Depositional environment and apparent age of the Fauske carbonate conglomerate, North Norwegian Caledonides.
The Fauske conglomerate represents a rather rare case of a monomict carbonate conglomerate in the Late Neoproterozoic to Silurian, lithostratigraphic successions of the Norwegian Caledonides. Lithological varieties of this conglomerate unit from the Løvgavlen quarry have a highly decorative quality...
Main Authors: | , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2000
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Subjects: | |
Online Access: | https://hdl.handle.net/11250/2674210 |