1887

Abstract

Sometimes seismic processing, when used separately, will not yield a correct silution of a seismostratigraphic problem due to the lack of information and instability of the computational procedures. The joint data inversion implementing a few methods (seismic and gravity, for example) can result in a correct solution.

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/content/papers/10.3997/2214-4609.201410711
1992-06-01
2020-10-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410711
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