反褶积是提高地震记录分辨率的主要手段。
Dcconvoluton is one of the main tools in enhancing resolution for seismic records.
通过合成地震记录与井旁地震道的对比，从地震道中提取了非零相位的实际地震子波，并据此对原地震数据体进行子波反褶积处理。
The actual non zero phase wavelet was extracted from seismic traces by comparing synthetic seismogram with near wellbore seismic traces and was used to be deconvolved with seismic data.
讨论了基于负熵的地震盲反褶积方法。
A seismic blind deconvolution method based on negative entropy was discussed.
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