A new heat flow map has been constructed for northeastern British Columbia, using log-heading temperature records corrected for drilling disturbance, at depths...
The methane hydrate stability zone beneath Sverdrup Basin has developed to a depth of 2 km underneath the Canadian Arctic Islands and 1 km below sea level...
High electrical conductivity and high heat flow coexist in much of the Canadian Cordillera, a region of recent accretion of crustal terranes to North America....
Over 8 400 bottom-hole temperature (BHT) values from the Canadian part of the Williston Basin were analyzed and a temperature high was discovered in the...
In much of the southern Canadian Cordillera, the top of the lower-crustal electrical conductor coexists with the 450°C isotherm. A statistical correlation...
Rapid gas hydrate release (the "clathrate gun" hypothesis) has been invoked as a cause for the rapid global warming and associated negative carbon isotope...
Maps of shallow depth (down to -250 m) temperature distribution across Canada show large variability, related mainly to surface climatic forcing. Very small...
To understand better the formation and history of petroleum gas hydrates in terrestrial permafrost regions, we have performed numerical temperature profile...
Geothermal gradients in the Alberta part of the Western Canadian sedimentary basin have been studied on the basis of 55,244 bottom-hole temperature values from...
Data from eleven petroleum exploration wells along a south-north profile in the Sverdrup Basin of the Canadian Arctic Islands indicate large variations in...
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