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CHIME Ages of Monazites from Metamorphic Rocks from the Precambrian Gyeonggi Gneiss Complex in the Shiheung and Seosan Group of the Gyeonggi Massif, South Korea  

Kim, Kyu-Han (Department of Science Education, Ewha Womans University)
Suzuki, Kazuhiro (Center for Chronological Research, Nagoya University)
Lee, Jong-Ik (Korea Polar Research Institute, KORDI)
Jang, Hyun-Kyung (Department of Science Education, Ewha Womans University)
Publication Information
Economic and Environmental Geology / v.41, no.2, 2008 , pp. 173-181 More about this Journal
Abstract
CHIME ages were obtained from monazites in metamorphic rocks from the Seosan and Siheung Groups in the Gyeonggi gneiss complex, Korean peninsula. Monazite CHIME ages range from 234 to 257 Ma, corresponding to the late Permian to middle Triassic Songrim disturbance due to the collision event between the North and South China blocks within the Gyeonggi gneiss complex in the Korean peninsula. The CHIME ages are consistent with the metamorphic ages from the Hongseong area (231 Ma, Kim et al., 2006) and the Odesan area (245-248 Ma, Oh et al., 2006b) in the Gyeonggi gneiss complex and are older than those from the Dabie-Sulu collision belt (220${\sim}$242 Ma, Yang or of., 2003; Liu et al., 2003, 2004) suggesting that the collision between the North and South China blocks had occurred earlier in Korea than China.
Keywords
Gyeonggi gneiss complex; CHIME age; Seosan Group; Siheung Group; monazite;
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