The Queen Charlotte Fault, British Columbia: seafloor anatomy of a transform fault and its influence on sediment processes

@article{Barrie2013TheQC,
  title={The Queen Charlotte Fault, British Columbia: seafloor anatomy of a transform fault and its influence on sediment processes},
  author={J. Vaughn Barrie and Kim W. Conway and Peter Townsend Harris},
  journal={Geo-Marine Letters},
  year={2013},
  volume={33},
  pages={311-318}
}
The Queen Charlotte Fault Zone (QCFZ) off western Canada is the northern equivalent to the San Andreas Fault Zone, the Pacific–North American plate boundary. Geomorphologic expression and surface processes associated with the QCFZ system have been revealed in unprecedented detail by recent seabed mapping surveys. Convergence of the Pacific and North American plates along northern British Columbia is well known, but how the QCFZ accommodates this convergence is still a subject of controversy… 
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References

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Transpression between two warm mafic plates: The Queen Charlotte Fault revisited
The Queen Charlotte Fault is a transpressive transform plate boundary between the Pacific and North American plates offshore western Canada. Previous models for the accommodation of transpression
Structure, seismicity, and thermal regime of the Queen Charlotte Transform Margin
[1] This study examines structural, seismicity, thermal, and current deformation constraints on the tectonic regime of the Queen Charlotte Margin located off the northwest coast of Canada. The margin
Evidence for underthrusting beneath the Queen Charlotte Margin, British Columbia, from teleseismic receiver function analysis
SUMMARY The Queen Charlotte Fault zone is the transpressive boundary between the North America and Pacific Plates along the northwestern margin of British Columbia. Two models have been suggested for
Queen Charlotte fault zone: microearthquakes from a temporary array of land stations and ocean bottom seismographs
A temporary array of land and ocean bottom seismograph stations was used to accurately locate microearthquakes on the Queen Charlotte fault zone, which occurs along the continental margin of western
Pacific‐North America plate boundary reorganization in response to a change in relative plate motion: Offshore Canada
The transition from subduction in Cascadia to the transform Queen Charlotte fault along western Canada is often drawn as a subduction zone, yet recent studies of GPS and earthquake data from northern
Queen Charlotte Area Cenozoic tectonics and volcanism and their association with relative plate motions along the northeastern Pacific Margin
Cenozoic relative plate interactions along the Queen Charlotte margin, based on published models for the North America and northeast Pacific plates, are related to the tectonic and igneous history of
Distribution of the Pacific/North America motion in the Queen Charlotte Islands‐S. Alaska plate boundary zone
We present GPS data that constrain the distribution of the relative Pacific/North America motion across the Queen Charlotte Islands‐Alaska Panhandle margin (NW North America). Velocities from a
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