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NTIS 바로가기자원환경지질 = Economic and environmental geology, v.51 no.6, 2018년, pp.473 - 483
구효진 (경상대학교 지질과학과 및 기초과학연구소) , 장정규 (경상대학교 지질과학과 및 기초과학연구소) , 도진영 (경주대학교 고고인류미술사학과) , 정기영 (안동대학교 지구환경과학과) , 조현구 (경상대학교 지질과학과 및 기초과학연구소)
Green-blue coloured supergene minerals are covering host rocks along the gallery wall in the Gukjeon mine, a lead - zinc skarn deposit located in Miryang, Gyeongsangnam-do. These minerals have been described as azurite or malachite, but recent study recognized that the green minerals are devilline a...
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핵심어 | 질문 | 논문에서 추출한 답변 |
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경남 밀양시의 국전광산은 어떻게 만들어진 광산인가? | 4’’-129°55’10.4’’/N 35°28’00’’-35°30’00’’)은 채광과 휴광을 반복중인 납-아연 광산으로, 백악기 말 유천층군의 정각산층 내에 협재된 석회암이 불국사 관입암류인 흑운모화강암에 의해 교대작용을 받아 형성된 스카른 광상이다(Yang et al., 2010; Kwak et al. | |
국전광산의 석회암층 특징은 무엇인가? | , 2010). 석회암층은 유천도폭에서 층회암으로 기재되었으나(Hong et al., 1988), 전암분석 결과 석회암에 가까운 조성을 보여주고, 전형적인 석회암에 비해 CaO가 적고, SiO2의 함량이 높아 석회규산염암으로 제시되었다(Kwak et al., 2015). | |
밀양 지역의 암석 구성은 어떻게 되는가? | 밀양 지역은 진동층과 주사산 안산암질암인 안산암질암류가 하부를 구성하고 그 상부를 운문사 유문암질암으로 명명된 유문암질 화산암류가 분포하며 후기에 이를 관입한 화강암질암류로 구성된다(Hong et al.,1988; Kim et al. |
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