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The mineralization is hosted by flysch rocks (of Triassic age) cut by dikes.
The thickness of the shallow marine formations is up to 150 m, and the bathyal flysch is up to 4 km thick.
Synorogenic flysch deposits were laid down in front of the advancing allochthonous complexes, and were overridden by them.
He interpreted pre-Easdale Subgroup rocks as flysch and subsequent molasse derived from a Knoydartian orogen.
There, the most widespread Ordovician flysch is the Garin Formation.
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