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NTIS 바로가기자원환경지질 = Economic and environmental geology, v.47 no.1, 2014년, pp.29 - 38
정동훈 (연세대학교 지구시스템과학과) , 송윤구 (연세대학교 지구시스템과학과) , 박창윤 (연세대학교 지구시스템과학과) , 강일모 (한국지질자원연구원) , 최성자 (한국지질자원연구원)
Recently developed illite-age-analysis (IAA) approach has been applied to determine the multiple events for the Singal and Wangsukcheon faults in the Chugaryeong fault belt, Korea. Fault reactivated events during Late Cretaceous to Paleogene events(
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핵심어 | 질문 | 논문에서 추출한 답변 |
---|---|---|
추가령단층대는 무엇을 포함하는가? | 추가령단층대는 추가령을 중심으로 발달된 일련의 단층군으로 정의되며, 추가령단층, 예성강단층, 동두천 단층(Kim, 1973), 대광리단층, 동송단층(Kim et al., 1984), 포천단층, 왕숙천단층, 신갈단층 등을 포함한다 (Fig. 1). | |
Lee et al.은 추가령단층대의 추가령단층선과 예성강단층선을 합하여 무엇을 제안하였는가? | (2000)은 추가령단층과 예성강단층을 한반도를 북동-남서 방향으로 가로지르는 지구조적 규모의 1등급 단층으로 분류하고 이들을 추가령-예성강 단층대로 묶은 바 있으며, Lee et al.(2001)은 추가령단층선과 예성강단층선을 합하여 추가령단층계(Fault system)를 제안하였다. 그러므로 추가령단층계는 예성강단층대와 추가령단층대를 합한 단층계로 정의된다(Choi et al. | |
한반도의 화강암 및 화산암은 언제부터 형성되었는가? | 한반도는 백악기부터 제3기까지 이어진 불국사 조산 운동으로 지속적인 마그마의 천부관입 및 분출이 이어져 다양한 시기의 불국사 화강암 및 화산암이 생성되었다. 이 시기 화성암의 관입 및 분출시기에 대한 많은 연대측정 연구결과가 나오면서 불국사 조산운동으로 인한 화성활동이 약 150~40 Ma 까지 지속적으로 이어졌음이 밝혀졌다 (Cheong and Kim, 2012 등). |
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