铁山岩体矿床成因类型再探  

The restudy on the genetic type of ore deposit of Tieshan rock body

作　　者：卢峰[1] 

机构地区：[1]湖北大学学报编辑部,湖北武汉430062

出　　处：《湖北大学学报（自然科学版）》2003年第3期271-276,共6页Journal of Hubei University：Natural Science

摘　　要："大冶式矽卡岩型"铜铁矿床成因类型,是世界上所有铜铁矿床成因类型中最著名的一种,它又以铁山岩体铜铁矿床为典型代表,并冠名"大冶式矽卡岩型".此次研究以地球化学方法为切入点,利用计算机数据统计分析手段,对已成定论的铁山岩体矿床成因类型进行再认识,作出了对铁山岩体矿床成因类型再分类.除主要有矽卡岩铜铁矿床外,还有大量的热液型矿床和少数淋积型矿床.The genetic type of iron and copper deposit of Daye-type skarn pattern is the most famous one of all the genetic type of iron and copper deposit in the world.It is represented by the iron and copper deposit of Tieshan rock body,and by the name of Daye-type skarn pattern.The research starts with its geochemical characteristics,applying numerical statistical analytical method,make a restudy on the genteic type of ore deposit of Tieshan rock body,and also reclassify it .

关 键 词：铁山岩体 矿床成因类型 铜铁矿床 大冶式矽卡岩型 地球化学 簇群分析 

分 类 号：P618.41[天文地球—矿床学] P618.31[天文地球—地质学]