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NTIS 바로가기암석학회지 = The journal of the petrological society of korea, v.23 no.3, 2014년, pp.197 - 208
Zircon separated from a biotite schist of the Guryong Group in Odesan area, eastern part of the Gyeonggi Massif in Korea were analysed for SHRIMP U-Pb ages. CL images display composite core-rim structures of the zircon, indicating an in-situ overgrowth of zircon through a high-grade metamorphism. Th...
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핵심어 | 질문 | 논문에서 추출한 답변 |
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미그마타이트질 편마암을 구성하는 광물은 무엇인가? | (1997)는 반상변성질 편마암 및 미그마타이트질 편마암과 이에 렌즈상으로 소규모 협재하는 규암, 각섬암, 결정질석회암과 우백질 편마암을 오대산편마암복합체로 명명한 바 있다. 미그마타이트질 편마암은 주로 석영, 사장석, 퍼다이트, 흑운모로 구성되고, 변성도에 따라 석류석, 근청석, 규선석, 백운모, 스피넬 등을 포함한다(Kwon et al., 1997). | |
구룡층군이 처음 명명된 도폭은 무엇인가? | 구룡층군은 1:50,000 지질도 현리 도폭에서 처음 명명되었다(Kim et al., 1975b). | |
경기육괴 오대산 지역의 기저를 이루는 암종은 무엇인가? | 오대산 지역은 이질 기원인 고원생대 미그마타이트질 편마암과 화강암류가 기저를 이루며, 시대 미상의 구룡층군, 트라이아스기의 맨거라이트(mangerite), 쥬라기의 화강암류와 백악기의 퇴적층이 분포한다(Fig. 1) (Kim et al. |
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