| 嵩县上庄坪铜铅锌多金属矿床地质特征及成因分析 |
| |
| 引用本文： | 王瑞良.嵩县上庄坪铜铅锌多金属矿床地质特征及成因分析[J].华南地质与矿产,2007,6(2):14-18. |
| |
| 作者姓名： | 王瑞良 |
| |
| 作者单位： | 河南省第一地质勘查院,河南,南阳,473056 |
| |
| 摘 要： | 本文着重论述了上庄坪铜铅锌多金属矿床的地质特征和成矿淀化,进行了成因分析。认为含矿岩系的物源主要来自海底火山喷发作用形成的黄铁矿化矿源层。经燕山期构造热液的叠加,驱使矿源层中的成矿元素活化、迁移,在有利的构造部位富集成矿。
|
| 关 键 词： | 地质特征 成矿演化 成因分析 黄铁矿化 矿源层 |
| 文章编号： | 1007-3071（2007）02-0014-05 |
| 修稿时间： | 2007-02-03 |
Geological characteristics and Origin Analysis of the Polymetallic Ore Deposit in Shangzhuangping, Songxian |
| |
| WANG Rui-liang.Geological characteristics and Origin Analysis of the Polymetallic Ore Deposit in Shangzhuangping, Songxian[J].Geology and Mineral Resources of South China,2007,6(2):14-18. |
| |
| Authors: | WANG Rui-liang |
| |
| Institution: | No. 1 Gological survey party of Henna, Nanyang 473003, Henan, China |
| |
| Abstract: | This paper emphasizes the geological characteristics and discuss on the origin analysis of polymetallic ore deposit in Shangzhuangping.According to the study of the mineral evolving,origin analysis etc.,it is considered that the source of minerals etc mainly comes from the pyritization sources of the submarine volcano eruption.By the time of Yanshanian structural hydrothermal superimposed caused the ore-forming chemical element of the pyritization sources activated,it results from the elements had been moving and expected turning into minerals in the beneficial structural position. |
| |
| Keywords: | Geology characteristic the mineral evolving origin analysis pyritization the mineral sources |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
