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...

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Bibliographic Details
Main Authors: F Stodt, A H N Rice, L Bjö Rklund, G Bax, G P Halverson, T C Pharaoh
Other Authors: The Pennsylvania State University CiteSeerX Archives
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