• 责任者：Lu Enlan (Fourth Geological Survey of Jilin Province ; Tonghua 134001 ; China) ; Gao Mingzhu
• 刊名：Jilin Geology
• 出版年：2012
• 卷期：31(2)
• 关键词：铁矿 ; iron ores ; 吉林 ; Jilin Province
• 页码：p.45-49
• 图表：2 illus., 1 table, 8 refs.
• 分类号：1001
• issnNo：ISSN1001-2427
• isbnNo：CN22-1099/P

Banshigou iron occurs in hornblende rock of the middle member of Late Archaean supracrustal rock, its protolyte is intermediate-basic eruptive rock. NEE synclinorium controls the orebody, the two slopes of synclinorium format the two ore-bearing zones of south and north, the location of them is consistent with that of magnetic anomaly, each sub-orebody in depth may successive, between sub-orebody and the others may exist concealed orebody by inference.