At subduction zones, geophysical and geochemical observations indicate that the arc and backarc regions are hot, in spite of the cooling effects of a...
The heat flow in the northern Canadian Cordillera between 59 and 64 N is very high, 105 ± 22 mW/m2. The average upper crust heat generation is 4.6 ± 2.4...
Seismic velocity-depth profiles are available from four types of measurements in the area of Ocean Drilling Program Leg 131,
Site 808; (1) laboratory...
Two important problems of continental tectonics may be resolved by recognizing that most subduction zone backarcs have hot, thin, and weak lithospheres over...
The amount of gas hydrates in the accretionary wedge sediments of the northern Cascadia subduction zone off Vancouver Island has been estimated from...
Evidence has been obtained for the accumulation of elastic strain across the northern Cascadia subduction zone that may be released in a future very large...
The elastic thickness of the continental lithosphere is closely related to its total strength and therefore to its susceptibility to tectonic deformation and...
Magnetic susceptibility measurements on near-surface sediment cores from the North Cascadia accretionary sedimentary prism show that seismic blanking or...
The boundary between the Pacific and North America plates along Canada's west coast is one of the most seismically active regions of Canada, and is where...
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