A number of studies suggest a significant decline of river discharge in the Canadian Plains that drain the eastern slopes of the Canadian Rocky Mountains, and...
The Ordovician saw major diversification in marine life abruptly terminated by the Late Ordovician mass extinction (LOME). Around 85% of species were...
The temporal link between large igneous province (LIP) eruptions and at least half of themajor extinctions of the Phanerozoic implies that large scale...
A combined sequence stratigraphic and geochemical study of the Latest Permian Extinction event in NW Pangea provides new insight into the onset and extension...
We summarize the feasibility of using geothermal energy from the Western Canada Sedimen-tary Basin (WCSB) to support communities with population >3,000,...
The Winnipeg and Deadwood formations form deep clastic reservoirs in Saskatchewan, Canada, with temperatures exceeding 40°C over most of southern Saskatchewan...
In order to help assessment of enhanced geothermal energy potential in Canada, we constructed a new series of heatflow and depth - temperature distribution...
Thermal springs are commonly thought to be an indicator of geothermal resource potential. However, there have been few analyses of the relationship between...
Brine springs discharging from Devonian carbonates of the Western Canada Sedimentary Basin have distinct water chemistry from brines in laterally equivalent...
A major late Paleozoic depocenter, the Sverdrup Basin, Canadian High Arctic, has been excluded from the end-Permian extinction debate as early workers presumed...
Périodique (revue)
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