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The crustal evolution of North Korea is poorly constrained. This study utilises detrital zircon U–Pb and Lu–Hf isotopic data, obtained from sands at the mouths of the Taedong, Chongchon and Songchon Rivers, in order to sample the Rangnim massif. These data are then used to constrain the magmatic age spectrum and crustal growth history of this massif. Zircon U–Pb analyses indicate that the Rangnim...
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