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Grant: Collaborative Research and Development Grants

Brandon University

$28,000.00

The significance of the silicification zones for the formation of unconformity-related uranium deposits in the Athabasca basin, Saskatchewan

FY 2019-20

Summary
It is becoming increasingly difficult to discover new uranium deposits in the Athabasca Basin due to the increasing depth of undiscovered mineralization, which necessitates an even better understanding of their formation conditions and setting. One feature of these deposits that has never been systematically studied is the silicification zone, or ""cap"", present immediately above the deposits in the Athabasca Group sandstones. The purpose of this project is to ascertain what the role, if any, this silicification played in the formation of the unconformity-related uranium deposits and to establish how it can affect exploration efforts. To achieve these goals, the project will focus on two main topics: (1) Establishing the three-dimensional spatial extent of the silicification zone. This will be done using drill logs available at AREVA and in the public domain. Two main possibilities are: the silicification zone is strictly local and situated directly above a deposit, or it occurs on a regional scale and is not directly related to a deposit. (2) Establishing the physical and chemical conditions of formation and the temporal relationship between the silicification zone and the deposits' formation. This will be achieved using mostly mineralogical and geochemical methods, in particular stable isotopes on quartz overgrowths and quartz filling pore space, using Secondary Ion Mass Spectrometry (SIMS), and fluid inclusions. It is anticipated that the findings of this project will help relate, spatially and temporally, the silicification zone with style and intensity of alteration, desilicification, structural setting, petrology, and most importantly, uranium deposition. The area studied will primarily be the Martin Lake U prospect, which exhibits well-developed silicification zones, with possible extension to the McArthur River Zone 2 and Centennial deposits. Once the significance of the silicification for uranium deposition has been established, the results will be assessed, in conjunction with AREVA geologists, in terms of increased exploration efficiency.
Program
Collaborative Research and Development Grants
Location
Manitoba, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data

As published

Application id
529837-2018
Name nom
Alexandre, Paul
Department département
Geology
Organization id
20
Institution établissement
Brandon University
Province en
Manitoba
Province fr
Manitoba
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2019
Competition year année de concours
2018
Award amount
28000
Program id
CRDPJ
Program name en
Collaborative Research and Development Grants
Program name fr
Subventions de recherche et développement coopérative
Group en
RESEARCH PARTNERSHIPS
Group fr
PARTENARIATS DE RECHERCHE
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
Installment
inst:1 - 1
Partie
1
Nb partie
1
Application title
The significance of the silicification zones for the formation of unconformity-related uranium deposits in the Athabasca basin, Saskatchewan
Keyword
NSERC
Application summary
It is becoming increasingly difficult to discover new uranium deposits in the Athabasca Basin due to the increasing depth of undiscovered mineralization, which necessitates an even better understanding of their formation conditions and setting. One feature of these deposits that has never been systematically studied is the silicification zone, or ""cap"", present immediately above the deposits in the Athabasca Group sandstones. The purpose of this project is to ascertain what the role, if any, this silicification played in the formation of the unconformity-related uranium deposits and to establish how it can affect exploration efforts. To achieve these goals, the project will focus on two main topics: (1) Establishing the three-dimensional spatial extent of the silicification zone. This will be done using drill logs available at AREVA and in the public domain. Two main possibilities are: the silicification zone is strictly local and situated directly above a deposit, or it occurs on a regional scale and is not directly related to a deposit. (2) Establishing the physical and chemical conditions of formation and the temporal relationship between the silicification zone and the deposits' formation. This will be achieved using mostly mineralogical and geochemical methods, in particular stable isotopes on quartz overgrowths and quartz filling pore space, using Secondary Ion Mass Spectrometry (SIMS), and fluid inclusions. It is anticipated that the findings of this project will help relate, spatially and temporally, the silicification zone with style and intensity of alteration, desilicification, structural setting, petrology, and most importantly, uranium deposition. The area studied will primarily be the Martin Lake U prospect, which exhibits well-developed silicification zones, with possible extension to the McArthur River Zone 2 and Centennial deposits. Once the significance of the silicification for uranium deposition has been established, the results will be assessed, in conjunction with AREVA geologists, in terms of increased exploration efficiency.
Brandon University - $28,000 Grant (2019-20) | Canada Spends