浅析香格里拉红牛铜矿地质特征及成因

A brief analysis of the geological characteristics and genesis of shangri-la hongniu copper mine

文章通过对红牛铜矿区域地质及研究区地质特征及其成因进行分析,认为该矿体在成因上与热液密切相关,矿床类型为多期次复成热液矽卡岩型矿床。研究区矿体主要产出于嘎寺组地层中,主要矿体为KT4,矿石矿物主要为黄铜矿及少量黄铁矿、磁黄铁矿。希望此观点为该地区寻找该类型矿床提供指导。

Based on the analysis of the regional geology and geological characteristics of the Hongniu copper deposit and its genesis,it is considered that the ore body is closely related to hydrothermal genesis,and the deposit type is multi-stage complex hydrothermal skarn type deposit.The ore body in the study area is mainly produced in the stratum of Gasi Formation,the main ore body is KT4,and the ore minerals are chalcopyrite and a small amount of pyrite and pyrrhotite.It is hoped that this view can provide guidance for the exploration of this type of deposit in this area.