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NTIS 바로가기자원환경지질 = Economic and environmental geology, v.52 no.6, 2019년, pp.541 - 554
장이랑 (한국지질자원연구원 국토지질연구본부) , 정희준 (연세대학교 지구시스템과학과)
The Taebaeksan Zone of the Okcheon Belt is a prominent fold-thrust belt, preserving evidence for overlapped polyphase and diachronous orogenic events during crustal evolution of the Korean Peninsula. The Pyeongchang-Jeongseon area of the northwestern Taebaeksan Zone is fault-bounded on the western J...
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핵심어 | 질문 | 논문에서 추출한 답변 |
---|---|---|
옥천대의 구분 방식은? | 한반도 중남부 지역에 북동-남서 방향으로 발달하고 있는 옥천대는 주로 선캠브리아 시대 편마암 복합체로 구성된 경기육괴 및 영남육괴와 각각 북서부와 남동부 경계를 이루며, 북동부의 태백산지역(TaebaeksanZone)과 남서부의 옥천지역(Okcheon Zone)으로 구분된다(e.g. | |
평창지역의 지질구조의 연구가 구조진화를 이해하는데 중요한 이유는? | 최근 평창지역 서쪽의 주천지역을 중심으로 클리페형태의 기반암 단층에 대한 구조기하학적 형태 및 키네마틱스 연구가 수행된 바 있으며(Kihm et al.,2010; Lee, 2016), 남쪽의 영월지역에서는 조선누층군을 반복시키는 수 매의 남-북 방향 트러스트들이 듀플렉스 트러스트시스템으로 새롭게 해석된 바 있다(Janget al., 2015). | |
옥천대 태백산지역은 무엇인가? | 옥천대 태백산지역은 한반도의 지각 진화 과정 동안 중첩된 다변형 조산운동의 증거를 보존하고 있는 주요 습곡-단층대 가운데 하나로, 북서부의 평창-정선지역을 중심으로 서쪽의 주천지역 및 남쪽의 영월지역이 각각 단층 경계로 구분되며, 층서 및 지질구조에 있어서 차이를 보인다. 본 논문에서는 북서부 태백산지역에 분포하는 고생대 지층들의 이러한 지역적 차이와 지구조 운동과의 연관성을 이해하기 위해 구조기하학적 형태 해석 연구를 수행하였다. |
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