Grant: Alliance Grants
University of Calgary
$154,500.00
A passive seismic investigation of the geothermal potential of strike-slip faults in the southern Yukon
EF 2023-24
Résumé
Geothermal energy is not widely used in Canada, and the location and extent of available resources are poorly understood. We will examine the geothermal viability throughout the southern Yukon, as several factors suggest the region is ideal for geothermal prospecting. First, the southern Yukon exhibits evidence of high temperatures at shallow depths. Additionally, large crustal faults transect the southern Yukon and likely mark locations of increased rock permeability that can facilitate fluid flow and heat transport. Finally, there are hot springs in the area where geothermal heat reaches the surface. Investigating geophysical conditions in the southern Yukon will facilitate the future development of geothermal resources in northern Canada by addressing specific knowledge gaps. These gaps include: (1) detecting and precisely locating earthquakes, (2) inferring the state of stress and style of deformation around large crustal faults, and (3) generating geophysical images of Earth's subsurface near these faults. Addressing these knowledge gaps will allow us to illuminate the location and extent of faulted rocks at depth, which act as pathways for geothermal fluids. Furthermore, the knowledge gained from this work will allow us to differentiate between regions where fluids can circulate and regions where tectonic forces close rock fracture networks and inhibit flow. For this project, we are partnering with the Yukon Geological Survey, which has significant experience studying the geology of the territory and has recently initiated several investigations related to the geothermal potential in the Yukon. Our study will exploit recent advances in monitoring technology that uses fiber-optic sensing to provide near-continuous spatial sampling of the seismic wavefield and thermal variations. As part of this work, we will collaborate with MoMacMo who are experts in distributed acoustic and temperature sensing (DAS and DTS) and will assist in the collection, analysis, and interpretation of these advanced datasets. The insights into fault structure and dynamics attained by this project will contribute to geothermal development in the Yukon, as well as in regions with similar geological conditions elsewhere in Canada and globally.
Programme
Alliance Grants
Bénéficiaire
Emplacement
Alberta, Canada
Type de bénéficiaire
Academia
Type
Grant
Source
NSERC's Awards Data
Tel que publié
Application id
580887-2022
Name nom
Gilbert, Hersh HJ
Department département
Geoscience
Organization id
11
Institution établissement
University of Calgary
Province en
Alberta
Province fr
Alberta
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2023
Competition year année de concours
2022
Award amount
154500
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
303
Area of application group en
Energy resources
Area of application group fr
Ressources d'énergie
Area of application en
Alternative energy resources
Area of application fr
Autres ressources d'énergie
Research subject code
4005
Research subject group en
Earth science
Research subject group fr
Structural geology andtectonics
Research subject en
Sciences de la terre
Research subject fr
Géologie structurale et tectonique des plaques
Application title
A passive seismic investigation of the geothermal potential of strike-slip faults in the southern Yukon
Keyword
Denali fault; earthquake hazard; geothermal; seismic array; Teslin fault; Tintina fault
Application summary
Geothermal energy is not widely used in Canada, and the location and extent of available resources are poorly understood. We will examine the geothermal viability throughout the southern Yukon, as several factors suggest the region is ideal for geothermal prospecting. First, the southern Yukon exhibits evidence of high temperatures at shallow depths. Additionally, large crustal faults transect the southern Yukon and likely mark locations of increased rock permeability that can facilitate fluid flow and heat transport. Finally, there are hot springs in the area where geothermal heat reaches the surface. Investigating geophysical conditions in the southern Yukon will facilitate the future development of geothermal resources in northern Canada by addressing specific knowledge gaps. These gaps include: (1) detecting and precisely locating earthquakes, (2) inferring the state of stress and style of deformation around large crustal faults, and (3) generating geophysical images of Earth's subsurface near these faults. Addressing these knowledge gaps will allow us to illuminate the location and extent of faulted rocks at depth, which act as pathways for geothermal fluids. Furthermore, the knowledge gained from this work will allow us to differentiate between regions where fluids can circulate and regions where tectonic forces close rock fracture networks and inhibit flow. For this project, we are partnering with the Yukon Geological Survey, which has significant experience studying the geology of the territory and has recently initiated several investigations related to the geothermal potential in the Yukon. Our study will exploit recent advances in monitoring technology that uses fiber-optic sensing to provide near-continuous spatial sampling of the seismic wavefield and thermal variations. As part of this work, we will collaborate with MoMacMo who are experts in distributed acoustic and temperature sensing (DAS and DTS) and will assist in the collection, analysis, and interpretation of these advanced datasets. The insights into fault structure and dynamics attained by this project will contribute to geothermal development in the Yukon, as well as in regions with similar geological conditions elsewhere in Canada and globally.