Early Cambrian and Late Precambrian Paleocurrents, Banff and Jasper National Parks
ABSTRACT Foreset beds in the upper part of the Late Precambrian Miette group and in the lower and upper parts of the Lower Cambrian Gog group were deposited by paleocurrents flowing mainly westward and southwestward. The source area of the sediments was therefore the Precambrian of the continental craton.