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NTIS 바로가기암석학회지 = The journal of the petrological society of korea, v.28 no.4, 2019년, pp.347 - 357
류충렬 (한국지질자원연구원 국토지질연구본부) , 천영범 (한국지질자원연구원 국토지질연구본부)
The main fault zone of the Yangsan Fault, located in the southeastern part of the Korean peninsula, is newly found at the Cheonjin-ri, Dudong-myeon, Ulju-gun, Ulsan, Korea. About 100 wide fault zone exposed along the Guryangcheon stream strikes N-S and dips over 70° toward east. The main faul...
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핵심어 | 질문 | 논문에서 추출한 답변 |
---|---|---|
양산단층의 특징은? | 양산단층은 연장 200 km 이상이며, 수 km 폭의 단층대와 20-35 km의 우향의 주향이동변위가 보고된바 있다(e.g. | |
구룡천 하상의 양산단층대 노두의 특징은? | 이번에 천전리에서 확인된 구룡천 하상의 양산단층대 노두는 양산단층곡의 거의 중심부에 발달하고 있으며, 단층대 폭이 100 m 내외의 심한 단층비지대와 각력대 그리고 단층파쇄대로 이루어져 있어, 주 단층대로 판단된다. 또한 주단층대의 중심부 일대에 분포하는 제4기 역층을 변형 또는 변위시키고 있어, 경주-언양 구간에서 제4기 단층으로 처음 확인되었던 신흥단층(Ryoo et al., 2003, 2006; Kang and Ryoo, 2009)에서 논의된 제4기 운 동의 존재와 같이 동측이 서쪽으로 올라탄 역단층 운동을 보임이 특징적이다. 이미 확인된 남측의 신흥단층이나 이번에 발견된 북쪽의 소위 제4기 ‘천전단층’의 발달특성으로 미루어 양산단층대를 따른 제4기 단층은 주로 양산단층대의 주 단층대의 단층핵 부분 일대가 재활동한 것일 가능성이 매우 높음을 지시하며, 향후 활성단층을 추적하는데 중요한 지표가 될 것으로 판단된다. | |
양산단층에서 단층대의 관찰과 연구가 어려운 이유는? | 1). 그러나 양산단층을 따라 대부분 제4기 퇴적층 피복되어져 있으며, 또한 부산, 양산, 울산, 경주, 포항 등 도시화 된 구간이 많아 단층의 내부변형을 파악하기 위한 주요 단층대의 관찰과 연구가 쉽지 않다(Fig. 1). |
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