摘要
云南泸水县石缸河钨锡矿矿体呈脉状、透镜状赋存于断层构造破碎带中,构造控矿明显,燕山期-喜马拉雅期花岗岩侵入为钨矿的形成则提供了岩浆热液成矿物质。通过进一步的地质找矿,在石缸河矿区外围已揭露到了新的矿化带和钨、锡、铋组合地球化学异常,因此在矿区边部或深部隐伏岩体接触带,对寻找钨锡矿化具有较大找矿前景。
The orebody of Shiganghe W-Sn deposit in Lushui,Yunnan is Veined,lenticular in the fault fracture zone,ore control of structure evident.Yanshanian-Himalayan granite intrusion provide the magmatic hydrothermal metallogenesis material for W deposit.According to the further prospecting,we have found out the new metallogenesis zone and W-Sn-Bi assemblage geochemical anomaly around Shiganghe orefield.So,the contact of marginal or deep part of the buried rock body has very good prospecting potentiality of W-Sn metallogenesis.
作者
殷伟
夏建峰
YIN Wei;XIA Jian-feng(Yunnan Institute of Geological Survey,Kunming 650216)
出处
《云南地质》
2020年第2期224-229,共6页
Yunnan Geology
基金
云南省泸水县石缸河外围矿产调查评价(编号:D2014003)。
关键词
钨锡矿
构造控矿
热液型矿床
找矿前景
云南泸水石缸河
W-Sn Deposit
Ore Control of Structure
Hydrothermal Deposit
Prospecting Potentiality
Shiganghe,Lushui,Yunnan