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Response highlights new detrital zircon data, suggesting implications for tectonic evolution in the northern Cordillera.
We thank G. Lowey for their comment and interest in our paper documenting new U-Pb age and Hf isotope analyses of detrital zircon from the Late Cretaceous Kluane Schist, Yukon, Canada. We also appreciate the opportunity to further highlight the important role that the Kluane Schist plays in informing ongoing debates regarding the Mesozoic tectonic evolution of the northern Cordillera.
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McKenzie et al. (2026) studied this question.
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