It is well recognized that active arc volcanism at nearly all subduction zones requires temperatures greater than 1200\'01C in the subarc mantle, despite the...
Global mountain belts are commonly concluded to be a consequence of crustal thickening resulting from continental collision, with high elevations supported by...
It has been proposed that the seismogenic zone of subduction thrust faults is primarily controlled by temperature or rock composition changes. We have...
The thermal structure of a subduction zone controls many key processes, including subducting plate metamorphism and dehydration, the megathrust earthquake...
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...
At subduction zones, geophysical and geochemical observations indicate that the arc and backarc regions are hot, in spite of the cooling effects of a...
Recordings of local earthquakes from 16 three-component broadband seismic stations in southwestern British Columbia, Washington, and northern Oregon are used...
We have examined shear wave splitting of SKS phases at 26 permanent broadband stations in western North America to constrain regional trends in anisotropy at...
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