段天柱. 沁水盆地黄土塬区三维地震勘探激发层位试验研究[J]. 地质与资源, 2019, 28(3): 309-314.
    引用本文: 段天柱. 沁水盆地黄土塬区三维地震勘探激发层位试验研究[J]. 地质与资源, 2019, 28(3): 309-314.
    DUAN Tian-zhu. EXPERIMENTAL STUDY ON THE EXCITATION HORIZON OF 3D SEISMIC EXPLORATION IN THE LOESS TABLE AREA OF QINSHUI BASIN[J]. Geology and Resources, 2019, 28(3): 309-314.
    Citation: DUAN Tian-zhu. EXPERIMENTAL STUDY ON THE EXCITATION HORIZON OF 3D SEISMIC EXPLORATION IN THE LOESS TABLE AREA OF QINSHUI BASIN[J]. Geology and Resources, 2019, 28(3): 309-314.

    沁水盆地黄土塬区三维地震勘探激发层位试验研究

    EXPERIMENTAL STUDY ON THE EXCITATION HORIZON OF 3D SEISMIC EXPLORATION IN THE LOESS TABLE AREA OF QINSHUI BASIN

    • 摘要: 沁水盆地黄土塬区地表黄土覆盖厚度不均,地震波速度差异较大,对地震勘探的激发有较大的影响.针对区域地表地层特点,设计地震地质模型,分析不同激发层位地震正演记录.结合试验区现场试验,对比分析了正演模拟记录.结果表明,合理的激发层位能够有效压制干扰波,突出目的层位反射波,提高黄土塬区三维地震原始资料的品质.

       

      Abstract: The uneven loess cover thickness and great difference of seismic wave velocity in the loess table area of Qinshui Basin have significant influence on the excitation of seismic exploration. In view of the characteristics of regional surface strata, the seismic geological modeling is designed to analyze the forward records of different excitation horizons. Combined with the field tests, the forward modeling records are compared and analyzed. The results show that the reasonable excitation horizon can effectively suppress interference wave, enhance the reflection wave of target horizon, and improve the quality of 3D seismic primary data in loess table area.

       

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