The North America Cordillera mobile belt has accommodated relative motion between the North America plate and various oceanic plates since the early Mesozoic....
The northern Canadian Cordillera is remarkably tectonically and seismically active, extending from a terrane collision zone on the continental margin to an...
A three-dimensional seismic reflection survey was carried out over a gas hydrate field offshore Vancouver Island in the area of Ocean Drilling Program Leg 146,...
On the northern Cascadia subduction margin, the multichannel seismic amplitude-versus-offset (AVO) behavior of a bottom-simulating reflector (BSR) suggests a P...
We estimate the rate of crustal deformation in the central and northern Cascadia forearc based on a combination of existing global positioning system (GPS)...
The Queen Charlotte Fault zone is the transpressive boundary between the North America and Pacific Plates along the northwestern margin of British Columbia....
Seafloor compliance, the transfer function between pressure induced by surface gravity waves and the associated seafloor deformation, can address outstanding...
At the northern Cascadia margin, the Juan de Fuca plate is underthrusting North America at about 45 mm yr-1 (ref. 1), resulting in the potential for...
We present a new three-dimensional (3-D) P-wave velocity model for the upper-crustal structure beneath the Strait of Georgia, southwestern British Columbia...
In this study we first summarize the constraints that on the Cascadia subduction thrust, there is a 70km gap downdip between the megathrust seismogenic zone...
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