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.
引文
[1]四川冕宁尤黑木向形构造解析及控矿模式(田作基,《成都理工大学学报(自然科学版)》,1997).
[2]稀土元素在尤黑木铜铁多金属矿床研究中的应用(吴启福《四川地质学报》,1996).
[3]四川省冕宁县尤黑木地区铜多金属矿产资源评价预查地质报告(中国地质调查局西南资料分馆,《沉积与特提斯地质》,2004).