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The North Qaidam terrane lies between the Qaidam and Qilian blocks of western China, and contains the Shenglikou ultrahigh-pressure (UHP) garnet peridotite massif. Simultaneously analyzed U–Pb ages, trace element patterns and Hf-isotope compositions of zircons from the peridotite massif and its country rocks (migmatite and gneiss) reveal the complex evolution of the terrane. Zircons in peridotite...
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