Paleocurrents and depositional environments of deep water conglomerates in the Cambro-Ordovician Cap Enrag Formation, Quebec Appalachians

The Cap Enragé conglomerates are deep water, resedimented types associated with pebbly and massive sandstones. They resemble other deep water conglomerates in Quebec, especially those at Lévis-Lauzon, L'Islet Wharf, and Grosses Roches. All of these conglomerates were derived from a carbonate shelf to the northwest, and flow directions at Lévis and L'Islet are dominantly southward. By contrast, flow directions at Grosses Roches are to the west …