Chapter 58 Evidence of late Neoproterozoic glaciation in the Caledonides of NW Scandinavia
Abstract: The northwestern part of the Scandinavian Caledonides, formed by SE-to ESE-directed thrusting through the Neoproterozoic W. Baltica continental shelf, contains numerous small and often isolated outcrops of diamictite and associated strata. No precise biostratigraphic or isotopic data are a...
Main Authors: | , , , , , |
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1047.9989 http://rockspace.se/publ/2011_Paper_Stodt_etal_NWNorway_GeolSoc_Mem.pdf |