1 resultado para 174-1071I
em Brock University, Canada
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Resumo:
Brown sediment with two different domains; one coarse grained, and one finer grained. In the coarse grained domain, clasts range from small to large in size. The clast shape ranges from sub-angular to rounded. Rotation structures and edge-to-edge grain crushing is commonly seen. In the finer grained domain, clasts are mainly small, with a few larger clasts, and there is an abundance of lineations.