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Abstract

In towed streamer marine seismic acquisition, data is typically recorded over a bandwidth of 2-250Hz. This is represented by a wavelet of finite width with side lobes in the time domain when zero phased. This ideal wavelet is distorted by two major factors: the source and receiver-side ghosts and absorption due to various propagation effects (Q). This paper presents two case studies of a deghosting, broadband processing workflow on conventionally acquired (single sensor, flat streamer) data from offshore West Africa.

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/content/papers/10.3997/2214-4609.20141690
2014-06-02
2024-04-18
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20141690
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