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F3 Uranium Corp V.FUU

Alternate Symbol(s):  FUUFF

F3 Uranium Corp. is a uranium exploration company. The Company is advancing its newly discovered high-grade JR Zone and exploring additional mineralized zones on its 100%-owned Patterson Lake North (PLN) Project in the southwest Athabasca Basin. PLN is accessed by Provincial Highway 955, which transects the property, and the new JR Zone discovery is located over 25 kilometers (km) northwest of Fission Uranium’s Triple R and NexGen Energy’s Arrow high-grade uranium deposits. The PLN project comprises the PLN, Minto and Broach properties. The PLN property is located near the south-western edge of the Athabasca Basin. The PLN project consists of two mineral claims covering a total of 4,074 hectares. The Minto Property is located directly north of the JR zone discovery and 28km south of the Shea Creek deposit. The Broach property is located five km south of the JR zone and 22km north of Fission Uranium Triple R deposit. The property sits along the estimated Athabasca basin boundary.


TSXV:FUU - Post by User

Post by Banner60on Jul 05, 2023 12:30pm
140 Views
Post# 35527492

F3 - Red Cloud Report

F3 - Red Cloud ReportF3 Uranium Corp. (TSXV:FUU)
 
JR Zone Extended by 50% to 156m Strike Length
 

Impact: Positive
 
Scintillometer results were reported from the initial eight holes of F3 Uranium’s 30-hole summer drill program at the JR zone on its 100%-owned PLN project in the SW Athabasca Basin. Step out drilling on lines 105S and 135S extended the mineralized strike by ~50% to 156m. Drilling at line 60S encountered sections of strong radioactivity up-dip, suggesting the presence of high-grade mineralization as drilling moves towards unconformity. Assays from all holes remain pending. While extension of the JR zone is a positive, results along the southern extension are not as strong as previous results. That said, the thickness of the zone core remains robust. This still would have acted as a major fluid flow conduit and allowed considerable hydrothermal mineralizing fluids to pass through the structure. Athabasca Basin deposits, whether basement hosted or unconformity, often occur as discontinuous zones or “pearls on a necklace”. We believe mineralization could pick up to the south or peter out altogether followed by a new zone emerging further to the south. This style of mineralization creating separate zones is evident at other nearby deposits including Shea Creek, Triple R, and the Arrow-Bow-Harpoon-Spitfire deposit. We still see potential along trend to the south and believe that further drilling along trend, and up-dip, is warranted to keep extending the zone.
 

 

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