Structural evolution of the Vuotso area, Finnish Lapland
The Vuotso area is structurally interesting because the fold interference pattern in rocks of central Lapland changes into thrust-related foliation of the Lapland Granulite Belt. A felsic volcanic rock yielded a 2.45 Ga age and conformed that the volcanic rocks in the Vuotso area are (mainly) Paleop...
Main Authors: | M. Nironen, I. Mänttäri |
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Format: | Article |
Language: | English |
Published: |
Geological Society of Finland
2003-12-01
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Series: | Bulletin of the Geological Society of Finland |
Subjects: | |
Online Access: | http://www.geologinenseura.fi/bulletin/Volume75/NironenManttari.pdf |
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