Rabbit Lake deposit, Saskatchewan

Rabbit Lake, northern Saskatchewan, Canada The Rabbit Lake occurrence in northern Saskatchewan is an example of a monometallic unconformity-related uranium deposit. [Pg.134]

Unconformity-Related Deposits. Deposits of the unconformity-related type occur spatially close to significant unconformities. These deposits usually developed during the period about 1800—800 million years ago in intracratonic basins. Deposits also developed during Phanerozoic time. Examples of unconformity-related deposits include the ore bodies at Cluff Lake, Key Lake, and Rabbit Lake in northern Saskatchewan, Canada, and those in the Alligator Rivers area in northern AustraHa (12). [Pg.184]

Hoeve, J. SiBBALD, T.I.I. 1978. On the genesis of Rabbit Lake and other unconformity-type uranium deposits northern Saskatchewan, Canada. Economic Geology, 73, 1451-1473. [Pg.456]

Saskatchewan Rabbit Lake Ore deposits and mining wastes Pichler, Hendry and Hall (2001)... [Pg.511]

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