Fission 3.0 Uses PLS Template to Stake New Claims with Shallow-Depth Potential in Athabasca Basin

KELOWNA, BRITISH COLUMBIA--(Marketwired - Mar 13, 2014) - FISSION 3.0 CORP. (TSX VENTURE:FUU) ("Fission3" or "the Company") is pleased to announce the addition of three new properties and the expansion of its Manitou Lake property, staked by the same award-winning technical team of both Fission3 and Fission Uranium Corp. (Fission), in the Athabasca Basin, Canada. The newly acquired properties are referred to as Perron Lake, Cree Bay and Grey Island. The new acquisitions are part of Fission's objective to stake highly prospective areas where the target depth of uranium mineralization is expected to be shallow, as is the case with Fission Uranium Corp's PLS property.

The new ground, which consists of nine claims on four properties for a total of 41,938.758 ha, was staked late 2013 to early 2014.

Fission3 now has a portfolio of nine properties in and around the Athabasca Basin (in both Saskatchewan and Alberta) and a property in the Macusani uranium district of south-central Peru. Fission's Athabasca Basin properties are all close to the margin of the Basin and thus the mineralization model is shallow depth.

In addition, Fission3 retains the patent-pending airborne survey invention entitled "System And Method For Aerial Surveying Or Mapping Of Radioactive Deposits". The invention was instrumental in Fission's high-grade uranium boulder field discovery. It relates to an airborne system and method for surveying a geographic area to detect and map the locations of radioactive geological deposits, such as boulders and clusters of rock.

Ross McElroy, COO, and Chief Geologist for Fission, commented,

"There remain many underexplored areas of the Athabasca Basin. These new claims represent highly prospective additions to our growing portfolio of high quality and shallow target depth properties."

Perron Lake

  • Four contiguous claims totaling 20,826.05ha, located approximately 20km north of the Athabasca Basin. The property lies along the ENE - WSW trending Grease River shear zone, which is a major basin scale tectonic zone.

  • Regional historic results of lake sediment sampling taken and compiled by SMDC (1980) in the Tait Lake and North Tait Lake area, show strong uranium anomalies in sediment (>100ppm U) over an area of 30 km2, of which ~75% of this area is within Fission3's claims. This sizeable anomalous area indicates an elevated regional uranium district and a favorable environment for hydrothermal and structure related concentration of uranium in basement rocks such as in both the western and eastern Athabasca Basin occurrences (PLS, Eagle Point, Roughrider).

  • Anomalous samples in outcrop are present in the area, including the 'Bradley' occurrence discovered by CanAlaska in 2007, where assays up to 3.53% U3O8 mineralized as pitchblende veins in a 3m wide shear, that is 800m from the southwest property boundary, and is spatially associated with the Grease River Shear Zone.