4/2/2023 0 Comments Fission uranium corp finances![]() ![]() This conductive zone was further refined by a ground EM survey in 2012 and named the "A1 conductor" tight spaced follow-up ground EM and IP resistivity surveys were conducted in early 2022 to create a more constrained EM plate model. Originally, an airborne EM conductor was identified in the area by Fission Energy, a predecessor to F3 Uranium, in 2008. The company is also pleased to provide a brief technical note to provide some additional context to the drill results reported thus far. * Hand-held Spectrometer Results On Mineralized Drillcore (>300 cps / >0.5m minimum) Drill Hole Summary and Handheld Spectrometer Results Collar Information To view an enhanced version of this graphic, please visit: for lithogeochemical analysis using their "Uranium Package".Īll depth measurements reported are down-hole and true thickness are yet to be determined but the Company estimates true thickness of the reported intervals in this news release to be close to reported interval widths. One half of the split sample will be submitted to SRC Geoanalytical Laboratories (an SCC ISO/IEC 17025: 2005 Accredited Facility) in Saskatoon, SK. Samples from the drill core are split in half on site and are standardized at 0.5m lengths. All depth measurements reported are down-hole and true thickness are yet to be determined. The reader is cautioned that scintillometer readings are not directly or uniformly related to uranium grades of the rock sample measured and should be used only as a preliminary indication of the presence of radioactive materials. The Company considers greater than 300 cps on the handheld spectrometer as anomalous, >10,000 cps as high grade and greater than 65,535 cps as off-scale. Natural gamma radiation in the drill core that is reported in this news release was measured in counts per second (cps) using a handheld Radiation Solutions RS-125 scintillometer.
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