The structure of three-dimensional convection beneath oceanic spreading centres
The combined effects of buoyancy forces due to thermal expansion and compositional gradients in the mantle beneath spreading centers have been investigated in a series of numerical experiments. Compositional buoyancy leads to three-dimensional flow beneath the spreading axis, with along-axis variations in upwelling and melt production. Thermal buoyancy drives upwelling beneath the axis and convective overturn, which forms rolls aligned perpendicular to the spreading axis. The distance from the axis at which these rolls form is controlled by the spreading rate, mantle viscosity, and relative strength of compositional buoyancy. Implications of the results for the spreading center structure are examined.