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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Published in: | Moscow University geology bulletin Vol. 71; no. 5; pp. 311 - 322 |
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Main Authors: | , , , , , , |
Format: | Journal Article |
Language: | English |
Published: |
New York
Allerton Press
01-09-2016
Springer Nature B.V |
Subjects: | |
Online Access: | Get full text |
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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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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0145-8752 1934-8436 |
DOI: | 10.3103/S0145875216050082 |