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Abstract

Summary

The deep crustal structure of the White Sea region and the surrounding areas has been well described in the framework of individual case studies. There are also a number of models for the geological structure available. We propose a uniform assessment of magnetic sourcies responsible for the long wavelength magnetic features. Within the considered area, the Precambrian formations of the Fennoscandian Shield and the Russian Plate overlain by a sedimentary cover are represented. Large geological domains are separated by regional faults and suture zones. The study is based on a 1: 1,000,000 scale aeromagnetic field map.

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/content/papers/10.3997/2214-4609.20215521153
2021-05-11
2024-04-28
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