湖北铜绿山铜铁矿床地球化学特征与矿床成因初探  

Geochemical characteristics and genesis of Tonglu Shan copper iron deposit in Hubei

作　　者：赵承佑 ZHAO Cheng-you(Daye Nonferrous Metals Co., Ltd. Tonglv Shan mine, Daye 435100,China)

机构地区：[1]大冶有色金属有限责任公司铜绿山矿,湖北大冶435100

出　　处：《世界有色金属》2018年第6期138-139,共2页World Nonferrous Metals

摘　　要：湖北铜绿山铜铁矿床处于长江中下游成矿带,该成矿带主要矿床类型为金属成矿带接触交代矽卡岩型的矿床。目前该矿床已有了三十多年的规模开采历史,资源已经存在着危机,因此,寻找到接替资源是一个尤为重要的问题。本文主要利用矿床成因理论和地球化学原理,对湖北铜绿山铁矿床地球化特征与矿床的成因进行探究,为矿体深部开采和在边端部寻找盲矿体提供一定指导。The Tonglu Mountain Copper iron deposit in Hubei is located in the middle and lower Yangtze River metallogenic belt, the main type of the metallogenic belt is the metasomatism of the metasomatic skarn type deposit in the metallogenic belt. At present, the deposit has been in the history of more than thirty years, and there is a crisis in the resources. Therefore, it is a particularly important problem to find the replacement resources. In this paper, the geochemical characteristics of the Tonglu mountain iron deposit in Hubei and the genesis of the deposit are explored by using the genesis theory of ore deposits and the principle of geochemistry, which provide some guidance for the deep mining of the ore body and the search for the blind ore body at the side end.

关 键 词：湖北铜绿山 铜铁矿床地球化学特征 矿床成因 

分 类 号：P618.41[天文地球—矿床学]