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 Canada's two largest …

Abstract The Pacific/North American plate boundary is undergoing predominantly right-
lateral strike–slip motion along the Queen Charlotte and Fairweather transform faults. The …

This article provides a summary of the structure and tectonic history of the Queen Charlotte
transform fault zone off western Canada, as background to understanding the 2012 M w 7.8 …

The Queen Charlotte Fault is a transpressive transform plate boundary between the Pacific
and North American plates offshore western Canada. Previous models for the …

Dynamic processes at sheared margins associated with the formation of sedimentary basins
and marginal ridges are poorly understood. The southern African margin provides an …

Abstract The 2012 M w 7.8 Haida Gwaii earthquake confirmed very oblique subduction and
slip partitioning at the southern Queen Charlotte margin. In this study, we re‐examine the …

All the significant (ML≥ 4) events in the 2012 Haida Gwaii earthquake sequence are
systematically relocated, and their moment tensor solutions are determined from waveform …

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 …

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 …

Abstract 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 …