摘要
德尔尼铜矿区位于康西瓦-苏巴什-阿尼玛卿晚古生代缝合带的东段部分玛沁段,矿区总的构造线方向为北西向,地层走向和褶皱轴方向一致,矿床成因类型为海底火山喷流沉积块状硫化物矿床,多种找矿标志明显,研究结果对以后的地质勘查具有一定的指导。
The denier copper mining area is located in the eastern part of the Maqin section of the late Paleozoic suture zone of Kangxiwa-Subash-Animaqing.The general tectonic line direction of the mining area is north-west,the stratigraphic strike is consistent with the fold axis,and the genetic type of the deposit is submarine volcanic jet sedimentary massive sulfide deposit.The results have certain guidance for future geological exploration.
作者
井孟恭
JING Meng-gong(Qinghai Second Geological Exploration Institute,Xining 810000,China)
出处
《世界有色金属》
2021年第8期173-174,共2页
World Nonferrous Metals
关键词
玛沁县
德尔尼铜矿
地质特征
找矿标志
Maqin County
Derne Copper Mine
Geological Characteristics
Prospecting Mark