录斗艘金矿床地质特征及矿床成因

Geological characteristics and genesis of ludouzhou gold deposit

录斗艘金矿床处于青藏高原的东部边缘,位于甘肃省甘南藏族自治州合作市,工作区位于西秦岭海西褶皱带的北缘,区内褶皱、断裂构造极为发育,岩浆活动强烈,铜、金矿床(点)及其异常广布,构成了重要的铜、金等多金属成矿带。本文对录斗艘金矿床地质特征及矿床成因进行了探讨,对充分开发利用录斗艘金矿具有重要的意义。

Luduoship gold deposit is located on the eastern edge of the Qinghai Tibet Plateau,located in the cooperative city of Gannan Tibetan Autonomous Prefecture,Gansu Province.The working area is located in the north margin of the West Qinling Haixi fold belt.The fold and fault structures are extremely developed in the area,with strong magmatic activity,and the copper,gold deposits(points)and their anomalies are widely distributed,which constitute important polymetallic metallogenic belts such as copper and gold.This paper discusses the geological characteristics and genesis of luduozhou gold deposit,which is of great significance to the full development and utilization of luduozhou gold deposit.