1887

Abstract

The opportunity of direct interpretation of 2D potential fields at the deep research on an example of the European part of Russia is established and demonstrated. The information on density inhomogeneity of the upper mantle up to 210 km using Bouguer anomaly only is obtained. The main difficulty is correct (reliable) choice of initial parameters of an interpreted function. Modes of outcomes estimation are analysed.

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/content/papers/10.3997/2214-4609-pdb.20.P151
2006-10-16
2020-08-15
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.20.P151
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