蛇紋石의 滑石化過程에 關한 硏究

• 영문명: A study on talc mineralization of serpentine
• 발행기관: 대한자원환경지질학회
• 저자명: Jeong Mahn Chi(池楨蔓) Kyu Bong Kim(金圭鳳)
• 간행물 정보: 『자원환경지질』10권 2호, 67~74쪽, 전체 8쪽
• 주제분류: 자연과학 > 지질학
• 파일형태: PDF
• 발행일자: 1977.06.30

영문 초록

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.

목차

Abstract

1. 序言

2. 地質

3. 鑛床

4. 鑛化作用

5. 結論

參考文獻