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Identification of a boulder pavement intercalated between two diamictites of the "Lutoe Series" in Angola points out for a glacial origin for these rocks. Measurement of striae on clasts, their disposition in the pavement and the fabric of diamictites indicate movement of Late Paleozoic (Gondwana) glaciers towards NW in this part of the Congo Basin.

Direction of movement of late paleozoic glaciers in Angola (Western Africa)