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NTIS 바로가기암석학회지 = The journal of the petrological society of korea, v.21 no.2 = no.68, 2012년, pp.151 - 171
The Permo-Triassic Songrim orogeny in the Korean peninsula was a major tectonic event involving complicated continental collisions at the eastern margin of Eurasia. Based on the previous studies on the metamorphic and deformations features of the Songrim orogeny, this paper presents metamorphic and ...
핵심어 | 질문 | 논문에서 추출한 답변 |
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태백산분지의 광역적인 주요 지질구조는 무엇인가? | 태백산분지의 광역적인 주요 지질구조는 N-S에서 NE-SW 방향(남동방향의 vergence)의 스러스트 단층과 습곡이다(Fig. 1). | |
석탄기 후기에서 삼첩기 초기동안 퇴적된 평안누층군은 무엇으로 구성되는가? | 1). 석탄기 후기에서 삼첩기 초기동안 퇴적된 평안누층군은 규산염질 쇄설성 퇴적암류와 소규모로 협재된 탄산염암으로 구성된다. 태백산 분지에서 평안누층군은 부정합관계로 조선누층군(캠브리안-오르도비스기) 상부에 놓여있으며, 주 구성 암석은 사암과 셰일이며 소규모로 역암, 탄층 그리고 석회암이 협재된다. | |
Kim et al. (1994)이 구분한 스러스트 단층의 두 가지 그룹은? | (1994)은 이들 스러스트 단층을 2가지 그룹으로 구분하였다. 첫 번째 그룹은 송림조산운동과 연관된 삼첩기 중기 스러스트이고, 두 번째는 대보조산운동과 관련된 쥬라기 중기스러스트이다(Choi et al., 1998; Hwang, 1998). |
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