摘要
研究区金矿床位于胶莱盆地东北缘,牟乳成矿带西侧,是郯庐断裂带重要分支-郭城断裂带内的主要矿床之一,其矿体严格受NNE和NEE向次级压扭性断裂控制。本文对研究区矿床成矿物质来源、矿床成因模式等特征进行了研究,简要的总结了其成矿过程。
The studied ore deposit lies in the northeast fringe of the Jiao-Lai basin, on the west flank of the Mo- Ru metallogenic belt, as one of major ore deposits in the Guocheng fault zone, an important branch of the Tan- Lu fault belt. The ore body is precisely controlled by NNE and NEE secondary compresso-shear faults. This paper discussed the ore-forming material source, genesis model of the deposit and summarized its mineralization process.
出处
《安徽地质》
2016年第3期194-197,共4页
Geology of Anhui
关键词
金矿床
成矿物质来源
成矿流体
成因模式
gold deposit
ore-forming material source
ore-forming fluid
genesis model
