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Elucidation of the Enrichment Mechanism of the Naturally Originating Fluorine Within the Eulwangsan, Yongyudo: Focusing on the Study of the Fault zone

용유도 을왕산 자연기원 불소의 부화기작 규명: 단층대 연구를 중심으로

  • Lee, Jong-Hwan (Department of Geology and Research Institute of Natural Science (RINS), Gyeongsang National University (GNU)) ;
  • Jeon, Ji-Hoon (Department of Geology and Research Institute of Natural Science (RINS), Gyeongsang National University (GNU)) ;
  • Lee, Seung-Hyun (Department of Geology and Research Institute of Natural Science (RINS), Gyeongsang National University (GNU)) ;
  • Kim, Soon-Oh (Department of Geology and Research Institute of Natural Science (RINS), Gyeongsang National University (GNU))
  • 이종환 (경상국립대학교 자연과학대학 지질과학과 및 기초과학연구소) ;
  • 전지훈 (경상국립대학교 자연과학대학 지질과학과 및 기초과학연구소) ;
  • 이승현 (경상국립대학교 자연과학대학 지질과학과 및 기초과학연구소) ;
  • 김순오 (경상국립대학교 자연과학대학 지질과학과 및 기초과학연구소)
  • Received : 2022.08.26
  • Accepted : 2022.09.20
  • Published : 2022.09.30

Abstract

In addition to anthropogenic origins, fluorine (F) is naturally enriched in rocks due to geological events, such as magma dissemination, hydrothermal alteration, mineralization, and fault activities. Generally, it has been well known that F is chiefly enriched in the region of igneous and metamorphic rocks, and biotite granite was mostly distributed in the study area. The F enrichment mechanism was not sufficiently elucidated in the previous studies, and the study on a fault zone was conducted to reveal it more precisely. The mineral composition of the fault zone was identical to that of the Eulwangsan biotite granite (EBG), but they were quantitatively different between the two areas. Compared with the EBG, the fault zone showed relatively higher contents of quartz and F-bearing minerals (fluorite, sericite) but lower contents of plagioclase and alkali feldspar. This difference was likely due to hydrothermal mineral alterations. The results of microscopic observations supported this, and the generation of F-bearing minerals by hydrothermal alterations was recognized in most samples. Accordingly, it might be interpreted that the mineralogical and petrological differences observed in the same-age biotite granite widely distributed in the Yongyudo was caused by the hydrothermal alterations due to small-scale geological events.

불소는 인위적 기원 외에 마그마 분화작용, 열수변질작용, 광화작용, 단층 활동과 같은 지질학적 기원에 의해 자연적으로 암석 내 부화될 수 있다. 일반적으로 화성암 및 변성암이 분포하는 지역에서 고농도의 불소가 산출되는 것으로 알려져 있으며, 연구지역은 흑운모화강암이 주로 분포하는 지역이다. 그러나 선행연구에서 자연기원 불소의 부화기작에 대한 규명이 부족했고 이를 보다 명확히 규명하기 위해 단층대에 대한 연구를 수행하였다. 을왕산 흑운모화강암과 단층대 암석의 구성 광물은 동일하지만 정량적인 차이가 나타난다. 석영과 불소함유광물(형석, 견운모 등)은 높은 함량으로 존재하며, 사장석과 알칼리장석은 낮은 함량으로 존재한다. 이러한 차이는 열수에 의한 광물의 변질작용 때문인 것으로 판단된다. 현미경 관찰 결과 또한 열수에 의한 불소함유광물의 생성이 대부분의 시료에서 관찰된다. 따라서 용유도 등지에 넓게 분포하는 동일한 연령의 흑운모화강암의 암석·광물학적인 차이는 소규모 지질학적 사건에 의한 열수변질작용에 의한 것으로 해석할 수 있다.

Keywords

Acknowledgement

This research was supported by Korea Environment Industry and Technology Institute (KEITI) through the Subsurface Environment Management (SEM) Project funded by Korea Ministry of Environment (MOE) (grant number: 2018002440002).

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