Figure 1: A calcite-carbonatite from Oka complex, Deux-Montagnes RCM, Laurentides, Québec, Canada. (source: mindat.org) | Samso Insights

The Splinter Rock clay-hosted REE prospect, located northeast of Esperance within the east Albany–Fraser Orogen in Western Australia, has emerged as one of the most scientifically compelling regolith-hosted REE systems in the country (Figure 1). A multidisciplinary study led by CSIRO has produced the first integrated geological, geophysical, mineralogical, and geochemical characterisation of this emerging clay-hosted REE district.

As the global energy transition accelerates, demand for base metals like copper (Cu), lead (Pb), zinc (Zn), and nickel (Ni) is booming. Yet, exploration success rates for major discoveries are shrinking worldwide. In Australia—home to an array of world-class resources—the biggest challenge isn’t finding the right rocks, it’s working out where to start looking beneath the post-mineralisation cover that hides up to 80% of the continent’s prospective geology.

Carbonatites are some of the rarest igneous rocks on the planet, comprising less than 1% of all identified igneous systems. Despite their rarity, they are highly significant in geology and resource economics.

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