The supracrustal assemblages of many Archean cratons contain significant volumes of graywacke-mudstone turbidites, and, notably, the stratigraphy of the Slave...
The Contact Lake Belt forms the NW-trending flank of a collapsed andesite stratovolcano complex adjacent to a subvolcanic intrusion within the northern, 1.87...
Our understanding of the onset and evolution of flood basalt volcanism is rooted in the study of the character and internal architecture of its eruptive...
The Lay Range assemblage, the lowest exposed lithostratigraphic unit of north-central Quesnellia, is separated into lower sedimentary and upper mafi c tuff...
The Paleoproterozoic Hottah terrane is the westernmost exposed bedrock of the Canadian Shield and a critical component for understanding the evolution of the...
The Wopmay orogen is a Paleoproterozoic accretionary belt preserved to the west of the Archean Slave craton, northwest Canada. Reworked Archean crystalline...
The NICO Au-Co-Bi(±Cu±W) deposit is located in the Great Bear magmatic zone, NWT, Canada, where numerous polymetallic, iron oxide-dominated mineralized systems...
Giant magmatic-driven hydrothermal systems are associated with episodic construction of 1.88 - 1.84 Ga continental stratovolcano complexes along the Great Bear...
The Paleoproterozoic Wopmay orogen is modelled as a classic arc-continent collision involving the Archean Slave craton and an enigmatic continental arc termed...
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