摘要
我国处于欧亚板块、太平洋板块和印度板块的交汇地带，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。
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.
出处
《黄金地质》
1995年第3期1-7,共7页
Gold Geology
关键词
地质背景
区域成矿
金矿床
矿化
China, gold deposit, geological setting, regional metallogeny
