| 中国金矿区域成矿地质背景 |
| |
| 引用本文： | 韦永福,孙培基.中国金矿区域成矿地质背景[J].黄金地质,1995,1(3):1-7. |
| |
| 作者姓名： | 韦永福 孙培基 |
| |
| 作者单位： | 地质矿产部沈阳地质矿产研究所(韦永福)，地质矿产部(孙培基) |
| |
| 摘 要： | 我国处于欧亚板块、太平洋板块和鳊板块的交汇地带，区域成矿背景可分为古亚洲成矿域、滨太平洋成矿域和特提斯－喜马拉雅成矿域。各成矿域有不同的演化历史与成矿特征。因此，我国金矿成矿环境多样，矿床类型繁杂，金矿空间分布呈现出明显的不均一性，具有区域集中的趋势和地域的差异，不同的大地构造单元有不同的金矿地质特征。
|
| 关 键 词： | 地质背景 区域成矿 金矿床 矿化 |
REGIONAL METALLOGENETIC CONDITIONS OF GOLD DEPOSITS IN CHINA |
| |
| Wei Yongfu.REGIONAL METALLOGENETIC CONDITIONS OF GOLD DEPOSITS IN CHINA[J].Gold Geology,1995,1(3):1-7. |
| |
| Authors: | Wei Yongfu |
| |
| Abstract: | Tectonically, China is situated in the junction of Eurasian, Pacific and Indian plates. The regional geological setting of gold deposits can be divided into paleoAsiatic, marginalPacitic and TethysHimalayan domains. Therefore, the geological backgrounds of gold deposits in China vary from place to another. The gold deposits in China are unevenly distributed and tend to concentrate in centain regions. Different tectonic units have different geological characteristics for gold deposits. |
| |
| Keywords: | China gold deposit geological setting regional metallogeny |
| 本文献已被 CNKI 维普 等数据库收录！ |
