个旧锡矿高松矿田层间氧化矿找矿方向探讨  

A PROBE INTO THE PROSPECTING DIRECTION OF INTERBEDDING OXIDIZED ORE OF GAOSONG OREFIELD OF GEJIU SN DEPOSIT

作　　者：谭敏 罗健 TAN Min;LUO Jian(Yunnan Sn Mining Company（Ltd）,Gejiu 661000)

机构地区：[1]云南锡业股份有限公司,云南个旧661000

出　　处：《云南地质》2018年第2期171-174,共4页Yunnan Geology

摘　　要：个旧锡矿高松矿田是以氧化矿为主的锡矿区,该区矿体成群出现,常常呈多层叠瓦状形态,分布于岩体外接触带中三叠统个旧组层间破碎带中。在距离花岗岩体外接触带500m-700m的一定范围内,是寻找层间氧化矿的有利地段。Gaosong orefield of Gejiu Sn deposit is a Sn orefield mainly with the oxidized ore. The orebody in this orefield is in group occurrence,often in multi-bed imbricate form in Middle Triassic Gejiu Formation interbedding fracture zone of rockbody outer contact. The advantageous area of interbedding oxidized ore prospecting is within 500-700 m of granite body outer contact.

关 键 词：层间破碎带 构造控矿 找矿方向 云南个旧 

分 类 号：P618.44[天文地球—矿床学]