该铅矿系笔者首次发现.地理座标:东经90°45′
北纬46°03′52″.矿体长10m
厚0.1-0.2m
主要矿物为方铅矿
块状构造.光谱分析:Cu1%、Ag>0.01%、Zn0.3%、Sb>0.1%、Cd0.05%;化学分析:Au2.13ppm、Ag118ppm铅矿脉北侧的褐铁矿—石英脉
含少量多金属硫化物.光谱分析:Cu0.04%、Pb0.05%、Zn>0.1、As0.01%.玛因鄂博—卡拉尕衣巴斯他乌断褶带是一条金、银多金属成矿带
晚古生代的火山岩、火山碎屑岩建造与北西西向断裂的交叉部位是成矿的有利地段.
A lead-ore deposit was discovered firstly by the author in the position of 46°03′52″N—90°45′E.The ore body is 10 meters long and 0.1~0.2 meters thick.The main ore mineral is galena (PbS)
massive structure
spectrum analysis:Cu 1%
Ag>0.01%
Zn0.3%
Sb>0.1%
Cd0.05%.Chemical
analysis:Au2.13 ppm
Ag 118 ppm.The Iimonite-quartz vein by the northern side of the lead-ore vein
contains a small proportion of multimetailic sulfides
spectral analysis:Fb0.05%、Cu0.04%、Zn>0.1%、As0.01%.Mayinebo-Kalagayibasitawu fracture-folded zone is a gold-cilver-multimetallic ore-forming one
the available ore-forming segments are situated in the intersections of NWW trending faults with the late-palaeozoic volcanic and volcaniclastic formations.
0
浏览量
8
下载量
0
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621
