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Reconstructions of ancient delta systems rely typically on a two‐dimensional (2D) view of prograding clinothems but may miss their three‐dimensional (3D) stratigraphic complexity which can, instead, be best documented on modern delta systems by integrating high‐resolution geophysical data, historical cartography, core data and geomorphological reconstructions offshore. We quantitatively compare three...
Lacustrine basins and their deposits are good paleoclimate recorders and contain rich energy resources. Shelf‐margin clinoforms do exist in deep lacustrine basins, but with striking differences from those in deep marine basins, caused by a correlation between the river‐derived sediment supply and the lake level. This study uses empirical relationships to calculate the water and sediment discharge...
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