Origin of the Magnetite-Bearing Amphibolites from the Yangyang Iron Mine, Korea: New Geochemical Data and Interpretation

양양(襄陽) 철광상(鐵鑛床)의 철(鐵)을 부존(賦存)하는 각섬석질암(角閃石質岩)의 성인(成因)

  • 소칠섭 (고려대학교 이공대학 지질학과) ;
  • 김상명 (고려대학교 이공대학 지질학과) ;
  • 손대성 (고려대학교 이공대학 지질학과)
  • Published : 1975.12.31

Abstract

The chemical similarity of the magnetite-bearing amphiboltes of the Yangyang iron mine to mixtures of sedimentary pelites and limestone or dolomite and to the Gyeonggi para-amphibolites (So, 1974) is consistently indicated by all the chemical data of the rocks. Eight amphibolite samples were each analyzed for 18 elements, by wet chemical and emission spectroscopic methods, and these chemical data were compared with the para-amphibolites from the Gyeonggi metamorphic complex. Petrography and oxidation ratios were also considered.

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