同位素地质在鄂东南铜铁矿床地质研究中的应用  

Application of Isotopes to the Geological Study on the Iron and Copper Deposits in Eastsouthern Hubei

作　　者：苏欣栋[1] 刘陶梅 

机构地区：[1]中南冶金地质研究所

出　　处：《地质与勘探》1994年第1期27-32,共6页Geology and Exploration

摘　　要：同位素地质在鄂东南铜铁矿床研究中，提供了地质年龄、硫同位素组成及硫同位素测温资料，为长江中下游鄂东南地区铜铁矿床的岩浆活动、成岩成矿规律、时代划分，以及矿床成因方面取得了令人满意的结果。Through the isotopic study on the iron and copper deposits in Eastsonthern Hubei.the geological age,sulfur isotope compositionand sulfur isotope temperature-measurement data are provided in this paper.Satisfactoryre,results have been achived in the magmatic ac-tivity,rock- forming and ore- forming regularities,age-determination and ore genesisfor the iron- copper deposits in the above areaof the middle and lower reaches of Yangtze River.

关 键 词：地质构造 同位素 铜矿床 铁矿床 

分 类 号：P618.202[天文地球—矿床学]