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- W2022909198 abstract "대전지역은 우리나라에서 고함량 우라늄 지하수에 대한 우려가 높은 지역이다. 대전의 복운모 화강암 지역의 지하수에서 우라늄의 함량이 높지만 복운모 화강암에서 우라늄 함량은 화강암의 세계 평균치 보다 낮고 우라늄 광물의 산출이 아직 보고되지 않았다. 이 연구는 우라늄의 근원암과 지하수에 우라늄을 공급할 수 있는 우라늄 광물의 산출상태를 규명하는데 있다. 이를 위해 지표 방사능 탐사와 전자현미경을 이용한 광물학적 연구를 수행하였다. 우라늄 이상은 화강암맥과 열수변질된 화강암에서 측정되었다. 우라늄 이상을 보이는 화강암맥은 복운모 화강암과 운모-편암의 경계부에 발달한다. 복운모 화강암 내의 우라늄 이상대는 열극대를 따라 석영 세맥이 충진한 열수변질대에 발달한다. 우세한 열수변질작용은 칼륨 변질작용과 프로필리틱 변질작용이다. 우라니나이트는 화강암맥과 열수변질된 화강암에서 공통적으로 산출되는 우라늄 광물이며, 코피나이트와 우라노페인은 열수변질 화강암에서 산출된다. 모든 우라늄 광물은 백운모, 녹니석, 녹염석, 방해석 등과 같은 열수변질 광물과 밀접히 공생한다. 우라늄 광물이 산출되는 화강암맥과 열수변질된 화강암은 대전지역 지하수 내 우라늄의 주요 기원암으로 판단된다. Some groundwater in Korea contains high U concentrations, especially where two-mica granite occurs in the Daejeon area. The elemental U in the two-mica granite is lower than that in normal granites elsewhere in the world, and U-minerals have yet to be reported in the two-mica granite in the Daejeon area. This study focuses on investigating the occurrence of U-minerals serving as the U source in groundwater. In situ gamma ray spectrometry and mineralogical analyses using EPMA were performed. U-count anomalies were identified in a granitic dyke and in hydrothermally altered granite. Uraniferous granitic dykes occur along the contact zone between the two-mica granite and mica-schist. The uraniferous parts within the two-mica granite are developed in the hydrothermally altered zone, which contains numerous quartz veinlets within a fracture zone. Hydrothermal alteration is dominated by potassic and prophylitic alteration. Uraninite is a common U-mineral in granitic dykes and hydrothermally altered granite. Coffinite and uranophane occur in the hydrothermally altered granite. All of these U-minerals are commonly accompanied by hydrothermal alteration minerals such as muscovite, chlorite, epidote, and calcite. It is concluded that granitic dyke and hydrothermally altered granite are the main source rocks of U in groundwater." @default.
- W2022909198 created "2016-06-24" @default.
- W2022909198 creator A5065289926 @default.
- W2022909198 date "2013-12-31" @default.
- W2022909198 modified "2023-10-03" @default.
- W2022909198 title "Occurrence of U-minerals and Source of U in Groundwater in Daebo Granite, Daejeon Area" @default.
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- W2022909198 doi "https://doi.org/10.9720/kseg.2013.4.399" @default.
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