摘要
云县邦东矿区铜铅矿体产于响水—邦东背斜南部倾没端、轴部断裂F1的旁侧,次级构造的交互部位是矿体的富集中心。F1是矿区的主要含矿和导矿构造,严格控制着矿床的展布,该断裂带及旁侧是下步工作的重要找矿靶区。
The Cu-Pb ore body of Bangdong orefield in Yunxian County is beside the axial fault F1 at S plunging end of Xiangshui—Bangdong anticline.The concentration center is at the intersecting part of secondary structure.F1 is the main ore-bearing and ore-transference structure,which close controls the distribution of ore deposit.The next important ore prospecting target is this fault zone and its surrounding area.
出处
《云南地质》
2011年第4期407-410,414,共5页
Yunnan Geology
关键词
玄武岩型矿床
构造、地层控矿
热液蚀变
前景分析
云县邦东
Ore Deposit of Basalt Type
Ore Control of Structure and Bed
Hydrothermal Alteration
Potentiality Analysis
Bangdong
Yunxian
