Abstract

Large-scale experiments on non-channelized turbidity currents show that a wide flow opening angle forms and a rapid dilution of the current with distance takes place. The thickness of the deposit decreases radially away from the source, resulting in tongue-shaped isopachs. The mean grain diameter also decreases with distance while the sorting improves. With increasing distance, the following succession of bedforms was observed: (Non-deposition) → parallel lamination → ripples → parallel lamination. This corresponds to the B, C and D division of the Bouma sequence for turbidites. The experiments are in good agreement with the models presented by Bouma, Mutti and Ricci Lucchi, and Walker for classical turbidites in the depositional lobes of submarine fans.

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