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Clean basal and capping argillaceous sandstone couplets in deep water settings have been previously interpreted as the result of spatially segregated turbidity currents and debris flows or spatio‐temporal transitioning of a turbulent flow to a transitional/laminar state. However, this paper presents three‐dimensional laboratory experiments demonstrating that a single sediment‐gravity flow can develop...
Deep‐lacustrine deposits provide records of palaeoclimate and tectonics, and often host major hydrocarbon reservoirs, but their facies description and long‐term stratigraphic architecture are not sufficiently reported. A combined outcrop and three‐dimensional seismic dataset in the western Dacian Basin of Romania is used to decipher depositional systems, basin‐fill architecture and clastic sediment...
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