Fission 3.0 Drilling Intersects Encouraging Clay-Altered Fault Zone at Hearty Bay

Kelowna, British Columbia--(Newsfile Corp. - April 25, 2022) - FISSION 3.0 CORP (TSXV: FUU) (OTCQB: FISOF) ("Fission 3" or "the Company") is pleased to report that drilling and ground geophysics at the Hearty Bay project in the Saskatchewan Athabasca region, in the main up-ice direction from the historic high-grade uranium boulder trains on Isle Brochet, has intersected a hydrothermally clay-altered fault zone in hole HB-22-008 at the SW end of a new conductor. This is encouraging as uranium mineralization in the Athabasca basin is often found in proximity to clay-altered and conductive fault zones and this new conductor is a promising target for future drilling.

Highlights of the drilling and geophysics program are as follows:

  • 14 drill holes completed for 1,304 metres of diamond drilling

  • 77 line-kms of ground EM geophysics completed

  • Hole HB22-005 and HB22-008 intersected a 3m zone and an 11.5m zone respectively of brecciated and faulted basement rock that displayed strong hydrothermal clay alteration, features often associated with uranium mineralization in the Athabasca Basin.

  • Hole HB22-008 intersected a significant fault with encouraging alteration furthest to the NE from the high-grade uranium boulder trains on Isle Brochet in the main up-ice direction, supporting that future drilling to locate the source should continue in this direction.

  • The ground EM survey has identified new basement conductors to the NE of Isle Brochet that coincide with interpreted faults from the 2019 marine seismic survey. Drill hole HB22-008 is located at the SW end of these 2km-long subparallel conductors, suggesting an association with the intersected hydrothermally altered fault and providing follow up targets for future drilling along these new conductors.

  • 429 drill core samples have been submitted to SRC Geoanalytical Laboratories in Saskatoon for geochemical analysis. The geochemical results will be used to try to vector in towards the source of the high-grade uranium boulder trains and refine future drill targets.

The objective of the drill program was to test interpreted structural features and sandstone outliers based on the 2019 marine seismic survey in the main up-ice direction from the historic high-grade uranium boulder trains on Isle Brochet and beyond the known edge of the Athabasca Basin. While no sandstone outliers were identified, holes HB22-005 and HB22-008 intersected a 3m zone and an 11.5m zone respectively of brecciated and faulted basement rocks with hydrothermal clay alteration. The significant fault zone from 74.5m to 86m in hole HB22-008 is comprised of a 1.6m clay-supported cataclasite breccia immediately followed by clay, quartz and calcite occurring in fractures and smaller scale faults. This is encouraging as uranium mineralization in the Athabasca Basin is often found in proximity to hydrothermal clay-altered fault zones.