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作 者:郭恺[1] 仝兆岐[1] 李振春[1] 吕晓东[2]
机构地区:[1]中国石油大学地球资源与信息学院,山东青岛266555 [2]河南油田测井公司,河南南阳473132
出 处:《物探与化探》2012年第5期821-826,共6页Geophysical and Geochemical Exploration
摘 要:由于在激发、接收和传播过程中受到众多干扰因素的影响,地震反射波形发生畸变,严重影响到叠加剖面的质量,因此,在叠前需要进行波形一致性校正。笔者针对单道匹配法的不足,引入伪多道匹配法,对地震波形的振幅、相位和时间进行高精度一致性校正,并能保持波形保真,提高叠加效果。模型测试和实际数据处理结果证明了本方法的有效性和适应性,在低信噪比资料处理中也可以获得比较好的效果。Because of numerous interference factors in stimulating, receiving and propagating processes, the waveform of the reflected wave is distorted in the data, which will affect the quality of the stacking section. Therefore, waveform correction is the chief factor which should be considered before stacking. This paper brings forward the pseudomuhichannel matching method aiming at remedying some de- fects in the single channel matching method. The proposed method has higher precision in amplitude, phase and travel time, and can ac- quire good effect in the low signal-to-noise data. In addition, it can gain waveform fidelity and improve the quality of the stacking sec- tion. Its validity and applicability have been proved by the processing of seismic data.
关 键 词:波形一致性校正 叠加剖面 低信噪比 单道匹配 伪多道匹配
分 类 号:P631.4[天文地球—地质矿产勘探]
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