抱川鑛山의 地質鑛床

• 발행기관: 대한자원환경지질학회
• 저자명: 神田四男 柳炳和
• 간행물 정보: 『자원환경지질』2권 2호, 53~68쪽, 전체 16쪽
• 주제분류: 자연과학 > 지질학
• 파일형태: PDF
• 발행일자: 1969.06.30

영문 초록

Magnetite deposit of Pocheon Iron Mine is a contact replacement skarn deposit embedded in the carbonate rocks (limestone and dolomite) which are intruded by granite porphyry. The shape of ore bodies is sweet potato-like and/or irregular massive form; D-ore body, the biggest one is of 180m×40m×200m in size. The ore is in general of high grade. The location of the ore bodies is controlled by the fault which strikes north south and dips 60° to 70° to the west. A regular distribution of mineralized zones is recognized in order of outward (hanging wall side) from granite porphyry as follows; compact fine-grained skarn, limesilicates, magnetite ore body, marble, limesilicates, pyritized meta-sediments.

목차

Abstract

1. 緖言

2. 開發 槪要

3. 地質 및 鑛床

4. 鑛體에 關한 事項

5. 스카른과 金屬鑛物과의 關聯性

6. 鑛床의 配列狀態

附言