武山铜矿围岩蚀变特征与成矿关系  

Relationship Between Wall rock alteration and mineralization in Wushan County copper deposi

作　　者：张明华[1] ZHANG Ming-hua(Northwestern Jiangxi Geological Team,Bureau of Exploration and Development of Geology and Mineral Researches of Jiangxi Province,Jiujiang 332000,China)

机构地区：[1]江西省地质矿产勘查开发局赣西北大队,江西九江332000

出　　处：《世界有色金属》2021年第8期88-89,共2页World Nonferrous Metals

摘　　要：武山铜矿是长江中下游地区著名的大型铜矿之一,具有“多位一体”矽卡岩铜矿成矿特征[1]。本文在武山铜矿床成矿地质背景的资料的基础上,通过矿床围岩蚀变类型,围岩蚀变分带,蚀变作用过程中元素的带出、带入计算,及其蚀变与成矿作用关系的研究工作,旨在对进一步总结出武山铜矿床乃九瑞矿集区同类型矿床的矿床成因、成矿规律以及找矿方向提供借鉴。Wushan copper deposit is one of the famous large scale copper deposits in the middle and lower reaches of the Yangtze River,with metallogenic characteristics of“multi-position in one”skarn copper[7].Based on the data of metallogenetic geological background,through wall rock alteration type,alteration zones,the calcaulation in the alteration process of elements out and into,the relation between wall rock alteration and mineralization,this article provides reference for further summing up the deposit genesis,metallogenic regularity,prospecting direction of the same types in WUshan even Jiurui ore concentration area.

关 键 词：山铜矿 围岩蚀变 蚀变分带 成矿关系 

分 类 号：P612[天文地球—矿床学]