Large-scale coast-parallel displacements in the Cordillera: a granitic resolution to a paleomagnetic dilemma

Resolution of the `Paleomagnetic dilemmaʹ, the discrepancy between large paleomagnetically determined dextral displacement of outboard portions of the northern Cordillera, and much smaller offsets implied by mapping and stratigraphic correlations, is fundamental to understanding the tectonic evolution of the Cordillera. This paper presents structural orientation data from the middle Cretaceous Dawson Range batholith of west central Yukon and its wallrocks, and suggests that some of the `missingʹ displacement may be found in intrusions. The elongate northwest-trending batholith has a margin-parallel foliation, a sub-horizontal stretching lineation, and records syn-intrusive dextral shearing. In country rocks adjacent to the batholith, north-trending lineations are deflected clockwise into near parallelism with the batholithʹs margins; lineations from wallrock screens within the batholith are all aligned parallel with the batholithʹs long axis. The Big Creek strike-slip fault forms the north-margin of the batholith and accommodated a minimum of 20 km of dextral slip. These observations imply that the batholith invaded an active dextral shear zone, accommodated shearing while crystallizing, and focused post-crystallization fault development. The batholith is conservatively estimated to have accommodated 45 km of syn-intrusive shearing. Collectively, middle Cretaceous intrusions of the northern Cordillera may account for >400 km of previously unrecognized dextral displacement.