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RISSA magnetic survey was conducted in detail at Song Chi mine area where magnetic anomalies were found by magnetic reconnaissance work. A detailed magnetic survey was made on a grid system of 15m×15m in an area of 270m×360m around the Song Chi anomaly...
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松峙 磁鐵鑛床의 磁力調査 硏究 = A study on the magnetic prospecting in Song Chi magnetite deposits, Sung Ju, Jeonnam, Korea
한글로보기https://www.riss.kr/link?id=A30062940
- 저자
- 발행기관
- 학술지명
- 권호사항
-
발행연도
1984
-
작성언어
Korean
-
KDC
321.3
-
자료형태
학술저널
-
수록면
39-48(10쪽)
- 제공처
-
0
상세조회 -
0
다운로드
부가정보
다국어 초록 (Multilingual Abstract)
A magnetic survey was conducted in detail at Song Chi mine area where magnetic anomalies were found by magnetic reconnaissance work.
A detailed magnetic survey was made on a grid system of 15m×15m in an area of 270m×360m around the Song Chi anomaly.
A magnetic ore is formed as a dyke type in the porphyry, parallel to fault face and joint striking N 6 , N 56 W.
As result of this survey, the anomalous area is wide and magnetic intensity varied from 12,500r to -4,200r.
Ore bodies are consisted of 2 veins, profiles A-A´, B-B´.
The trenching should be done to identify the ore location being at sites, O-O, S_6-W_8.
Two bore holes are recommended to be identify direction and location of ore body in the Song Chi anomalous zone.
A detailed magnetic survey was made on a grid system of 15m×15m in an area of 270m×360m around the Song Chi anomaly.
A magnetic ore is formed as a dyke type in the porphyry, parallel to fault face and joint striking N 6 , N 56 W.
As result of this survey, the anomalous area is wide and magnetic intensity varied from 12,500r to -4,200r.
Ore bodies are consisted of 2 veins, profiles A-A´, B-B´.
The trenching should be done to identify the ore location being at sites, O-O, S_6-W_8.
Two bore holes are recommended to be identify direction and location of ore body in the Song Chi anomalous zone.
A magnetic survey was conducted in detail at Song Chi mine area where magnetic anomalies were found by magnetic reconnaissance work.
A detailed magnetic survey was made on a grid system of 15m×15m in an area of 270m×360m around the Song Chi anomaly.
A magnetic ore is formed as a dyke type in the porphyry, parallel to fault face and joint striking N 6 , N 56 W.
As result of this survey, the anomalous area is wide and magnetic intensity varied from 12,500r to -4,200r.
Ore bodies are consisted of 2 veins, profiles A-A´, B-B´.
The trenching should be done to identify the ore location being at sites, O-O, S_6-W_8.
Two bore holes are recommended to be identify direction and location of ore body in the Song Chi anomalous zone.
목차 (Table of Contents)
- Ⅰ. 序言
- Ⅱ. 位置 및 交通
- Ⅲ. 地質槪要
- Ⅳ. 鑛 床
- Ⅴ. 磁力調査
- Ⅰ. 序言
- Ⅱ. 位置 및 交通
- Ⅲ. 地質槪要
- Ⅳ. 鑛 床
- Ⅴ. 磁力調査
- 1) 使用機器
- 2) 調査方法
- 3) 調査面積
- 4) 測定値處理
- 5) 測定結果
- Ⅵ. 磁探結果 解析
- Ⅶ. 結言
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