| 河南省嵩县小公峪矿区构造破碎带型金矿体特征及成因分析 |
| |
| 引用本文： | 郭克剑,刘传权,周红春.河南省嵩县小公峪矿区构造破碎带型金矿体特征及成因分析[J].华南地质与矿产,2008(2):9-14. |
| |
| 作者姓名： | 郭克剑 刘传权 周红春 |
| |
| 作者单位： | 1. 河南地矿建设工程集团公司,郑州,450000
2. 河南省地质调查院,郑州,450051 |
| |
| 基金项目： | 国土资源部地质调查项目 |
| |
| 摘 要： | 通过对金矿特征分析，认为小公峪矿区金矿主要受构造破碎带控制。根据硫、铅同位素及稀土元素分析结果，该金矿成矿物质主要来源于燕山期花岗岩浆，成因为燕山晚期岩浆热液型中低温矿床。
|
| 关 键 词： | 金矿特征 构造破碎带 成因分析 燕山期花岗岩浆 |
Analysis of the Characteristics and Genesis of Tectonoclastic Zone-type of Gold ore body of Xiaogongyu Mining Area in Song County,Henan Province |
| |
| GUO Ke-jian,LIU Chuan-quan,ZHOU Hong-chun.Analysis of the Characteristics and Genesis of Tectonoclastic Zone-type of Gold ore body of Xiaogongyu Mining Area in Song County,Henan Province[J].Geology and Mineral Resources of South China,2008(2):9-14. |
| |
| Authors: | GUO Ke-jian LIU Chuan-quan ZHOU Hong-chun |
| |
| Institution: | GUO Ke - jian, LIU Chuan - quan, ZHOU Hong - chun ( 1. Henan Geological ＆Mineral Resources Construction Engineering CO. LTD, Zhengzhou 450000, Henan, China; 2. Henan Institute of geological Survey, Zhengzhou 450051, Henan, China) |
| |
| Abstract: | Through the analysis of the characteristics of Xiaogongyu gold mine, we think it is mainly controlled by the tectonic zone. According to the analytic results of the Sulfur isotopes, Lead isotopes and REE, we think that the gold mine minerals mainly came from the granitic magma during the stage of Yanshanian. The genesis of this gold mine is magmatic hydrothermal deposits in the middle - low temperature of the late stage of Yanshanian. |
| |
| Keywords: | Characteristics of gold mine Tectonoclastic zone Genesis analysis Granitic magma of Yanshanian stage |
| 本文献已被 维普 万方数据 等数据库收录！ |
|
