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The Cooper and Eromanga Basins of South Australia and Queensland are the largest onshore hydrocarbon 9 producing region in Australia. Igneous rocks have been documented infrequently within end of well reports 10 over the past 34 years, with a late Triassic to Jurassic age determined from well data. However, the areal 11 extent and nature of these basaltic rocks were largely unclear. Here, we integrate seismic, well, gravity, and 12 magnetic data to clarify the extent and character of igneous rocks preserved within Eromanga Basin 13 stratigraphy overlying the Nappamerri Trough of the Cooper Basin. We recognise mafic monogenetic 14 volcanoes that extend into tabular basalt lava flows, igneous intrusions and, more locally, hydrothermally 15 altered compound lava flows. The volcanic province covers ~7500 km 2 and is proposed to have been active 16 between ~180-160 Ma. We term this Jurassic volcanic province the Warnie Volcanic Province (WVP) after the 17 Warnie East 1 exploration well, drilled in 1985. The distribution of extrusive and intrusive igneous rocks is 18 primarily controlled by basement structure, with extrusive and intrusive igneous rocks elongate in a NW-SE 19 direction. Finally, we detail how the WVP fits into the record of Jurassic volcanism in eastern Australia. The 20 WVP is interpreted as a product of extension and intraplate convective upwelling above the subducting Pacific 21 Slab. The discovery of the WVP raises the possibility of other, yet unidentified, volcanic provinces worldwide.