Abundance and distribution of gallium in some spinel and garnet lherzolites

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Abundance, Earth Mantle, Gallium, Garnets, Spinel, Earth Core, Meteoritic Composition, Neutron Activation Analysis

Scientific paper

The abundance and distribution of the moderately siderophile element gallium has been determined by radiochemical neutron activation analysis in spinel lherzolites from Mt. Porndon (Australia) and garnet lherzolites from Bultfontein (S. Africa). Minerals in the lherzolite concentrate Ga in the sequence olivine- orthopyroxene-clinopyroxene-garnet-spinel. Whole rock Ga abundances calculated from the modal mineralogy are equal to those actually determined, thus demonstrating that intergranular Ga-bearing phases are unimportant. Spinel lherzolites are richer in Ga than garnet lherzolites. Revised values for the Ga content of the mantle and garnet lherzolite-based pyrolite suggest that previous estimates are too high. The Ga content of the mantle may have been controlled by equilibrium core-mantle separation and does not require the presence of a meteoritic component.

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