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Figure 1 | Flow driven by buoyancy and osmotic sources in saturated porous sediment under the seafloor. (a) An extended buoyancy source in a homogeneous sediment, (b) a two-dimensional buoyancy source at a continental margin, (c) a buoyant or osmotic pumping mechanism associated with a developed seep, (d) buoyant or osmotic pumping in a fully developed mud volcano.

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