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基于地震波形指示反演的扇三角洲有效储层预测技术

Effective reservoirs prediction technique for fan deltas based on seismic waveform indication inversion

  • 摘要: 为精准刻画海拉尔盆地乌南次凹南屯组扇三角洲强非均质性薄互层有效储层,探索地震波形指示反演技术的适用性。基于岩性敏感性分析,优选自然伽马(GR)曲线区分砂泥岩;通过电阻率(>3.5 Ω·m)与密度(<2.45 g/cm3)交会确定有效储层敏感参数。通过多种反演方法对比分析,优选波形指示反演方法,设置4个样本集对应沉积微相,先开展GR反演识别岩性,再对电阻率与密度体交会反演,实现有效储层定量预测。反演结果清晰反映“上泥下砂”旋回及2 m级隔夹层,电阻率-密度交会剖面与测井解释结果吻合良好。29口后验井平均符合率87.57%。结合构造与成藏条件,优选6个潜力区块(面积共6.09 km2),预测地质储量673.554×104 t,提出6口井的部署方案。波形指示反演显著提升扇三角洲薄互层有效储层预测精度,为同类陆相盆地储层评价与开发提供可靠技术支撑。

     

    Abstract: To accurately characterize the highly heterogeneous, thin-bedded effective reservoirs in fan-delta deposits of Nantun Formation, in Wunan Sub-sag, Hailar Basin, this study evaluates the applicability of seismic waveform indication inversion. Based on lithology sensitivity analysis, gamma-ray (GR) logs are selected to distinguish sandstone from mudstone. Cross-plots of resistivity (>3.5 Ω·m) and density (<2.45 g/cm3) are used to screen sensitive parameters for identifying effective reservoirs. After comparing various inversion methods, waveform indication inversion was adopted with four sample sets corresponding to sedimentary microfacies. GR inversion was first conducted for lithology identification, followed by cross-plot inversion of resistivity and density data to quantitatively predict effective reservoirs. The inverted sections clearly reveal "mudstone-over-sandstone" cycles and 2 m-scale mudstone interlayers. Resistivity-density cross-plot sections are highly consistent with interpreted results from well log. Validation using 29 blind wells yields an average coincidence rate of 87.57%. Combined with structural and accumulation conditions, six favorable blocks (total area 6.09 km2) were selected, with predicted reserves of 673.554×104 t, and a six-well deployment plan was proposed. Waveform indication inversion significantly improves prediction accuracy for thin, heterogeneous fan-delta effective reservoirs, providing a reliable technical basis for reservoir evaluation and development in similar continental basins.

     

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