Coda Minerals Limited announced the results from field work at its the highly prospective Cameron River Project, located in the Mt Isa mineral province in North Queensland. Cameron River consists of 35km2 of copper and gold exploration tenure in the heart of the highly productive Mt Isa region, immediately north of the historic Mary Kathleen Uranium Mine. In March 2021 the Company entered into a binding Farm-in and Joint Venture Agreement giving it the right to acquire up to an 80% ownership in the Cameron River Project. Since entering into the project, Coda have carried out three rock chip sampling programmes over the most prospective areas, collecting a total of 696 samples, generally on 300m x 100m or 150m x 100m spacings at the most prospective areas across the two tenements. Of these, a total of 31 returned anomalous copper (> 0.1% Cu) and 16 returned anomalous gold (>0.1 g/t). The historical Copper Weed and Rebound prospects have been the focus of the majority of historical exploration on the tenure, and validation of historical rock chipping was one of the primary objectives of the programme. A total of 37 samples were taken in the area around these two prospects. The prospectivity for copper-gold mineralisation was confirmed, with several of the most highly mineralised samples collected from this area. Better samples from the area included R21CR0142 (12.6% Cu, 2.72g/t Au and 4.3g/t Ag), R21CR0143 9.2% Cu, 2.74g/t Au and 156.7g/t Ag) and R21CR0310 (22.9% Cu, 0.29g/t Au and 4.1g/t Ag). These programmes have expanded the scale of the Copper Weed-Rebound geochemical anomaly, which currently consists of a NNE aligned anomalous copper zone defined by modern and historical rock chips extending over at least 2,000m N/S and 800m E/W in the eastern half of the project, with potential to expand to the north. This zone is coincident with several fault splays which extend north from the regional scale Cameron Fault. Rock chips taken from traverses over this area have highlighted anomalous gold and copper associated with the faults with best results of 5.14% Cu (R21CR0285), and 0.15% Cu (R21CR0486). Another splay from the Cameron fault southeast of Rebound which defines the boundary between the Corella Formation and the Knapdale Quartzite was also tested, returning anomalous gold and copper (2.51g/t Au and 0.2% Cu in sample R21CR0074, 0.8% Cu in sample R21CR0092, and 0.4g/t Au in sample R21BTH0007). Several geophysical targets have been generated from historic VTEM and hyperspectral data collected over the Project, and two of the most prospective were selected for sampling. VTEM (Versatile Time Domain Electromagnetics) involves a transmitter that generates a current in the ground, this current flows most easily through conductive material, and a strong conductor will absorb and release more of the current than a weak conductor, this response is measured by the receiver. Hyperspectral imagery consists of satellite images taken over an area with sensors measuring a broad band of the electromagnetic spectrum, including visible light, infrared and ultraviolet. Different materials reflect and absorb differently at different wavelengths, As such, it is possible to differentiate among materials by their spectral reflectance signatures as observed in these remotely sensed images, whereas direct identification is usually not possible. Sampling over the VTEM anomaly (the "Scooby" prospect) in the centre of the Project returned anomalous rare earth values over a broad area 1000m x 600m oriented north-south over the central ridge of outcropping Corella Formation. Neither copper nor gold were anomalous in the immediate area, but anomalism was noted further south along the same trend, including R21MAC0003 (0.2% Cu, 0.5g/t Au) and R21CR0285 (5.1% Cu, 1.1g/t Ag) The Clear Waters prospect in the northeast of the Project was identified as an Allanite/Cuprite (REE/Cu) anomaly in hyperspectral imagery and is associated with a structural and geochemical trend extending southwest from the Six Kangaroos Uranium prospect. Rock chipping by Coda confirmed the presence of copper with malachite occurring on fracture surfaces, with best results from sample R21CR0550 of 12.1% Cu and 0.23g/t Au, and 0.26% La and 0.05% Ce in sample R21CR0578. The Wishbone prospect, located in the northwest of the project was also identified from hyperspectral imagery, and returned anomalous copper and gold grades with best results from sample R21CR0601 of 2.6% Cu and 0.15g/t Au, and 0.5% Cu in sample R21CR0578.