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A careful literature review reveals that the Gyeonggi Massif in Korea extensively undergoes the collision-related metamorphism during the Triassic and thus represents a subduction complex with the South China affinity. The Triassic subduction complex is bounded by the Imjingang belt to the north and the Hongseong–Odesan belt to the south and can be well correlated with the Sulu–Dabie belts of China...
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