Hf model ages yielded by rutiles in a garnetrich lower-crustal granulite xenolith from the McBride Province and whole-rock Nd and Hf model ages for the plagioclase-and garnet-rich Chudleigh and McBride granulites overlap with the well-defined U-Pb ages for detrital zircons and zircons in granitoids (Murgulov et al.
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