摘要
都龙金石坡锡锌多金属矿床主要分布在云南省马关县境内,矿床主要金属元素组合与矿体之间的距离由远而近出现由锡、钨到锡、铅、锌、银有规律的变化,结合矿区地质特征,该区钨矿化规律由北-南矿化逐渐变弱,由东-西矿化逐渐变强。
The stone slope Dulong tin zinc polymetallic deposit is mainly distributed in the territory of Maguan County of Yunnan Province,between the main metal elements deposit in combination with the distance from the youyuanerjin by tin,tungsten,tin and lead to the change of zinc and silver regularly,combined with geological characteristics,the tungsten mineralization regularity from North-South mineralization gradually weak,from the East-West mineralization becomes stronger gradually.
作者
王代斌
许红峰
WANG Dai-bin;XU Hong-feng(Yunnan Hualian mineral exploration Co., Ltd.,Qujing 650000,China)
出处
《世界有色金属》
2018年第1期143-144,共2页
World Nonferrous Metals
关键词
锡锌多金属矿床
矿区构造
分布规律
Tin zinc polymetallic deposit
Mining area structure
Distribution law