Proceedings of the KSEEG Conference (대한자원환경지질학회:학술대회논문집)
- 2003.04a
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- Pages.194-195
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- 2003
REE variation of Ultramafic rocks related to the Serpentinization, the Gyeonggi Massifs in the western Korea
- Seo, Ji-Eun (Department of Earth and environmental Sciences, Korea University) ;
- Park, Seon-Gyu (Department of Earth and environmental Sciences, Korea University) ;
- Oh, Chang-Whan (Department of Earth and Environmental Sciences, Chonbuk National University) ;
- Song, Suck-Hwan (Department of Environmental Engineering, Joonbu University)
- Published : 2003.04.01
Abstract
High-pressure amphibolite-facies rocks with serpentinized ultramafic rocks occur in the Gyeonggi Massif. Ultramafic rocks occur as lenses within Precambrian granite gneiss, which showing dominantly tectonic lines of NNE directions as well as east extensional area of the chinese collision belt between south and north China block(\ulcorner). This study regionally makes a comparative study of ultramafic rocks in the western part of the Gyeonggi Massif in Korea. (omitted)
Keywords
- ultramafic rocks, peridotite(PD);
- partly serpentinized peridotite(PSP);
- serpentinite(SP);
- rare earth element(REE);
- Gyeonggi Massif