摘要
八里桥铅锌多金属矿位于将乐—宁化钨、锡多金属成矿带上,产于三叠系下统溪口组地层中,矿体呈似层状—透镜状,赋存于北东向含矿断裂与矽卡岩或大理岩的相交复合部位,属于矽卡岩—热液充填型脉状铅锌(铁)多金属矿床。
Baliqiao lead-zinc polymetallic deposit which is located in Jiangle-Ninghua W-Sn polymetallic mineralization zone occurs in the lower Triassic Xikou formation. The ore bodies as lens or stratified are hosted in the conjunction between NE-striking mineralization-related faults and skarn or marble, so the deposit in genesis belongs to skarnhydrothermal filling vein-like lead-zinc （iron） polymetallie deposit.
出处
《资源与产业》
2008年第6期119-124,共6页
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