Geochemistry for the Serpentinites of the Igneous and Metamorphic Origins

  • Song, Suck-Hwan (Joongbu University, Dept. of Environmental Engineering) ;
  • Park, Seong-Gyu (Korea University, Dept. of Earth and Environmetal Science) ;
  • Oh, Chang-Whan (Chonbuk National University, Dept. of Earth and Environmental Science) ;
  • Seo, Ji-Eun (Korea University, Dept. of Earth and Environmental Sciences)
  • Published : 2003.04.01

Abstract

Several masses of the alpine type ultramafic rocks are found within the Precambrian Kyeonggi gneiss complex, western part of Chungnam province. They occur as discontinuous isolated lenticular bodies along the fault line(NNE direction), dominant tectonic directions of Kyeonggi gneiss complex. The ultramafic rocks occur as fault contacts with the adjacent Precambrian metamorphic and metasedimentary rocks. (omitted)

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