摘要
卯独庆金矿床赋存在古元古代二道凹岩群的绿片岩层与大理岩层过渡带。金矿化明显受构造片理化带控制。该类金矿化控矿因素是岩性层 +构造。
Maoduqing gold deposit occurred in the green schist and marble stratum transitional belt of paleoprotozoic Erdaowa Group in Inner Mongolia. The gold mineralized are controlled by structural schistosition belt. The type ore-controlling factor is lithohorizon + structure.
出处
《内蒙古地质》
2000年第4期9-12,共4页
Geology of Inner Mongolia
关键词
金矿床
地质特征
大青山区
gold deposit
geological characteristics
Daqingshan area
