The Creelman-Roberts Uranium Property is located about 50 km
north of Sudbury, Ontario. Past surface sampling, trenching, and shaft
sinking between 1959 and 1972 revealed uranium mineralization in the
Mississagi Formation which is the similar sedimentary formation that
hosts uranium mineralization in the Elliot Lake Uranium Camp, located
125 km to the southwest.
The Rupert River Uranium property is underlain by major north-east-southwest trending package of gneisses and granitoids, including pegmatites, historically known for their anomalous radioactive content, numerous circular and planar faults and structural features, according to a Quebec government survey. This style of mineralization model is not too different from that of the uranium vein mineralization of the French Massif, France, Bancroft, Ontario and Crackingstone Peninsula, Saskatchewan (Gunnar-type mineralization). In addition, the Rossing Deposit in Namibia is ssociated to gneisses and granites crosscut by faults and pegmatites.
The Cosby Gold property, IKI’s latest property acquisition, is located 60km east – northeast of Timmins, Ontario.
The property is comprised of 45 claim units in Walker Township, Ontario and consists of felsic, mafic and ultramafic volcanic units within the Kidd-Munro Assemblage. Previous work by AMAX, Falconbridge and Cosby includes magnetometer, VLFEM, HLEM, geology and geochemical surveys and five diamond drill holes.