Fig. 7From: Thickening-upward cycles in deep-marine and deep-lacustrine turbidite lobes: examples from the Clare Basin and the Ordos BasinSimulation diagram of the laboratory experiment conducted by Hoyal et al. (2003). a Deposits showing three zones dominated by processes of bypass, bed load, and suspension; b Across-stream deposit shape, showing less erosional features downflowBack to article page