红透山铜锌矿床地质特征及成矿模式浅析  

Geological characteristics and metallogenic model of hongtoushan copper and zinc deposit

作　　者：高桂荣 GAO Gui-rong(China Nonferrous HongTouShan Fushun Mining Group Co.,Ltd,Fushun 113321,China)

机构地区：[1]中国有色集团抚顺红透山矿业有限公司生产技术处,辽宁抚顺113321

出　　处：《世界有色金属》2018年第24期84-85,共2页World Nonferrous Metals

摘　　要：红透山铜锌矿床是一座位于辽宁省清原县境内的矿床,它自1957年被发现后一直被开采利用至今,是中国最具有开采深度的矿山之一。虽然红透山铜锌矿床被开采多年,但是它仍然不断有新的矿产资源被发现。通过对红透山铜锌矿床的研究,本文主要介绍了红透山铜锌矿床的地质特征,以及从矿床的形态构造、矿石的结构等方面对红透山成矿模式进行了分析,旨在寻找深部找矿方向,延长红透山铜锌矿床的寿命。Hongtuoshan copper and zinc deposit is a deposit located in qingyuan county, liaoning province. It has been exploited and utilized since it was discovered in 1957. It is one of the mines with the deepest mining depth in China. Although hongtoushan copper and zinc deposit has been exploited for many years, new mineral resources are still discovered. Based on the study of hongtuoshan cu-zn deposit, this paper mainly introduces the geological characteristics of hongtuoshan cu-zn deposit, and analyzes the ore-forming model of hongtuoshan from the aspects of the ore structure and the ore structure, so as to find the deep ore-prospecting direction and extend the life of hongtuoshan cu-zn deposit.

关 键 词：红透山铜锌矿 地质特征 成矿模式 

分 类 号：P618.4[天文地球—矿床学]