Two important problems of continental tectonics may be resolved by recognizing that most subduction zone backarcs have hot, thin, and weak lithospheres over...
The elastic thickness of the continental lithosphere is closely related to its total strength and therefore to its susceptibility to tectonic deformation and...
Processing and interpretation of magnetotelluric data, recorded as part of the LITHOPROBE Southern Cordillera transect studies, across the boundary of the...
We investigate the thermal consequences of sediment thickening and fluid expulsion in subduction zone accretionary prisms using a model where the rate of fluid...
It has been proposed that the seismogenic zone of subduction thrust faults is primarily controlled by temperature or rock composition changes. We have...
Recordings of local earthquakes from 16 three-component broadband seismic stations in southwestern British Columbia, Washington, and northern Oregon are used...
Large offset multichannel seismic reflection data from the subduction zone margin off Vancouver Island define the geometry, internal structure, and deformation...
A fundamental problem in plate tectonics is the shear strength of major plate boundary faults. This translates to the question whether the generally observed...
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