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Detrital zircons from the Nanaimo basin, Vancouver Island, British Columbia: an independent test of Late Cretaceous to Cenozoic northward translation
The development of the Cordilleran orogen of western North American is disputed despite a century of study. Paleomagnetic observations require large-scale dextral displacements of crustal fragments along the western margin of North America, from low latitudes to moderate latitudes during the Cretaceous-Paleogene.
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