摘要
尤黑木铁铅锌矿为一以铁为主的小型矿床。本文结合实际地质资料,对矿床成因进行了类比分析,认为矿区内铁铅锌矿属火山沉积成矿,经区域变质、岩浆期后热液充填的改造矿床。
Juheimu iron lead-zinc deposit is a small iron deposit.In this paper,the genesis of the deposit is analyzed by analogy with the actual geological data,and it is considered that the iron-lead-zinc deposit in the mining area belongs to volcanic sedimentary metallogenesis and is transformed by hydrothermal filling after regional metamorphism and magmatic stage.
作者
童彬
张浩
TONG Bin;ZHANG Hao(Xi'an Northwest Nonferrous Geochemical Exploration Group Co.,Ltd.,Xi'an 710068,China)
出处
《世界有色金属》
2019年第7期153-154,共2页
World Nonferrous Metals
关键词
铁铅锌矿
矿床成因
火山沉积
热液充填改造矿床
iron lead zinc ore
Genesis of the deposit
Volcanic deposits
Hydrothermal filling to transform ore deposit