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Hyperpycnal currents are river‐derived turbidity currents capable of transporting significant volumes of sediment from the shoreline onto the shelf and potentially further to deep ocean basins. However, their capacity to deposit sand bodies on the continental shelf is poorly understood. Shelf hyperpycnites remain an overlooked depositional element in source to sink systems, primarily due to their...
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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