摘要
狮子山矿田是铜陵地区乃至长江中下游地区最为重要的矿田之一。矿田内矿床众多,矿床类型多样,可以将它们划分为斑岩型、矽卡岩型、热液型、层控矽卡岩型、层控型与风化淋滤型矿床。本文对这些矿床类型的矿床形成机理做了粗浅探讨,以便更深入地了解其成因。
The Shizishan ore field is one of the most important ore fields in the Tongling area and even in the mid-lower Yangtze River reach.In the field there are numerous ore deposits,which can be classified into porphyry,skarns,hydrothermal,strata-bound skarns,strata-bound,weathered-eluvial types.This paper discussed the forming mechanism of these types of deposits for further understanding their origins.
出处
《安徽地质》
2011年第2期114-118,共5页
Geology of Anhui
关键词
狮子山矿田
矿床类型
形成机理
Shizishan ore field
ore deposit type
forming mechanism
