 in Pingbei area, Xihu Sag, East China Sea Shelf Basin

    图  5  东海陆架盆地西湖凹陷平北地区平湖组各层段煤层累积厚度统计

    Figure  5.  Cumulative thickness of coal seams in each section of Pinghu Formation, Pingbei area, Xihu Sag, East China Sea Shelf Basin

    图  6  东海陆架盆地西湖凹陷平北地区过W1-W3-W2井煤层识别剖面

    Figure  6.  Coal seam identification profile crossing wells W1, W3 and W2 in Pingbei area, Xihu Sag, East China Sea Shelf Basin

    图  7  东海陆架盆地西湖凹陷平北地区过W3-W5-W2井储层预测与煤层识别剖面

    Figure  7.  Reservoir prediction and coal seam identification profile crossing wells W3, W5 and W2 in Pingbei area, Xihu Sag, East China Sea Shelf Basin

    图  8  东海陆架盆地西湖凹陷平北地区顺凹槽(a)、顺斜坡(b)地震反射结构特征

    Figure  8.  Seismic reflection structure along groove (a) and down slope (b) in Pingbei area, Xihu Sag, East China Sea Shelf Basin

    图  9  东海陆架盆地西湖凹陷平北地区沉积体反射特征追踪砂体厚度(a)及P11b砂体预测厚度(b)

    Figure  9.  Tracked sand body thickness by sediment reflection features (a) and predicted thickness of P11b sand body in Pingbei area, Xihu Sag, East China Sea Shelf Basin

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  • 收稿日期:  2021-12-07
  • 修回日期:  2022-07-25
  • 刊出日期:  2022-09-28

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