南方煤系地层小断层地震物理模型研究

    Seismic physical model of small fault in southern coal-bearing strata

    • 摘要:
      研究目的 针对南方煤田煤系地层岩性特征和地质构造分布,目前依靠传统方法,识别落差≤5 m小断层存在极大的局限性且难度较大,而地震物理模型是目前最有可能实现系统研究小断层的技术手段。
      研究方法 以南方煤田——贵州省六盘水煤田为例,根据对研究区的实地勘探与资料收集,设计地震物理模型。由于小断层的制作难度及特殊性,采用特有的空间尺寸比例1∶2 000,速度比为1∶1.74,首次在国内实现对不同埋深5 m、3 m和1 m小断层的构建,从而制作完成了南方煤系地层小断层地震物理模型,对地震数据进行采集,并对模型原始地震数据进行分析及处理,得到模型叠加剖面。
      研究结果 可以通过相似比原理选取特定比例因子,进行原料配比,完成包含落差≤5 m小断层地震物理模型的制作,为后续采集地震数据对煤田小断层进行识别及研究小断层波场特征提供试验平台。
      结论 本次研究建立了一套适用于南方煤田小断层识别的地震物理模型实验体系,验证了相似比原理与小断层模型构建的可行性,突破了传统方法难以识别小断层的技术局限。该模型为研究小断层的波场特征、地震响应机制及后续小断层精细识别提供了实验平台与理论支撑,对提升南方煤系构造精细解释能力具有重要意义。

       

      Abstract:
      Objective Given the lithological characteristics and geological structure distribution of coal−bearing strata in southern coalfields, traditional methods face significant limitations and challenges in identifying small faults with a displacement of ≤5 m. Seismic physical modeling is currently the most promising technique for systematically studying small faults.
      Methods Taking the southern coalfield—Liupanshui Coalfield in Guizhou Province, as an example, a seismic physical model was designed based on field exploration and data collection. Due to the complexity and specificity of constructing small faults, a unique spatial scale ratio of 1∶2000 and a velocity ratio of 1∶1.74 were adopted. For the first time in China, small faults at different burial depths of 5 m, 3 m, and 1 m were successfully simulated, leading to the completion of a seismic physical model of small faults in coal−bearing strata. Seismic data were then acquired, and the raw seismic data from the model were analyzed and processed to obtain the stacked seismic profile.
      Results By applying similarity principles and selecting specific scaling factors, raw materials were proportioned to successfully construct a seismic physical model incorporating small faults with a displacement of ≤5 m. This model provides an experimental platform for acquiring seismic data, identifying small faults in coalfields, and studying their wavefield characteristics.
      Conclusions This study establishes a seismic physical modeling system suitable for identifying small faults in southern coalfields, demonstrating the feasibility of constructing fault models based on the similarity principle. The developed model overcomes the technical limitations of conventional methods in detecting small faults, and offers a reliable experimental foundation for investigating wavefield responses and seismic recognition mechanisms. It provides theoretical support for the refined interpretation of geological structures in southern coal-bearing stratas.

       

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