安徽铜陵狮子山矿田矿床形成机理探讨  

DISCUSSION OF DEPOSIT-FORMING MECHANISM OF THE SHIZISHAN ORE FIELD,TONGLING,ANHUI

作　　者：储国正[1] 

机构地区：[1]安徽省地质矿产勘查局,安徽合肥230001

出　　处：《安徽地质》2011年第2期114-118,共5页Geology of Anhui

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.

关 键 词：狮子山矿田 矿床类型 形成机理 

分 类 号：P612[天文地球—矿床学]