1887

Abstract

Within the scope of multi-technology interpretation projects in Mexico and the Gulf of Mexico, gravity, gravity gradient and magnetic data are jointly modelled and inverted. This iterative seismic and non-seismic interpretation process improves the geological depth model, focusing on salt features as main imaging problem zones. Analysing well logging data results in regionally valid, layer specific density-velocity relations which enable an independent gravity-based control of the seismic velocity model. This results in a final increase of seismic imaging quality.

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/content/papers/10.3997/2214-4609.20131251
2013-06-10
2021-10-16
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20131251
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