1887

Abstract

The presence of absorption anomalies in the overburden causes seismic images of the geological structures underneath to<br>suffer from resolution degradation, wavelet distortion and amplitude dimming, therefore reduces our ability to image and<br>interpret events inside the resulting “shadow zone”. Imaging in the presence of gas accumulations in the overburden has long<br>been recognized as a challenging problem, particularly in Southeast Asia where gas receives increasing exploration and<br>development attention. Thus, there is a need to compensate for the attenuation due to shallow gas.

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/content/papers/10.3997/2214-4609-pdb.280.iptc15048_noPW
2012-02-07
2024-04-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.280.iptc15048_noPW
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