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The Clay Castles in the Hoarusib River valley are fine-grained deposits in a tributary immediately upstream of a narrow gorge. Sedimentological analysis reveals three lithofacies associations: (1) Channel Facies Association near the mouth of the tributary, (2) Back-Flow Facies Association in the middle section, and (3) Silt and Massive Sand Facies Association in the head of the tributary. Overall...
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