Petrogenesis and evolution of an early Proterozoic collisional orogenic belt: The granulite belt of Lapland and the Belomorides (Fennoscandia)

Pierre Barbey, J. Convert, B. Moreau, R. Capdevila, Jean Hameurt

Bulletin of the Geological Society of Finland · 1984 · 78 citations · 34 references

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Abstract

The tectonic and metamorphic pattern of the Precambrian crust exposed in the eastern Baltic Shield is characterized by two adjacent high-grade belts (Tana and Granulite belts) located between the Archean Inari-Kola craton to the east and the South Lapland-Karelia craton to the west.

References

34