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전기 고생대 태백산분지의 분지 진화

Basin Evolution of the Taebaeksan Basin during the Early Paleozoic

자원환경지질 = Economic and environmental geology, v.52 no.5, 2019년, pp.427 - 448  

권이균 (공주대학교 지질환경과학과) ,  권유진 (공주대학교 지질환경과학과) ,  여정민 (공주대학교 지질환경과학과) ,  이창윤 (한국지질자원연구원 석유해저연구본부)

초록
AI-Helper 아이콘AI-Helper

본 연구는 최근 수행된 퇴적층서학 및 고생물학적 연구결과를 종합하고, 새롭게 분석된 자료를 보강하여, 전기 고생대 태백산분지의 고환경과 고지리를 복원하였다. 또한 순차층서학적 방법을 사용하여 조구조적 운동과 해수면 변동을 추적하여 종합적인 분지해석을 수행하였다. 태백산분지는 태백, 정선-평창, 영월-제천, 문경 지역에 넓게 분포하고 있으며, 암상 및 층서 특성에 따라 태백, 영월, 용탄, 평창, 문경 층군으로 구분되어 조사 및 연구가 진행되어 왔다. 태백산분지의 퇴적체는 탄산염암과 규산쇄설성 퇴적암이 혼합되어 있는데, 최근 쇄설성 퇴적물의 기원과 퇴적 연대에 대한 연구가 집중적으로 이루어졌다. 태백산분지에 공급되는 쇄설성 퇴적물의 근원지는 크게 곤드와나지괴와 한중지괴 기원지로 나누어진다. 태백산분지의 형성 초기에 태백대지와 정선-평창대지는 주로 한중지괴 기원지로부터 퇴적물을 공급 받았으며, 영월-제천 대지는 지리적 혹은 지형적 분리에 의해 한중지괴의 영향이 차단되고, 주로 곤드와나지괴 기원지로부터 퇴적층을 공급받았다. 쇄설성 저어콘 분석 결과는 중기 캠브리아 시기의 전 지구적 해수면 상승으로 인해 태백산분지 전체적으로 곤드와나지괴 기원의 퇴적물이 공급되었으며, 한중지괴 기원의 퇴적물은 공급이 멈추었음을 보여주고 있다. 한편, 태백산분지의 북쪽에 분포하는 정선-평창 대지의 퇴적체는 전기 캠브리아기와 오르도비스기 지층사이에 부정합 관계를 보여주고 있는데, 이것은 중기-후기 캠브리아 시기에 전 지구적 해수면 상승효과를 상쇄할 규모의 지역적 융기 운동이 정선-평창 대지 인근에서 존재했음을 보여준다. 이러한 융기운동은 최후기 캠브리아기와 최전기 오르도비스기에 태백산 분지 전역으로 확대되었다. 최전기 오르도비스기 이후에 태백산 분지는 조구조적으로 안정화되었고, 분지 전체적으로 해수면이 상승하면서 천해 탄산염 퇴적환경이 조성되어 두꺼운 탄산염암이 형성되었다. 전기 고생대 태백산분지의 퇴적작용은 후기 오르도비스기 동안 태백산분지와 한중지괴 전역에서 발생한 융기운동에 의해 종료되었다.

Abstract AI-Helper 아이콘AI-Helper

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...

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표/그림 (10)

질의응답

핵심어 질문 논문에서 추출한 답변
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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