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Abstract

Where subsurface structure is complex, reflection data from land seismic surveys often suffer triply - from statics variations, the presence of various types of noise, and imperfect moveout correction due to crossing events and rapidly varying non-hyperbolic moveout.

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/content/papers/10.3997/2214-4609.201409401
1995-05-29
2024-04-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409401
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