Metamorphic and magmatic evolution of the Paleoproterozoic gneisses in the Sancheong area, Yeongnam Massif, South Korea, and their implications to the tectonics in the Northeast Asia

- The study area underwent intermediate-P/T metamorphism between ca. 1920-1880 Ma.
- The study area also underwent low-P/T metamorphism at ca. 1860 Ma.
- The post-collision igneous activity occurred between two metamorphism (1880-1860 Ma)
- The study area underwent collision and post-collision process during 1920-1860 Ma.
- The study area may be correlated to eastern Cathaysia Block in the South China Craton.

The Sancheong area in the southwestern Yeongnam Massif mainly consists of Precambrian paragneisses (quartz-feldspathic and garnet gneiss), orthogneiss (porphyritic gneiss) and anorthosite and is important for an understanding the tectonic evolution of the southern part of the Korean Peninsula and Northeast Asia. The Precambrian paragneisses in the Sancheong area underwent intermediate-P/T metamorphism (quartz-feldspathic gneiss; 730 °C and 12.2 kbar). The intermediate-P/T metamorphism was overprinted by regional low-P/T metamorphism (750-820 °C and 7.0-9.0 kbar) which was followed by amphibolite-facies retrograde metamorphism. In contrast, the orthogneiss only experienced the low-P/T (750-800 °C and 8.0-8.7 kbar) metamorphism followed by the amphibolite-facies retrograde metamorphism. Zircon U-Pb dating indicates that the intermediate-P/T metamorphism likely occurred at ca. 1880-1920 Ma and that the low-P/T metamorphism occurred at ca. 1855-1859 Ma. The whole-rock geochemical data and zircon U-Pb ages indicate that the protolith of the porphyritic gneiss and the anorthosite were emplaced in a post-collisional tectonic setting during ca. 1872-1880 Ma and ca. 1860 Ma, respectively. These data suggest that the Sancheong area underwent continental collision associated with the intermediate-P/T metamorphism (ca. 1920-1880 Ma) and post-collisional igneous activity associated with the low-P/T metamorphism during the Paleoproterozoic (ca. 1856-1880 Ma). Similar Paleoproterozoic tectonic events were recently reported from the eastern Cathaysia Block, suggesting that the Yeongnam Massif may have a close affinity to the eastern Cathaysia Block.