A primary goal is to improve understanding of the magmatic and hydrothermal processes that concentrate valuable elements, informing exploration strategies and mineral resource assessments. Their formation is commonly associated with extensional tectonic regimes and mantle processes, often coinciding with supercontinent breakup events like Rodinia. These carbonatites were linked to extensional regimes that created pathways for magma migration, often along crustal boundaries and zones of weakness. It confirms that the Aileron Province’s carbonatites formed during a dynamically extensional phase associated with the breakup of Rodinia, which created structural conduits for magma ascent and mineralization. Multi-method geochronology and isotope geochemistry of carbonatites in the Aileron Province, central Australia.