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首页> 外文期刊>Open Journal of Geology >The Seismic-Geological Comprehensive Prediction Method of the Low Permeability Calcareous Sandstone Reservoir
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The Seismic-Geological Comprehensive Prediction Method of the Low Permeability Calcareous Sandstone Reservoir

机译:低渗透钙质砂岩油藏地震地质综合预测方法

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Currently in Niu-zhuang sub-sag, the seismic reflection amplitude of the newly discovered turbidite sandstone is stronger in the third Segment. The main reason is that Calcareous components accounts for a large part and physical properties is relatively poor, which results in no corresponding relation between reservoir and seismic attributes, and effective reservoir is difficult to predict and describe. Therefore, using the method of geological statistics, we firstly study the distribution of calcareous matters, secondly study the contribution to seismic reflection amplitude made by Calcareous high impedance component; thirdly analyze its influence on actual seismic reflection amplitude and determine the lithology thickness of Calcareous via replacement forward modeling. At last, we characterize the reservoir using the amplitude of calcareous matters. It proves that the method of seismic-geological comprehensive prediction is reliable. It has good guidance for exploration and development of the calcareous sand lithologic reservoir in similar areas.
机译:目前,在牛庄子凹陷,新发现的浊积砂岩的地震反射幅度在第三段更强。主要原因是钙质组分占很大一部分,物性相对较差,致使储层与地震属性之间没有对应关系,有效储层难以预测和描述。因此,我们首先采用地质统计的方法,研究了钙质的分布,其次研究了钙质高阻抗成分对地震反射振幅的贡献。第三,分析其对实际地震反射振幅的影响,并通过置换正演模拟确定钙质的岩性厚度。最后,我们利用钙质的振幅来表征储层。证明了地震地质综合预测方法是可靠的。对类似地区的钙质砂岩岩性油藏勘探开发具有很好的指导意义。

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