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자원환경지질 = Economic and environmental geology, v.42 no.6, 2009년, pp.635 - 643
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In this paper, a Quaternary fault is described, which is developed in the mid-eastern part of Ulsan Fault Zone, near the southern Gaegok-ri, Oedong-eub, Gyeongju, Korea. The Gaegok 6 fault is developed along the contact between Early Tertiary granite and Quaternary gravel deposit overlying unconform...
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| 핵심어 | 질문 | 논문에서 추출한 답변 |
|---|---|---|
| 울산단층대 중동부의 동변인 경상북도 경주시 외동읍 개곡리 남부에서 제3기초의 화강암이 무엇을 경계로 접하고 있는가? | 울산단층대 중동부의 동변인 경상북도 경주시 외동읍 개곡리 남부에서 제3기초의 화강암이 제4기의 미고결 모래층이나 자갈층과 단층을 경계로 접하고 있다. 새로이 알려진 이 단층(개곡 6단층)은 $N02^{\circ}{\sim}22^{\circ}E$의 주향에 $45^{\circ}{\sim}80^{\circ}W$의 경사를 보인다. | |
| 경주시 외동읍 개곡리 일원의 지질의 특징은 무엇인가? | 경주시 외동읍 개곡리 일원의 지질은 제3기초 화강암과 안산암, 그리고 암맥 등이 발달하고 있으며, 제4기의 선상지 퇴적층이 이들을 부정합으로 덮고 있다(Jin et al., 1991; Chwae et al. | |
| 경주-울산 사이의 울산단층대에 존재하는 제4기 단층의 관찰에 한계가 있는 이유는 무엇인가? | 그러나 아직도 이들의 분포나 연장성으로 구분되는 기하학적인 발달 특성은 물론 운동학적이고 동력학적인 양상 및 단층운동시기와 이 일대에 자주 발생하는 지진활동과의 연관성에 대해 불확실한 점이 제기되고 있다. 이러한 문제점을 해결하기 위해서는 단층의 분포와 연장성을 찾는 것이나, 단층들이 대체로 불국사 산맥의 서편에 넓게 분포하는 충적선상지 퇴적층에 의해 덮여 있거나 단층면이 침식, 삭박되어 단층의 관찰에 한계가 있다(Fig. 1). |
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