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Grant: Alliance Grants

University of Regina

$20,010.00

Structural evolution and mineral potential of the Tazin River shear zone in the Hill Island Lake area, southern Taltson orogen, Northwest Territories

EF 2024-25

Résumé
The Precambrian shield of Canada consists of several large Archean (> 2.5 billion year) blocks that collided during a major period of mountain building, ca. 2.0-1.8 billion years ago to form earth's first supercontinent, Nuna. While progress has been made on understanding how these blocks came together, significant uncertainty remains, especially in the western shield where the relative effects of superposed tectonism related to older (2.5-2.3 billion year) Arrowsmith orogenesis (mountain building) and younger (2.01-1.91 billion year) Thelon-Taltson orogenesis are difficult to distinguish. Within this context, faults have a profound influence on the development of mountain belts. While they typically play a role, early on (i.e., collisional stages) they are commonly also re-activated during the later stages. Faults are also major conduits for hot, deep crustal fluids that carry critical elements, including gold. The proposed research deals with the Tazin River shear zone, a major fault zone in the southern Taltson orogen, Northwest Territories. While this fault/shear zone appears to have a long-lived history, the nature and timing of fault movement remains uncertain. It is also unclear if this fault zone represents an early boundary between colliding blocks, or merely a locus of younger differential movement and uplift. Through mapping and cutting-edge techniques in geochronology this research will help to determine the history of this fault zone; and in particular, figure out if it was active (i.e., a fundamental boundary) during early stages of orogenesis, and if and how it was reactivated during later stages. It will also study the timing/controls of fault-related mineral occurrences, including gold. This knowledge of fault history within a regional geologic framework, coupled with mineralogical controls, will provide up-dated knowledge on mineral prospectivity within a poorly known region of the shield. This research thus promises to help a variety of stakeholders, including federal, territorial and Indigenous governments/organizations, to make informed decisions on mineral resource potential in this region, which could impact future prosperity.
Programme
Alliance Grants
Bénéficiaire
Emplacement
Saskatchewan, Canada
Type de bénéficiaire
Academia
Type
Grant
Source
NSERC's Awards Data

Tel que publié

Application id
601744-2024
Name nom
Bethune, Kathryn KM
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
2024
Competition year année de concours
2024
Award amount
20010
Program id
ALLRP
Program name en
Alliance Grants
Program name fr
Subventions Alliance
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
1203
Area of application group en
Advancement of knowledge
Area of application group fr
Avancement des connaissances
Area of application en
Earth sciences
Area of application fr
Sciences de la terre
Research subject code
4005
Research subject group en
Earth science
Research subject group fr
Sciences de la terre
Research subject en
Structural geology andtectonics
Research subject fr
Géologie structurale et tectonique des plaques
Field of research list names en
Not available
Field of research list names fr
Non disponible
Socioeconomic objective list names en
Not available
Socioeconomic objective list names fr
Non disponible
Application title
Structural evolution and mineral potential of the Tazin River shear zone in the Hill Island Lake area, southern Taltson orogen, Northwest Territories
Keywords
40-39ar thermochronology; mapping & structural analysis; mineral potential; petrology; shear zone; southern taltson orogen (nts 75c); structural geology; tectonics; u-pb geochronology
Application summary
The Precambrian shield of Canada consists of several large Archean (> 2.5 billion year) blocks that collided during a major period of mountain building, ca. 2.0-1.8 billion years ago to form earth's first supercontinent, Nuna. While progress has been made on understanding how these blocks came together, significant uncertainty remains, especially in the western shield where the relative effects of superposed tectonism related to older (2.5-2.3 billion year) Arrowsmith orogenesis (mountain building) and younger (2.01-1.91 billion year) Thelon-Taltson orogenesis are difficult to distinguish. Within this context, faults have a profound influence on the development of mountain belts. While they typically play a role, early on (i.e., collisional stages) they are commonly also re-activated during the later stages. Faults are also major conduits for hot, deep crustal fluids that carry critical elements, including gold. The proposed research deals with the Tazin River shear zone, a major fault zone in the southern Taltson orogen, Northwest Territories. While this fault/shear zone appears to have a long-lived history, the nature and timing of fault movement remains uncertain. It is also unclear if this fault zone represents an early boundary between colliding blocks, or merely a locus of younger differential movement and uplift. Through mapping and cutting-edge techniques in geochronology this research will help to determine the history of this fault zone; and in particular, figure out if it was active (i.e., a fundamental boundary) during early stages of orogenesis, and if and how it was reactivated during later stages. It will also study the timing/controls of fault-related mineral occurrences, including gold. This knowledge of fault history within a regional geologic framework, coupled with mineralogical controls, will provide up-dated knowledge on mineral prospectivity within a poorly known region of the shield. This research thus promises to help a variety of stakeholders, including federal, territorial and Indigenous governments/organizations, to make informed decisions on mineral resource potential in this region, which could impact future prosperity.