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An Abrupt Transition in the Mechanical Response of the Upper Crust to Transpression Along the Queen Charlotte Fault ; Bulletin of the Seismological Society of America

Published in 2015 by Anne M. Trehu, Maren Scheidhauer, Kristin M. M. Rohr, Basil Tikoff, Maureen A. L. Walton, Sean P. S. Gulick, Emily C. Roland
This paper was not found in any repository; the policy of its publisher is unknown or unclear.
This paper was not found in any repository; the policy of its publisher is unknown or unclear.

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Abstract

The Queen Charlotte Fault (QCF) is a major strike-slip fault that forms the boundary between the Pacific and North American plates from 51 degrees to 58 degrees N. Near 53.2 degrees N, the angle of oblique convergence predicted by the Mid-Ocean Ridge VELocity (MORVEL) interplate pole of rotation decreases from > 15 degrees in the south to