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Grant: Collaborative Research and Development Grants

University of Regina

$62,900.00

Thermal - hydrolic - mechanical - chemical (THMC) modeling of fluid flow and its control on localization of uranium deposits in the northeastern Athabasca basin, Saskatchewan

FY 2017-18

Summary
Uranium is an important source of energy, and Canada is the second largest uranium producer in the world. Currently all the uranium production in Canada is from high-grade uranium deposits known as unconformity-related uranium deposits in the Athabasca Basin in northern Saskatchewan. Many of these deposits were discovered based on an empirical model that uranium mineralization took place near faults crosscutting the unconformity between the basin and the basement, where uranium-bearing oxidizing fluids met and reacted with reducing agents, especially graphite and hydrocarbons derived from it. However, with increasing degrees of exploration, this model is facing more and more challenges, and a better understanding of the factors controlling mineralization is needed. The formation of large and rich uranium deposits requires that a large amount of uranium-bearing fluids passed through limited areas where one or more uranium precipitation mechanisms effectively removed uranium from the fluids. This involves thermal - hydraulic - mechanical - chemical (THMC) processes that may be simulated using numerical methods. The numerical models, if correctly established, can be used to predict favourable mineralization sites. In order to find the correct THMC model, multiple scenarios of numerical modeling using different physical and chemical parameters must be carried out and verified by comparing the modeling results with geological observations. It is therefore important to select a study area where much geological data relevant to mineralization have been accumulated. The northeastern part of the Athabasca Basin is chosen for this study because a number of world-class uranium deposits have been discovered in this area, and many of them have been studied in detail in terms of host rock lithology, basement structure, alteration, and orebody geometry and distribution. The research results will help the sponsor (Areva Resources Canada Inc.) and other uranium exploration companies to find more uranium deposits, which will contribute to job creation and economic prosperity for isolated northern communities.
Program
Collaborative Research and Development Grants
Location
Saskatchewan, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data

As published

Application id
492026-2015
Name nom
Chi, Guoxiang
Department département
Geology
Organization id
17
Institution établissement
University of Regina
Province en
Saskatchewan
Province fr
Saskatchewan
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2017
Competition year année de concours
2015
Award amount
62900
Program id
CRDPJ
Program name en
Collaborative Research and Development Grants
Program name fr
Subventions de recherche et développement coopérative
Group en
Research partnerships programs
Group fr
Programmes de partenariat
Committee code
96
Committee name en
RPP Internal Decision Cttee
Committee name fr
Cté de décision interne - PPR
Area of application code
202
Area of application group en
Natural resources (economic aspects)
Area of application group fr
Ressources naturelles (aspects économiques)
Area of application en
Mineral resources ( prospecting, exploration, mining, extraction, processing)
Area of application fr
Ressources minérales (prospection, exploration, mines, extraction et préparation)
Research subject code
4003
Research subject group en
Earth science
Research subject group fr
Sciences de la terre
Research subject en
Economic geology
Research subject fr
Géologie économique
Partie
2
Nb partie
3
Application title
Thermal - hydrolic - mechanical - chemical (THMC) modeling of fluid flow and its control on localization of uranium deposits in the northeastern Athabasca basin, Saskatchewan
Keyword
NSERC
Application summary
Uranium is an important source of energy, and Canada is the second largest uranium producer in the world. Currently all the uranium production in Canada is from high-grade uranium deposits known as unconformity-related uranium deposits in the Athabasca Basin in northern Saskatchewan. Many of these deposits were discovered based on an empirical model that uranium mineralization took place near faults crosscutting the unconformity between the basin and the basement, where uranium-bearing oxidizing fluids met and reacted with reducing agents, especially graphite and hydrocarbons derived from it. However, with increasing degrees of exploration, this model is facing more and more challenges, and a better understanding of the factors controlling mineralization is needed. The formation of large and rich uranium deposits requires that a large amount of uranium-bearing fluids passed through limited areas where one or more uranium precipitation mechanisms effectively removed uranium from the fluids. This involves thermal - hydraulic - mechanical - chemical (THMC) processes that may be simulated using numerical methods. The numerical models, if correctly established, can be used to predict favourable mineralization sites. In order to find the correct THMC model, multiple scenarios of numerical modeling using different physical and chemical parameters must be carried out and verified by comparing the modeling results with geological observations. It is therefore important to select a study area where much geological data relevant to mineralization have been accumulated. The northeastern part of the Athabasca Basin is chosen for this study because a number of world-class uranium deposits have been discovered in this area, and many of them have been studied in detail in terms of host rock lithology, basement structure, alteration, and orebody geometry and distribution. The research results will help the sponsor (Areva Resources Canada Inc.) and other uranium exploration companies to find more uranium deposits, which will contribute to job creation and economic prosperity for isolated northern communities.