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...

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Bibliographic Details
Main Authors: Heldal, Tom, Fallick, Anthony E., Gorokhov, Igor M., Roberts, David, Melezhik, Victor A.
Format: Article in Journal/Newspaper
Language:English
Published: 2000
Subjects:
Online Access:https://hdl.handle.net/11250/2674210