| 金矿床的热液流体特征研究 |
| |
| 引用本文： | 王建国,孙丽娜,赵玉山,侯根群,赵纯福.金矿床的热液流体特征研究[J].国土资源,1993(4). |
| |
| 作者姓名： | 王建国 孙丽娜 赵玉山 侯根群 赵纯福 |
| |
| 作者单位： | 沈阳黄金学院地质系 110015 |
| |
| 摘 要： | 通过对中国东部金成矿区域地质特征的分析,根据氢氧同位素及流体包裹体数据特征,表明中国东部金矿床成矿流体主要来自大气降水,其次为变质作用过程释放的水和岩浆分异水;成矿金属组分主要来自太古宙变质岩系。
|
| 关 键 词： | 金矿床 氢-氧同位素 包裹体 |
THE CHARACTERISTICS OF HYDROTHERMAL FLUID IN GOLD DEPOSITS IN THE EASTERN CHINA |
| |
| Wang Jianguo Sun Lina Zhao Yushan Hou Genqun Zhao Chunfu.THE CHARACTERISTICS OF HYDROTHERMAL FLUID IN GOLD DEPOSITS IN THE EASTERN CHINA[J].Land & Resources,1993(4). |
| |
| Authors: | Wang Jianguo Sun Lina Zhao Yushan Hou Genqun Zhao Chunfu |
| |
| Abstract: | The paper has discussed the characteristics on regional geology of gold deposits all over the eastern China. According to the comprehensive analysis on H, O isotopes and fluid inclusions, it is concluded that the ore-forming fluid of gold deposits was mainly from meteoric water, secondly from metamorphism or magmatic differentiation, and ore-forming materials (gold) came mainly from Archean metamorphic series. |
| |
| Keywords: | Gold deposit H and O isotopes Inclusion |
| 本文献已被 CNKI 等数据库收录！ |
|
