OVT域地震资料分偏移距相干体融合技术在挠曲带解释中的应用

    Application of an OVT-domain seismic data split-offset coherence cube fusion technique in flexure zone interpretation

    • 摘要: 挠曲构造作为煤矿井下一种致灾性强的重要地质构造,其精确识别与刻画一直是矿井地质保障的技术难点,常规地震勘探方法受限于分辨率和信噪比影响,难以实现对其构造的精细识别。全数字高密度三维地震技术凭借其宽频带、宽方位、高覆盖次数的技术特点,为挠曲构造的精细解释提供了高质量的数据基础。本文以阳泉矿区某区块为研究对象,基于全数字高密度三维地震勘探数据,提出并系统实践了一种基于OVT域的分偏移距相干体融合技术。该方法首先在OVT域中将地震数据按偏移距划分为远、中、近3个区间,分别采用第三代C3相干算法计算各偏移距范围的相干数据体;在此基础上,运用属性融合技术将分偏移距相干体切片融合成为一幅综合相干体切片,从而实现了研究区内主挠曲带及其他隐伏构造的精细刻画,研究表明,该技术对挠曲构造的识别结果与井下实际揭露情况吻合,OVT域分偏移距相干体融合技术能够充分利用宽方位地震数据中丰富的方位角与偏移距信息,有效克服单一相干体在多解性和分辨率方面的局限,通过不同偏移距间地震响应特征的互补与融合,显著提升了挠曲带构造精细识别能力,为实现煤矿隐蔽致灾地质因素的“透明化”探测提供了有效技术途径。

       

      Abstract: Flexure structures are highly hazardous geological structures in underground coal mines. Their accurate identification and characterization have long been a technical challenge in the geological guarantee of the mines. Conventional seismic exploration methods struggle to achieve fine-scale identification of flexure structures due to their limitations in resolution and signal-to-noise ratio. In contrast, fully digital high-density 3D seismic exploration technology, characterized by wide frequency bands, wide azimuths, and high coverage frequency, can provide high-quality data for fine-scale interpretation of flexure structures. This study investigated a block in the Yangquan mining area. Using the fully digital, high-density 3D seismic exploration data, this study proposed and systematically implemented an offset vector tile (OVT)-domain split-offset coherence cube fusion technique. Specifically, the seismic data were classified into far-, moderate-, and near-offset intervals in the OVT domain. The coherence cubes in the three intervals were computed using the third-generation coherence (C3) algorithm. Furthermore, the attribute fusion technique was employed to integrate the split-offset coherence cube slices into a comprehensive coherence cube slice, enabling fine-scale characterization of the main flexure zone and other concealed structures within the study area. The results demonstrate that the identified flexure structures based on the proposed technique align with the actual wellbore exposures. By leveraging the rich azimuth and offset information in wide-azimuth seismic data, the proposed technique can effectively overcome the limitations of individual coherence cubes in terms of the multiplicity of solutions and resolution. Furthermore, by complementing and integrating seismic response characteristics across different offsets, this technique can significantly enhance the capability for fine-scale identification of flexure structures. Therefore, this study provides an effective technical approach for achieving transparent detection of concealed geological hazards in coal mines.

       

    /

    返回文章
    返回