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Grant: Collaborative Research and Development Grants

University of Manitoba

$55,743.00

Assessing the geochronology,geochemistry and regional tectonic setting of uranium deposits as drivers for exploration

FY 2018-19

Summary
Worldwide, there will be ~500 nuclear reactors operating by 2030, which will result in a 66% increase in global nuclear power generation. As global appetite for energy and commodities expands with the world's population, Canada's rich natural resources will continue to enjoy international prominence. This is particularly true for uranium (U) where demand will outstrip supplies in 10-20 years. To remain at the forefront of an ever-competitive mining and energy exploration market, Canada and its industries need to adopt a leadership position in the development of strategies for innovative and sustainable resource extraction. Sedimentary basins are host to some of the largest and richest U resources in the world, and there are tens of underexplored basins in Canada and the world. How can we distinguish between prospective and barren structures? One possible method is to quantitatively compare mineralized and barren tectonic structures, and the source of mineralizing and barren fluids. Uranium mineralizing processes are generally associated with complex hydrothermal systems that involved repeated fault slip and fluid flow along major structures. Consequently, understanding fluid movement through structures within these terrains and the source of U is of great importance for mineral exploration. It is necessary to use different isotopic methods because host rocks, fluid composition and possibly temperature are different, thus, precipitating different types of minerals. Therefore, we propose to use different isotopic systems to determine the age of faults and fluid compositions from different minerals. This proposal brings together academic researchers in partnership with industry members (AREVA) to develop improved exploration criteria for U deposits. The expected outcome is to train 4 HQP, and provide the U and mineral industry with a method that will allow them to distinguish between barren and mineralized faults and fractures, thus reducing drilling costs and impact on the environment by targeting only prospective structures.
Program
Collaborative Research and Development Grants
Location
Manitoba, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data

As published

Application id
508255-2016
Name nom
Fayek, Mostafa
Department département
Geological Sciences
Organization id
19
Institution établissement
University of Manitoba
Province en
Manitoba
Province fr
Manitoba
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2018
Competition year année de concours
2016
Award amount
55743
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
300
Area of application group en
Energy resources
Area of application group fr
Ressources d'énergie
Area of application en
Energy resources (including production, exploration, processing, distribution and use)
Area of application fr
Ressources d'énergie (production, exploration, traitement, distribution et utilisation de l'énergie)
Research subject code
4200
Research subject group en
Geochemistry and geochronology
Research subject group fr
Géochimie et géochronologie
Research subject en
Geochemistry and geochronology
Research subject fr
Géochimie et géochronologie
Partie
2
Nb partie
2
Application title
Assessing the geochronology,geochemistry and regional tectonic setting of uranium deposits as drivers for exploration
Keyword
NSERC
Application summary
Worldwide, there will be ~500 nuclear reactors operating by 2030, which will result in a 66% increase in global nuclear power generation. As global appetite for energy and commodities expands with the world's population, Canada's rich natural resources will continue to enjoy international prominence. This is particularly true for uranium (U) where demand will outstrip supplies in 10-20 years. To remain at the forefront of an ever-competitive mining and energy exploration market, Canada and its industries need to adopt a leadership position in the development of strategies for innovative and sustainable resource extraction. Sedimentary basins are host to some of the largest and richest U resources in the world, and there are tens of underexplored basins in Canada and the world. How can we distinguish between prospective and barren structures? One possible method is to quantitatively compare mineralized and barren tectonic structures, and the source of mineralizing and barren fluids. Uranium mineralizing processes are generally associated with complex hydrothermal systems that involved repeated fault slip and fluid flow along major structures. Consequently, understanding fluid movement through structures within these terrains and the source of U is of great importance for mineral exploration. It is necessary to use different isotopic methods because host rocks, fluid composition and possibly temperature are different, thus, precipitating different types of minerals. Therefore, we propose to use different isotopic systems to determine the age of faults and fluid compositions from different minerals. This proposal brings together academic researchers in partnership with industry members (AREVA) to develop improved exploration criteria for U deposits. The expected outcome is to train 4 HQP, and provide the U and mineral industry with a method that will allow them to distinguish between barren and mineralized faults and fractures, thus reducing drilling costs and impact on the environment by targeting only prospective structures.