A Petrological and Geochemical Study of Granites in the Cheju Island

제주도에서 산출되는 화강암에 관한 연구

  • 안건상 (조선대학교 사범대학 지구과학과) ;
  • 이현구 (충남대학교 자연과학대학교 지질학과) ;
  • 임현철 (한국자원연구소 환경지질부)
  • Received : 1995.08.19
  • Published : 1995.10.30

Abstract

A granite drilling core (-1200 m) obtained near the Majang cave in east part of the Cheju island. The rock is pinksh in color and has miarolitic cavities. It is coarse-grained rock and consists of quartz, plagioclase, alkali feldspar, biotite and magnetite. The rock shows characteristically micrographic texture. The alkali feldspar is subhedral to anhedral and generally interstitial grains and fonns micrographic texture. K/Ar age of alkali feldspar in the core specimen is $58.14{\pm}1.4Ma $ (early Tertiary). The age, rock features and whole rock chemistry of the rock has strong resemblance to micrographic granites, so called "masanite", in southeastern part of the Korean peninsular. The granitic fragments from drilling core (- 920 m) obtained in Jungmun area in south part of the Cheju island consist of quartz, plagioclase, alkali feldspar and biotite. The fragments in the Jungmun area are similar to granitic xenolith near the Cheju city for the absence of micrographic texture and different alkali feldspar.

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