The Paleoproterozoic remagnetization trend in rocks of the Belomorian mobile belt: Paleomagnetic and geologic evidence

As a resulting of comprehensive studies of Paleoproterozoic igneous complexes a regular remagnetization trend is revealed. It is shown that the remagnetization front propagated from the northwest to southeast. The obtained remagnetization trend probably reflects the direction of the collision in the...

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Bibliographic Details
Published in:Moscow University geology bulletin Vol. 71; no. 5; pp. 311 - 322
Main Authors: Lubnina, N. V., Slabunov, A. I., Stepanova, A. V., Bubnov, A. Yu, Kosevich, N. I., Novikova, M. A., Tarasov, N. A.
Format: Journal Article
Language:English
Published: New York Allerton Press 01-09-2016
Springer Nature B.V
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Summary:As a resulting of comprehensive studies of Paleoproterozoic igneous complexes a regular remagnetization trend is revealed. It is shown that the remagnetization front propagated from the northwest to southeast. The obtained remagnetization trend probably reflects the direction of the collision in the Paleoproterozoic. Correlation between remagnetization processes and rock compositions was found. The degree of conservation of secondary earlier and later magnetization components is likely associated to both the compositions of protoliths and different transformation conditions of rocks, including their fluid saturation.
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ISSN:0145-8752
1934-8436
DOI:10.3103/S0145875216050082