托拉木汗冬窝子铅矿初报

苗锡仲

您当前的位置：

首页 >

文章列表页 >

托拉木汗冬窝子铅矿初报

更新时间：2026-01-21

- 托拉木汗冬窝子铅矿初报
- Journal of Xinjiang University (Natural Science Edition in Chinese and English) Issue 1, (1989)
- 作者机构：
  
  新疆大学地理系,
- 作者简介：
- 基金信息：
- DOI：
  CLC：
- Published：1989
- 稿件说明：
移动端阅览
[1]苗锡仲.托拉木汗冬窝子铅矿初报[J].新疆大学学报(自然科学版),1989(01):92-96.

苗锡仲. 托拉木汗冬窝子铅矿初报[J]. Journal of Xinjiang University (Natural Science Edition in Chinese and English), 1989, (1).
[1]苗锡仲.托拉木汗冬窝子铅矿初报[J].新疆大学学报(自然科学版),1989(01):92-96. DOI：

苗锡仲. 托拉木汗冬窝子铅矿初报[J]. Journal of Xinjiang University (Natural Science Edition in Chinese and English), 1989, (1). DOI：

摘要

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.

Abstract

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.

关键词

Keywords

references

Views

下载量

CSCD

Alert me when the article has been cited

提交

Tools

Publicity Resources

No data

Related Author

No data

Related Institution

No data

⁰