{"type":"rich","version":"1.0","provider_name":"Transistor","provider_url":"https://transistor.fm","author_name":"Company Interviews","title":"F3 Uranium (TSXV:FUU) Advances Tetra Zone Discovery with $20 Million Financing","html":"","width":"100%","height":180,"duration":1857,"description":"Interview with Sam Hartmann, VP Exploration, and Dev Randhawa, Chairman & CEO, of F3 Uranium Corp.\nOur previous interview: https://www.cruxinvestor.com/posts/f3-uranium-tsxvfuu-billion-dollar-discovery-team-strikes-again-in-worlds-best-uranium-district-7874\nRecording date: 27th November 2025\nF3 Uranium Corp. (TSXV: FUU) has completed a $20 million financing to fund a year-long drilling campaign at its Tetra Zone discovery in Saskatchewan's Athabasca Basin. The financing, which included $15 million in flow-through funds, brings the company's treasury to $30 million and eliminates near-term dilution pressure as the exploration program advances.\nCEO Dev Randhawa explained the strategic shift toward Tetra Zone, which has emerged as the company's primary focus after the JR Zone failed to grow as anticipated. Despite JR's promising initial indicators, including peak grades of 4.5 meters at 50% uranium along a large conductor, the system has not delivered the expansion investors expected. Tetra Zone, by contrast, shows significantly greater potential with 60 meters of mineralization-three times what JR produced-sits just 12 kilometers from the Arrow and Triple R deposits along an apparent productive geological trend.\nRecent drilling results support management's confidence in the discovery. The most recent hole intersected mineralization in a 15-meter step-out, with scintillometer readings exceeding 10,000 counts per second across 30+ meters. Chief Geologist Sam Hartmann estimates a 2.3-meter high-grade interval \"will be well over a percent\" when laboratory assays are returned. This successful step-out confirms both continuity and the geological model's predictive capability.\nThe technical understanding of Tetra has evolved considerably from initial interpretations. Unlike typical Athabasca deposits controlled by graphitic conductors, Tetra appears to be shear-zone-controlled, with mineralization in micaceous structures that generate weaker geophysical signatures. This...","thumbnail_url":"https://img.transistorcdn.com/1wv-MFlQAgnm-ca64e5kK4984dZB0os8-HJdRVsI74M/rs:fill:0:0:1/w:400/h:400/q:60/mb:500000/aHR0cHM6Ly9pbWct/dXBsb2FkLXByb2R1/Y3Rpb24udHJhbnNp/c3Rvci5mbS9zaG93/LzEzNTcyLzE2MjM5/NTQyMDctYXJ0d29y/ay5qcGc.webp","thumbnail_width":300,"thumbnail_height":300}