Fig. 5: Compositional comparisons within the Yilgarn leucogranites and between them and sanukitoids.

a Variation in Nd-isotopic composition (ɛ_{Nd (2.65Ga)}) with SiO₂ for leucogranites and sanukitoids; b Variation in zircon saturation temperature with zircon crystallisation age for leucogranites and sanukitoids.