“…Overlying Palaeoproterozoic basement of the North Australian Craton, the McArthur Basin is an unmetamorphosed and largely undeformed sequence of sedimentary and volcanic rocks deposited over a period of more than 500 million years (e.g., Ahmad & Munson, 2013;Rawlings, 1999;. Intriguingly, the basin hosts considerable hydrocarbon reserves derived from Mesoproterozoic source rocks, which have been preserved to the present day (Cox et al, 2016(Cox et al, , 2022Jackson et al, 1986). While extensive research has been undertaken characterising the hydrocarbon source, chemistry and maturity (e.g., Cox et al, 2022;Crick et al, 1988;George et al, 1994;Jackson & Raiswell, 1991;Lanigan et al, 1994;Summons et al, 1988), the timing of hydrocarbon maturation remains poorly resolved.…”