Exploration was undertaken for possible stratabound uranium occurrences formed within the Jurassic Algebuckina Sandstone or the overlying Cretaceous Cadna-owie Formation, over an area lying near the north-western margin of the Mesoproterozoic-Adelaidean Peake and Denison Inliers. The types of occurrence sought were sandstone-hosted roll-front deposits and palaeodrainage controlled sandstone and conglomerate-hosted deposits. The only work undertaken comprised a review of available exploration records, including historic drillhole data. From this it was concluded that the area's sedimentary uranium potential is limited.