Presenter: Vanessa Elongo
The Tombstone-Tungsten Belt (TTB) in the Canadian Cordillera is host to large tungsten deposits. The Cantung skarn deposit is one of the highest grade tungsten deposits in the TTB and is hosted in carbonate units surrounded by argillites.
Presenter: Rebecca Canam
The Nonacho Lake area located along the western margin of the Rae craton in the southeastern Northwest Territories consists of the ca. 1.91-1.82 Ga siliciclastic Nonacho Group interpreted to have been deposited
Presenter: Michel Plouffe
GEM-GeoNorth is the next version of the Geo-Mapping for Energy and Minerals (GEM). The new program will continue to enhance geological understanding of Canada’s North, focusing on areas with high potential for critical minerals and other mined commodities.
Presenter: Matthew Steele-MacInnis
Pine Point is a major carbonate-hosted Pb-Zn deposit, but key questions remain regarding its formation.
Presenter: Laurén Langlois
In this study we aim to identify elements that can act as geochemical indicators within the Yellowknife greenstone belt that allow the discrimination of mineralized structures.
Presenter: Kerstin Landry
Two styles of U mineralization are associated with the Nonacho Basin: early U of the Hope Occurrence (northern basin) is disseminated in quartz-biotite-albite basement breccia, whereas later vein-hosted
Presenter: Janina Czas
Copper isotope ratios are an important tool in tracing the sources and pathways of base metal forming fluids in the crust.
Presenter: Jade H. Lockie
The Paleoproterozoic Nonacho Basin remains an enigmatic sedimentary unit in the south-western portion of the Rae craton
Presenter: Isabelle McMartin
A new glacial geomorphology map covers 415 000 km2 in a core region of the Laurentide Ice Sheet in Nunavut.
Presenter: Grayson Bilak
The Exeter Lake Esker (ELE) extends across the Northwest Territories from Dubawnt Lake to Exmouth Lake and, sampling led to the discovery of the Lac de Gras kimberlite field.
