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    基于波动方程的散射波成像在复杂岩溶成像的探索与应用

    Exploration and Application of Diffraction Imaging Based on Wave Equation in Complex Karst Imaging

    • 摘要: 散射波成像是利用地震波在地下介质中的散射特性来获取地下结构信息的一种成像技术。相比传统的成像技术,散射波成像可以提供更高的空间分辨率,能够更准确地揭示地下介质的微观结构,如裂隙、孔隙和岩石类型等,对于复杂碳酸盐岩的油气勘探具有重要意义。相比于传统的反射波地震成像,散射波成像技术能够利用地震波的散射波场信息,能够更充分地利用地震数据,提高了对岩溶缝洞等地质特征的识别。由于地下介质的复杂性和地震波在介质中的多种传播方式,散射波与反射波的能量往往会相互混合,导致难以准确识别和分离。为此,本文提出了一种基于波动方程的散射波成像算法,利用常规成像提取地层倾角作为散射波与反射波的分离约束条件,根据散射波与反射波在共倾角道集上的差异,实现散射波和反射波分离后,最终实现散射波成像。结果表明,散射波成像针对西南地区复杂岩溶裂缝具有良好的应用前景。

       

      Abstract: Diffraction imaging is a technique that leverages the characteristics of seismic diffracted waves to gain insights into subsurface structures. Unlike traditional imaging methods that primarily utilize reflection waves, diffraction imaging offers enhanced spatial resolution, enabling a more accurate depiction of the microstructure. This capability is particularly significant for oil and gas exploration in complex carbonate reservoirs. The distinctive feature of diffraction imaging lies in its ability to harness information from diffracted wavefields, thereby maximizing the utility of seismic data and improving the identification of geological features like karst reservoirs. Due to the intricate nature of the subsurface medium and the various propagation modes of seismic waves, the energies associated with diffracted waves often overlap with those of reflection waves, creating challenges in accurately identifying and separating them. A wave-equation based diffraction imaging algorithm is proposed with stratigraphic dip angle as constrains. The results demonstrate that diffraction imaging holds significant promise for applications in complex karst reservoirs in the Southwest China.

       

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