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Deep seismic reflection data interpretation using balanced filtering method
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DOI：10.1190/GEO2016-0061.1.png)
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Abstract
En 中文
Inverse Q filtering can perform energy compensation and phase correction of seismic reflection data, but it has an instability problem due to its high-pass characteristics. Although improved methods, such as gain-limited inverse Q filtering and stabilized inverse Q filtering, overcome the instability to some extent, they are not suitable for compensating deep seismic reflection events with weak energy. Focusing on the enhancement of deep seismic events, we have developed a balanced filtering method based on the ratio of the phase-compensated signal to its analytic signal counterpart. The method is insensitive to the depth of seismic records, and it can make shallow and deep seismic records visible simultaneously. When tested on synthetic data and real seismic data, compared with other methods, the balanced filtering method improves the amplitude strength of the deep reflection events and the continuity of shallow and deep seismic events effectively, which makes the deep reflection data easier to interpret.
Keywords:
INVERSE Q-FILTER
FOURIER-TRANSFORM
ATTENUATION
PROPAGATION
DISPERSION
MIGRATION
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