摘要
发现五个金矿体一个钒矿体,金矿受岩石建造及构造破碎蚀变带控制。可以划分出沉积成岩预富集期、构造热液改造期和表生氧化—次生富集成矿期三阶段,属热水沉积—构造热液再造层控矿床,矿体有向深部侧伏延伸趋势。
The Au deposit is controlled by rock formation and structural fracture alteration zone. 5 Au ore bodies and 1 V ore body have been discovered, which can be divided into 3 stages, ie, sedimentation diagenesis preliminary concentration, structure hydrothermal reformation and epigenetic oxidation - secondary concentration metallogenesis, and belong to the hydrothermal deposition - structure hydrothermal reformation stratabound deposit. The ore body has the trend of side pitching toward deep.
出处
《云南地质》
2013年第3期282-285,281,共5页
Yunnan Geology
关键词
层控金
钒矿
区域大断裂导矿
次级破碎带赋矿
侧状延深
陕西山阳夏家岩
Stratabound Au - V Deposit
Ore Transmission of Regional Megafault
Ore - Bearing of Secondary Fracture Zone
Side Pitching Extension toward Deep
Xiajiadian, Shanyang, Shanxi
