1887

Abstract

The use of gravity data to estimate parameters and to determine near-surface static corrections is becoming more popular. Of particular importance is the application of this method at the Siberian platform, where amplitudes of the structures are small, and the influence of strong near-surface inhomogeneities greatly distorts the wave pattern. We offer a technology of co-processing and interpretation of seismic and gravity data. The technology is based on the adaptive methods for inverse problems of gravimetry and magnetometry, implemented in packages ADG-3D and the ADM-3D, as well as existing seismic data processing packages

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/content/papers/10.3997/2214-4609.20143125
2012-09-10
2021-10-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20143125
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