CHIME ages of zircons in granitic gneiss and granite from Samilpo, southeastern Democratic People's Republic of Korea
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概要
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The CHIME (chemical Th-U-total Pb isochron method) dating was carried out for zircons from pyrope-rich (Prp_<28>-Prp_<32>) garnet-bearing granitic gneiss and topaz-bearing biotite granite from the Samilpo region in the southeastern part of Democratic People's Republic of Korea. Zircons from the garnet-bearing granitic gneiss show a distinct core-rim structure ; the cores yield an early Proterozoic age of 2133±56 Ma, and the rims yield a poorly defined age of ca. 1500 Ma. The core and rim ages agree well with those for protolith formation and high-grade metamorphism, respectively, of the basement gneiss complex in the Gyeonggi Massif. Zircons from the topaz-bearing granite show a middle Jurassic age of 172±4 Ma, suggesting the granite to be assigned to the Jurassic Daebo Granite.
- 名古屋大学の論文
著者
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Suzuki Kazuhiro
Department of Earth and Environmental Sciences, Nagoya University
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Kato Takenori
Department Of Earth And Planetary Sciences Graduate School Of Science Nagoya University
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Yonezawa Chinatsu
Remote Sensing Technology Center Of Japan
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MORISHITA Taisei
Department of Earth and Planetary Sciences, Graduate School of Science, Nagoya University
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Morishita Taisei
Department Of Earth And Planetary Sciences Graduate School Of Science Nagoya University
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Suzuki Kazuhiro
Department Of Cardiovascular Surgery Yamaguchi Grand Medical Center
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