摘要
本文根据归来庄金矿矿床特征，结合区域地球化学统计资料及中南、西南地区同类地层的含金性，运用“三源成矿”理论综合分析后认为：归来庄金矿是受寒武—奥陶系矿源层控制的层控金矿床。
This paper suggests that Guilaizhuang gold deposit is a stratabound one controlled by the Cambrian-Ordovician source beds according to its geological features,tegional geochemical statistical data and gold abundance of the strata ,as compared to that of the same kind of strata in central and south-west china,and to the theory of“three-resources forming ares”as well.
出处
《山东地质》
1994年第2期34-40,共7页
Geology of Shandong
