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석곡광산(石谷鑛山) 부근의 지질과 광화작용(鑛化作用)에 대하여
梁承榮,李倫鐘 慶北大學校 師範大學 1972 敎育硏究誌 Vol.14 No.-
The Seokgok Mine area, which is located in Dong-myun, Jungseon-gun, Kangwon-do, is composed of Pungchon limestone formation, Hwajeol formation, Dongjeom quartzite formation, Dumudong formation and Magdong limestone formation in ascending order, which are included in the so-called Great limestone Series, Cambro-Ordovician in age. The ore deposit is developed partially along the fracture in the Pungchon limestone formation. And its origin is considered as a filling replaced type. The shape of the ore body is very irregular and in which remains the non-replaced limestone relicts. Ore minerals are mainly galena, sphalerite, pyrite and chalcopyrite, which are associated with small amount of other sulfide minerals.