摘要
本文对什库尔干县孜利吉尔一带多金属矿床地质特征及矿床成因进行了相关分析,该矿床成因类型主要为矽卡岩型,并在矿体形成后叠加后期热液改造,随后探讨了该地区今后的找矿标志,为下一步区域内深部找矿提供相应的理论参考。
In this paper, the geological characteristics and genesis of polymetallic deposits in zirgill area of shkkorgan county were analyzed. The genetic types of the deposit were mainly skarn type, and after the formation of the orebody, the hydrothermal transformation was made after the superposition of the ore body. The future prospecting marks in this area were discussed, which provided for the deep prospecting in the next area. The corresponding theoretical reference.
作者
冯晓霞
FENG Xiao-xia(Second regional geological brigade of the Xinjiang geological and Mining Bureau,Changji 831100,China)
出处
《世界有色金属》
2018年第7期209-209,211,共2页
World Nonferrous Metals
关键词
铜多金属矿
地质特征
矿床成因
找矿标志
copper polymetallicore
geological characteristics
ore genesis
prospecting criteria