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학술저널

蛇紋石의 滑石化過程에 關한 硏究

A study on talc mineralization of serpentine

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Biggest talc deposits of South Korea, localized in Choong-Chung-Nam-do, are known as a products of hydrothermal metamorphism of serpentine. From studying mineral paragenesis and localization, three types of talc mineralization is presumed as follows: 1) Extended tale mineralization from autometamorphiam (serpentinization) of ultra-basic igneous rocks, 2) Schistose talc rock as green schist facies of regional metamorphism and 3) Late hydrothermal mineralization and purification of serpentine and pre-existing low grade ores.

Abstract

1. 序言

2. 地質

3. 鑛床

4. 鑛化作用

5. 結論

參考文獻

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