摘要
大渡河金成矿带位于康滇地轴南北向构造带北端,鲜水河、龙门山与攀西裂谷所构成的三叉裂谷交会形成的特殊构造部位。本文通过对大渡河金矿床的成矿地质条件,对本矿床的成矿特征进一步的进行研究。
The gold metallogenic belt of Dadu River is located at the northern end of the North-South tectonic belt of the Xikang Yunnan axis. The special tectonic site formed by the intersection of the fresh water river, the Longmen mountain and the Panxi rift valley formed by the intersection of the three gorges. Based on the metallogenic geological conditions of the Dadu gold deposit, the metallogenic characteristics of the deposit are further studied.
出处
《世界有色金属》
2017年第14期167-168,共2页
World Nonferrous Metals
基金
大渡河流域金成矿带成矿模式及其找矿模式研究
项目编号:12120113095000
关键词
金矿床
控矿因素:成矿特征
Gold deposit
Controlling factors
metallogenic characteristics
