摘要
庆云金矿体矿石类型为强硅化蚀变岩型、石英脉型和糜棱岩型。通过1:1万土壤化探圈定的综合异常为该矿区的发现提供了较好的找矿意义,矿体赋存于北东向韧性剪切带中,由于成矿作用的多期性,导致了矿床的多样性,在断裂构造、岩浆活动等成矿作用下使金元素进一步前移富集在适宜的空间成矿。
The ore types of Qingyun gold deposit are strongly silicified altered rock type,quartz vein type and mylonite type.The comprehensive anomaly delineated by 1:10000 soil geochemical exploration provides a good prospecting significance for the discovery of the mining area.The ore body occurs in the northeast trending ductile shear zone.Due to the multi-stage mineralization,it leads to the diversity of the deposit.Under the mineralization of fault structure and magmatic activity,the gold element further moves forward and enriches in the suitable space for mineralization.
作者
申家新
SHEN Jia-xin(Tonghua Geology&Mineral Resource Prospecting&Exploitation Institute Jilin Province,Tonghua 134000,China)
出处
《世界有色金属》
2020年第12期92-93,共2页
World Nonferrous Metals
关键词
地质特征
韧性剪切带
矿石类型
geological characteristics
ductile shear zone
ore type