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40Ar-39Ar Age Determination for the Quaternary Basaltic Rocks in Jeongok Area

전곡 지역 제4기 현무암질 암석의 40Ar-39Ar 연대 측정

  • Kim, Jeongmin (Division of Earth and Environmental Science, Korea Basic Science Institute) ;
  • Choi, Jeong-Heon (Division of Earth and Environmental Science, Korea Basic Science Institute) ;
  • Jeon, Su In (Division of Earth and Environmental Science, Korea Basic Science Institute) ;
  • Park, Ul Jae (Radioisotope Research Division, Korea Atomic Energy Research Institute) ;
  • Nam, Seong Soo (Radioisotope Research Division, Korea Atomic Energy Research Institute)
  • 김정민 (한국기초과학지원연구원 환경과학연구부) ;
  • 최정헌 (한국기초과학지원연구원 환경과학연구부) ;
  • 전수인 (한국기초과학지원연구원 환경과학연구부) ;
  • 박울재 (한국원자력연구원 동위원소이용연구본부) ;
  • 남성수 (한국원자력연구원 동위원소이용연구본부)
  • Received : 2014.10.31
  • Accepted : 2014.12.18
  • Published : 2014.12.31

Abstract

Quaternary basaltic rocks occur as volcanic plateau and/or river cliff in the watershed area of Hantan River in Jeongok, central Korea. We measured $^{40}Ar-^{39}Ar$ ages for the basaltic rocks from Jeongok area using the multi-collector noble gas mass spectrometer and laser heating device introduced for the first time in Korea. The basaltic rocks from the river cliff in Eundae-ri area show the systematic change in $^{40}Ar-^{39}Ar$ ages from $0.54{\pm}0.07Ma$ through $0.48{\pm}0.01Ma$ to $0.12{\pm}0.01Ma$ toward the top. The other sample from Jeongok-ri area yields the age of $0.43{\pm}0.04Ma$. This results suggest that there might be a episodic volcanic eruption between 0.12-0.54 Ma in Jeongok area.

한반도 중부 전곡 지역 한탄강 유역에는 제4기 시기에 분출한 현무암질 암석들이 화산대지 및 하식절벽으로서 분포한다. 국내 최초로 도입된 다검출기 불활성기체 질량분석기와 레이저 가열장치를 이용하여 전곡 지역에서 산출하는 현무암질 암석의 $^{40}Ar-^{39}Ar$ 연대를 측정하였다. 전곡읍 은대리 지역 하식절벽의 현무암들은 하부에서 상부로 가면서 $0.54{\pm}0.07Ma$, $0.48{\pm}0.01Ma$, $0.12{\pm}0.01Ma$의 연대를 나타내며 전곡리 지역의 현무암에서 $0.43{\pm}0.04Ma$의 연대가 얻어진다. 이 결과는 0.12-0.54 Ma 사이에 전곡 지역에 단속적인 화산암의 분출이 있었을 가능성을 시사한다.

Keywords

References

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