摘要
人站石铜矿矿体主要赋存于然薪厂背斜西冀的次级人占石向斜轴部近南北向断裂内,赋矿岩石为青龙山组蚀变白云岩,矿体产状与断层产状基本一致,铜矿化的周围均发育有断裂或者充填有热液脉体,受断裂控制明显,属于热液侵染型矿床,而非传统意义的“东川式”铜矿。
Renzhan copper ore body is mainly located in the nearly north-south fault of the axis of the secondary renzhanshi Syncline in the West Hebei of the ranxuchang anticline.The host rock is the altered dolomite of Qinglongshan formation.The occurrence of the ore body is basically the same as that of the fault.There are faults or filled with hydrothermal veins around the copper mineralization,which are obviously controlled by the faults.It belongs to the hydrothermal intrusion type rather than the traditional significance"Dongchuan type"copper mine.
作者
赵讯
龙训荣
ZHAO Xun;LONG Xun-rong(School of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China)
出处
《世界有色金属》
2020年第21期76-77,共2页
World Nonferrous Metals
关键词
铜矿床
地质概况
矿床成因
copper deposit
geological survey
ore genesis
作者简介
赵讯,男,生于1995年,汉族,山东烟台人,硕士,研究方向:三矿。
