摘要
以八卦庙金矿和八方山－ 二里河铅锌矿为例， 重点论述了凤太矿田金属矿床的主要特征， 并将其分为两个不同的成矿系列，即热水沉积型Ｐｂ、Ｚｎ （Ｃｕ） 成矿系列和热水沉积－岩浆热液叠加型金成矿系列。这两个成矿系列在成矿地质环境、含 （赋） 矿层特征、成矿物质来源、成矿作用方式等方面均有较大的差异。
The main metallogenic characteristics of Baguamiao gold deposit and Bafangshan-Erlihe Lead Zinc deposit in Fengtai Ore field are described with detailed data in this paper Comparing the two deposits, there are many differences between them Including the metallogenic environment, the source of metallogenic materials, the metallogenic ways and ore fluid, which indicated that all metal deposits in FengTai area can be divided two series: The Lead zinc metallogenic series and the gold metallogenic series
出处
《西北地质科学》
1999年第2期42-50,共9页
Northwest Geoscience
基金
西北有色地质勘查局人才培养基金
关键词
秦岭
金属成矿系列
热水沉积
岩浆热液
金属矿床
Qinling, Metal metallogenic series, Hydrothermal sediment, Magmatic hydrothermalism
