HE-4/HE-3 DISPERSION AND MANTLE CONVECTION

Histograms of the He-4/He-3 ratios analysed in MORB glasses from individual ridge segments show a linar correlation between the ridge spreading rate and the standard deviation of the corresponding averaged He-4/He-3 ratio. We interpret the form of these histograms in terms of stirring time ((tau)stir) of the upper mantle. This stirring time corresponds to the time that perturbations brought in from outside into the upper mantle, in the form of oceanic island source material or slabs, were attenuated by a factor of l/e through the effect of convection. Using He-4/He-3 ratios of oceanic basalts, we calculate a stirring time close to 250 Ma, distinct from the residence time of similar to 1 Ga. This may indicate the existence of two scale upper mantle convection, rapid convection being responsible for the homogenisation of helium in the upper mantle, and the consequent uniformity of the He-4/He-3 ratio, and slower convection being responsible for mantle outgassing and plate tectonic motion.