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NTIS 바로가기자원환경지질 = Economic and environmental geology, v.52 no.5, 2019년, pp.427 - 448
권이균 (공주대학교 지질환경과학과) , 권유진 (공주대학교 지질환경과학과) , 여정민 (공주대학교 지질환경과학과) , 이창윤 (한국지질자원연구원 석유해저연구본부)
This study reconstructed the paleoenvironments and paleogeography of the Taebaeksan Basin, through a review of the previous researches on sedimentology, paleontology and stratigraphy. This study also carried out a sequence stratigraphic analysis on regional tectonism and sea-level fluctuations on th...
핵심어 | 질문 | 논문에서 추출한 답변 |
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태백산분지의 위치와 특징은? | 태백산분지는 한반도 중동부에 위치하는 고생대 퇴적분지이며, 북동쪽으로 부채꼴 모양으로 넓어지는 형태를 가지고 있다(Fig. 1A). 태백산분지는 남동쪽으로 영남육괴의 선캠브리아기 화강편마암, 남서쪽으로는 옥천변성대의 변성퇴적암, 북서쪽으로는 선캠브리아기 화강편마암과 경계를 이루고 있다. 북동쪽의 경계는 다양한 시기와 규모의 화성암 관입체에 의해 선캠브리아기 화강편마암과의 경계가 불분명하다(Chough et al.,2000)(Fig. | |
태백산분지의 전기 고생대 퇴적체의 분포지역은 어떻게 나누어지는가? | 태백산분지 전기 고생대 퇴적체의 분포지역은 크게 태백, 정선-평창, 영월-제천, 문경 지역으로 나뉘어진다. 태백층군은 태백 지역에 분포하고 있으며, 동-서 방향으로 발달한 백운산 향사대를 축으로 지향사 구조를 보이고있다(Chough et al. | |
태백층군을 구성하는 주요 암상은 어떻게 구분되는가? | 2). 주요 구성 암상은 조립질 규산쇄설성 퇴적암(장산/면산층, 동점층), 세립질 규산쇄설성 퇴적암(묘봉층, 세송층, 직운산층), 탄산염-규산쇄설성 퇴적암 복합체(세송층, 화절층, 두무골층), 조하대 탄산염암(대기층 하부, 막골층하부), 조상대 탄산염암(대기층 중상부, 막골층 상부, 두위봉층)으로 구분된다. |
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