The Paleoproterozoic Hottah terrane is the westernmost exposed bedrock of the Canadian Shield and a critical component for understanding the evolution of the...
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...
The supracrustal assemblages of many Archean cratons contain significant volumes of graywacke-mudstone turbidites, and, notably, the stratigraphy of the Slave...
The Lay Range assemblage, the lowest exposed lithostratigraphic unit of north-central Quesnellia, is separated into lower sedimentary and upper mafi c tuff...
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 Slave craton underwent widespread extension during the Paleoproterozoic. The East Arm basin of Great Slave Lake formed during this period and preserves a...
Giant magmatic-driven hydrothermal systems are associated with episodic construction of 1.88 - 1.84 Ga continental stratovolcano complexes along the Great Bear...
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...
The Wopmay orogen is a Paleoproterozoic accretionary belt preserved to the west of the Archean Slave craton, northwest Canada. Reworked Archean crystalline...
Detrital zircon from three coarse-grained marine siliciclastic rocks was analyzed for U-Pb, Lu-Hf, and trace element data to determine the timing of deposition...
Périodique (revue)
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