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Numerical modelling of mud volcanoes and their £ows using constraints from the Gulf of Cadiz

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Fig. 1. Schematic location and bathymetry chart (contours at 1000-m intervals) of the study area in the Gulf of Cadiz, easternNorth Atlantic.
Fig. 3. Schematic ¢gure showing the main elements of the isostatic model, comprising the columns of mud breccia, the mud vol-cano conduit, and a two-layered sediment column model, in which:kg mcompensation (i.e
Fig. 4. Compilation of clastic sediment densities from ODP holes in accretionary complexes including the Barbados ForearcWedge (see references in text)
Fig. 5. Schematic cross-section (not to scale) showing ele-ments of a vertically stacked model of mud volcano forma-tion, with a central conduit of constant diameter, in whichthe thickness and radius of superimposed, cylindrical mud£ows both decrease with increasing volcano height.
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