Geological Structure Features and Prospecting Direction of the Lobe Iron Deposit , Cameroun
详细信息
- 责任者：Wang Fenghua (North China Engineering Investigation Institute Limited Company ; Shijiazhuang 050021 ; China) ; Lin Bin
- 刊名：Geological Survey and Research
- 出版年：2011
- 卷期：34(3)
- 关键词：铁矿 ; iron ores ; 喀麦隆 ; Cameroon
- 页码：p.210-214
- 图表：3 illus., 6 refs.
- 分类号：1001
- issnNo：ISSN1672-4135
- isbnNo：CN12-1353/P
摘要
Cameroun Lobe iron deposit lies in the Archean strong metamorphic area,structurally located in the west limb of the east anticline which belongs a one-synclinal-two-anticlinal mulitple fold. authors analyse the structure of this deposit and suggest that the ore-control structure is composite syncline structure which is resulted from the superimpositions of multiple geological structures,the magnetite-quartzite occurs in the core part with the amphibolite and gneiss in two wings. Based on the composite syncline core ore-control regularity,the most fovorable mineralization position is delineated,which lays a foudation for the next geological prospecting in the Cameroun Lobe Iron deposit.
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