摘要
野马铜多金属矿位于中祁连加里东铁铜、钨、钼、金、铜多金属成矿带,区内地层出露复杂,岩浆活动强烈,成矿条件有利。本矿区大地构造属塔里木板块敦煌地块柳园裂谷活动带的北缘。文章对该矿地质特征及成因进行了简要分析。
The Mustang copper polymetallic ore is located in the copper, tungsten, molybdenum, gold and copper polymetallic ore belts of the East China Railway, and the strata in the area are complex, magmatic activity is strong, and metallogenic conditions are favorable. The geodetic structure of this mining area belongs to the northern margin of the Liuyuan Rift activity belt of the Dunhuang block of the Tarim block. This paper briefly analyzes the geological characteristics and genesis of the mine.
引文
[1]吴永阔,程主华,赵吉昌.野马铜多金属矿地质特征及成因浅析[J].世界有色金属,2018,505(13):132+134.
[2]张丽倩.新疆西准噶尔托里县野马井一带成矿预测研究[D].长安大学,2012.