层析静校正在延川南地区地震资料现场处理中的应用
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摘要
随着地震勘探的发展,勘探区域日趋复杂化。地表起伏大,横向岩性速度变化剧烈,低降速带横向厚度分布不均匀等因素带来的静校正问题更加突出,解决好静校正问题变得尤其重要。在讨论层析静校正原理以及分析延川南地区地震资料的基础上,采用层析静校正方法较好地解决了长波长静校正问题,有利于延川南地区地震资料后期的处理解释。
With the development of seismic survey,conditions in exploration area are becoming more complex.Because the problem of static correction caused by undulating surface,fierce lateral lithologic velocity variation and uneven transverse gage distribution in low velocity belt becomes prominent,it is important to resolve it in seismic data processing.Based on the discussion of tomographic statics correction principle and analysis of seismic data in south YanChuan area,the long wavelength correction problem has been solved by means of tomographic statics correction,contributing to later processing and interpretation for its seismic data.
引文
[1]陆基孟.地震勘探原理[M].北京:石油工业出版社,1993:93-102.
    [2]李庆忠.关于低信噪比地震资料的基本概念和质量改进方向[J].石油地球物理勘探,1986(4):343-352.
    [3]杨文采.应用地震层析成像[M].北京:地质出版社,1993:59-61.

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