深层砂泥岩薄互层的地震识别方法
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国家大型油气田及煤层气开发科技专项资助项目(2011ZX05006-004)


Seismic identification method of deep thin sand shale interbedding
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    摘要:

    深层砂泥岩薄互层油气藏是一类典型的低孔、低渗型油气藏,储层一般具有埋藏深、横向变化快、深层物性差的特点。利用常规的薄层定量描述方法只能识别地层厚度不小于λ/4的孤立薄层,很难实现精细解释。为此,采用正-反演联合预测技术,通过建立符合地下实际情况的的地球物理模型,从正演角度分析目的层的地震波场特征;同时对正演结果进行模型反演,定量分析反演砂体的横向及纵向展布特征。结果表明这种基于模型正演的地震识别方法既能够发挥地震资料在地层横向展布上的优势,又能够提高纵向上的解释精度,为识别前梨园地区深层砂、泥岩互层结构的隐蔽性储层提供参考。

    Abstract:

    The deep interbeds of sand and shale reservoir is a kind of typical low porosity and low permeability reservoir, which generally has the characteristics of deep burial, rapid lateral variation, and deep physical difference, etc. The traditional thin layer quantitative description method can only identify the stratigraphic whose thickness is less than λ/4, and it’s difficult to realize fine interpretation. Therefore, the paper firstly uses inversion joint prediction techniques to establish geological models for wave equation forward, and then analysis the target layer’s characteristics of seismic wave field from the forward angle. Finally, we apply wave impedance inversion that is based on forward modeling results to make quantitative analysis for inversion sand’s horizontal and vertical distribution characteristics. The results show that the seismic identification method which is based on forward model can not only unleash the advantages of seismic horizontal distribution, but also improve the accuracy of interpretation in the vertical direction. And the results can provide references for identifying deep thin sand shale interbedding reservoirs in Qianliyuan area.

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杨飞,黄诚,李鹏飞,桂红兵.深层砂泥岩薄互层的地震识别方法[J].重庆大学学报,2014,37(9):136-143.

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  • 收稿日期:2014-07-15
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  • 在线发布日期: 2014-12-29
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