1887

Abstract

Summary

The development of geophysical methods for modeling the sources of gravitational and magnetic fields for large data sets makes it possible to move from studying the deep structure of the lithosphere along the DSS profiles to three-dimensional models. In this paper, the interpretation of the magnetic field on the basis of modern computer technologies was carried out, three-dimensional sources of anomalies were constructed and new results on the structure of the Earth’s crust of the northern part of the Southern Urals were obtained. These results make it possible to clarify the position of deep faults in the upper crust of the Southern Urals and their connection with deep hyperbasite belts protruding above the basaltic layer of the Earth’s crust.

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/content/papers/10.3997/2214-4609.201801859
2018-05-14
2024-04-27
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References

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