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Abstract

In areas with complex near surface and topographic variations, field statics do not generally fix all delays within the seismic traces. The complexities in the study area include large variations between areas of hard rock to areas covered by sheeted sands and sand dunes.

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/content/papers/10.3997/2214-4609-pdb.287.1186982
2012-03-04
2021-10-16
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.287.1186982
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