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NTIS 바로가기암석학회지 = The journal of the petrological society of korea, v.22 no.3, 2013년, pp.235 - 249
김종선 (부산대학교 지구환경시스템학부) , 조형성 (부산대학교 지구환경시스템학부) , 김홍균 (한국건설기술연구원 Geo-인프라연구실) , 손문 (부산대학교 지구환경시스템학부)
The Gusandong Tuff (Kusandong Tuff), known as a very significant key bed in the Cretaceous Gyeongsang Basin, is divided into (1) Northern Gusandong Tuff (NKT), (2) Southern Gusandong Tuff (SKT), and (3) Sinsudo Tuff, which were derived from different vents. In order to suggest their more accurate er...
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핵심어 | 질문 | 논문에서 추출한 답변 |
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한반도의 백악기 지층의 분포는 어떠한가? | 한반도의 백악기 지층은 호남과 옥천대 일부 지역에 소규모로 분포하는 것을 제외하면 대부분 한반도 남동부의 경상분지에 집중되어 분포한다(Fig. 1a). | |
구산동응회암의 층서적 특징은 무엇인가? | 층서적으로 구산동응회암은 의성지괴에서는 하양층 군의 사곡층과 춘산층의 경계에서 나타나며, 밀양지괴에서는 함안을 기점으로 북쪽으로는 진동층과 함안층의 경계에서 그리고 남쪽으로는 함안층의 중상부에 출현한다(Chang et al., 1998; Jeong et al. | |
경상분지 퇴적층의 화산기원 물질을 대상으로 절대연령 측정에 의한 층서대비 연구가 활발하게 된 배경은 무엇인가? | 경상분지의 지층들은 측방으로 상변화가 심하고, 층서대비에 필요한 건층(key bed)의 불연속성과 화석의 부족으로 인해 지층들의 층위확립과 지괴간의 층서대비가 명확하게 이루어지지 못하고 있다. 또한, 분지충 전물이 대부분 비화산성 퇴적층들로 구성되어 있어 지층의 정확한 절대연령이 밝혀지지 못해 인접대륙과의 비교에도 어려움이 있다. 최근 이러한 문제점을 극복하기 위해, 경상분지 퇴적층의 화산기원 물질들을 대상으로 절대연령 측정에 의한 층서대비 연구가 활발히 진행되고 있다(Chang et al. |
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