Tectonostratigraphic position of the Finnish Caledonides at the Fennoscandian margin of the northern Scandes
The Finnish Caledonides consist of the lower structural units characteristic of much of the northern Scandes, whose foreland is now known to be Archaean throughout its extension in Finland. The autochthonous Dividal sedimentary rocks pass very gradually into the somewhat overthrust Jerta rocks. Thes...
Published in: | Bulletin of the Geological Society of Finland |
---|---|
Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Geological Society of Finland
1989
|
Subjects: | |
Online Access: | https://doi.org/10.17741/bgsf/61.2.004 https://doaj.org/article/4304dca2c7f34fd7863851b669e8c87a |