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Abstract

Summary

We present a new 1D inversion algorithm for potential field data, which consists in the inversion of vertical soundings of data at different altitudes. The inversion of multiple 1D vertical gravity/magnetic soundings is made over the same source-volume, which is a finite volume of layers of different densities, for interpreting anomalies along a profile or over a measurement surface. The inversion algorithm was tested on synthetic data and on a real case, relative to gravity data referred to a sedimentary basin in Nevada, USA.

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/content/papers/10.3997/2214-4609.201601300
2016-05-31
2020-04-09
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References

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