Unconformity-associated uranium deposits of the Athabasca Basin, Saskatchewan and Alberta

@inproceedings{Jefferson2007UnconformityassociatedUD,
  title={Unconformity-associated uranium deposits of the Athabasca Basin, Saskatchewan and Alberta},
  author={Chief Justice Wallace Jefferson and D. J. Thomas and Sunil S. Gandhi and Paul Ramaekers and Gary D. Delaney and Dan Brisbin and Christopher J. Cutts and P. Portella and R. A. Olson},
  year={2007}
}
This review of the geology, geophysics, and origin of the unconformity-associated uranium deposit type is focused on the Athabasca Basin. Pods, veins, and semimassive replacements of uraninite (var. pitchblende) are located close to unconformities between late Paleoto Mesoproterozoic conglomeratic sandstone basins and metamorphosed basement rocks. The thin, overall flat-lying, and apparently unmetamorphosed but pervasively altered, mainly fluvial strata include red to pale tan quartzose… 
Empirical Models for Canadian Unconformity-Associated Uranium Deposits
  • Geology
  • 2007
This review of the geology and geochemical-geophysical attributes of the unconformity-associated uranium (U) deposit type is based mainly on deposits in the Athabasca Basin. Pods, veins, and
Regional Setting, Geology, and Paragenesis of the Centennial Unconformity-Related Uranium Deposit, Athabasca Basin, Saskatchewan, Canada
The Centennial unconformity-related uranium deposit represents the first significant uranium mineralization along the Snowbird tectonic zone in the south-central part of the Athabasca Basin. The
Geology, alteration system, and uranium metallogenic potential of Pasha-Ladoga Basin, Russia
The Mesoproterozoic Pasha-Ladoga Basin is located at the margin of the Karelian Craton and Svecofennian Belt in northwest Russia. It is the only basin in Russia that is currently recognized to host
Magmatic and Metamorphic Uraninite Mineralization in the Western Margin of the Trans-Hudson Orogen (Saskatchewan, Canada): A Uranium Source for Unconformity-Related Uranium Deposits?
The genetic model for the giant unconformity-related uranium deposits of the Athabasca Basin is still being debated, with one of the main issues being the source of the uranium concentrated by
Formation and Evolution of the Centennial Unconformity-Related Uranium Deposit in the South-Central Athabasca Basin, Canada
The Centennial U deposit is situated in the south-central Athabasca Basin (Canada) and straddles the unconformity between early Paleoproterozoic to Archean metasedimentary and metavolcanic rocks and
ydrogeology , sequence stratigraphy and diagenesis in the Paleoproterozoic estern Thelon Basin : Influences on unconformity-related uranium ineralization
The Paleoproterozoic (Statherian) Thelon Formation consists of unmetamorphosed sandstone and conglomerate that was deposited in the Thelon Basin, a continental basin in northern Canada. This study
Hydrothermal activity in the basement granite associated with the unconformity-related uranium deposit in Chitrial area, Cuddapah Basin, India
Uranium mineralization occurs adjacent to the unconformity between Paleoproterozoic granite and Meso- to Neoproterozoic cover sediments in Chitrial prospect of Cuddapah Basin in Indian shield.
Geochemical footprint of the Millennium unconformity-type uranium deposit, Canada: implications for vectoring new targets
The Millennium deposit, a c. 650-m deep monomineralic uranium deposit, is located in the southeastern Athabasca Basin, Saskatchewan, a region containing numerous high-grade unconformity-type U
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References

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On the genesis of Rabbit Lake and other unconformity-type uranium deposits in northern Saskatchewan, Canada
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Significance of Alteration Assemblages for the Origin and Evolution of the Proterozoic Nabarlek Unconformity-Related Uranium Deposit, Northern Territory, Australia
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