基于地震融合属性的砂体连通性判断方法以渤中凹陷中浅层砂体为例

A method for judging sand body connectivity based on seismic fusion attributes: A case of the Bozhong Sag

  • 摘要: 关于渤中凹陷区中浅层明化镇组下段砂体精细化描述的薄互层以及地震、测井资料较少,砂体连通性的判定问题难以解决。基于研究区实际地震、测井和地质资料,根据砂体实际特征建立了对应模型,通过正演模拟技术中的波动方程法验证、优选适合的地震属性。由地震属性分析技术探究出砂体在最小尺度横向距离 \frac18\mathrm\lambda 、纵向叠置 \frac16\mathrm\lambda 的情况下,均方根振幅属性、甜点属性和主频属性在中浅层层段比地震资料判断砂体连通性的效果更好。研究区的X5井验证得到,地震融合属性与砂体厚度相关性明显提升,可以定量计算出砂体本身的厚度以及砂体间接触点的距离,对研究区砂体的连通性起到良好的判定作用。

     

    Abstract: The fine description of sand bodies in the lower member of the Minghuazhen Formation (Neogene) in the middle and shallow layers of the Bozhong Sag, Bohai Bay, is limited due to thin interbeds and insufficient seismic and logging data, making it difficult to determine the connectivity of sand bodies. Based on the actual seismic, logging, and geological data in the study area, a corresponding model was established based on the actual characteristics of the sand bodies in the study area, and suitable seismic attributes were verified and optimized through the wave equation method in forward modeling technology. By using a minimum horizontal distance of 1/8 of wavelength and a vertical overlap of 1/6 the wavelength, the root mean square amplitude attribute, sweet spot attribute and main frequency attribute were more effective than using seismic data in determining the connectivity of sand bodies in mid-to-shallow layers. According to the verification of Well X5 logging in the study area, the correlation between seismic fusion attribute and sand body thickness was significantly improved, and the thickness of sand body itself and the distance of contact points among sand bodies could be quantitatively calculated, which played a good role in determining the connectivity of sand bodies in the study area.

     

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