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Several isolated lensoidal mafic and serpentinized ultramafic bodies occur in the Hongseong area, South Korea, which is the Korean extension of the Dabie–Sulu collisional belt of China and the northern margin of the South China Block. The mafic and ultramafic bodies are important in any interpretation of the Neoproterozoic tectonics of northeast Asia related to the amalgamation and break-up of the...
The Hongseong area in the western Gyeonggi Massif, South Korea, is characterized by the occurrence of several isolated ultramafic lenses in close association with metabasites within the granitic gneiss. Most of these bodies suffered various degrees of serpentinization and also have been highly deformed and metamorphosed. The Bibong ultramafic rock is assumed to be a mantle section of a probable Neoproterozoic...
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