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gases, and (5) diamonds sometimes have suffered little interplay with crust or environment, owing to their great crystallization depths and extremely rapid emplacement to shallow crustal levels in kimberlite and lamproite pipes. However, just about all these data are from samples which can be successfully of zero-age, and due to this fact, they only give details about the current composition of mantle noble gases. New SHRIMP U-Pb ages from a number of tuffaceous sediments instantly above the calcareous and gossanous, base-metallic enriched Bimba Formation in the Olary Area are remarkably consistent on a regional scale.These zircons are relatively homogeneous in composition: they have Th/U ratios < 0.09, are typically depleted

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