摘要
西昆仑造山带是我国一条非常重要的成矿带,区内矿产资源丰富,具有非常优越的成矿条件,尤其是铜矿资源在该区具有非常好的成矿潜力。由于该区具有非常突出的断裂构造特征,在其作用下存在很多次级断裂,规模上比较大的有木吉-布仑口-库斯拉甫断裂,其展布方向从西往东主要呈现NW-NWW-NNW向。文中在对布仑口铜矿带地质特征进行分析的基础上,探讨其找矿方向,以期为相关工作提供借鉴与参考。
The western Kunlun orogenic belt is a very important metallogenic belt in China.The area is rich in mineral resources and has very favorable metallogenic conditions.Especially,copper resources have very good potential for mineralization in this area.Because of the characteristics of faults is very prominent in this area,there are many secondary faults under the action,there is a relatively large scale of Muji-Bulunkou Cuse Rahv fault,the direction from west to east to the main show NW-NWW-NNW.On the basis of the analysis of the geological characteristics of the brenkou copper ore belt,the prospecting direction is discussed in order to provide reference and reference for the related work.
出处
《世界有色金属》
2017年第24期290-290,292,共2页
World Nonferrous Metals
关键词
布仑口
铜矿床
地质特征
找矿方向
brenkou
copper deposit
geological characteristics
prospecting direction
