摘要
储广山花岗岩体受郯庐断裂系遂川——热水走滑断裂带控制,区内塘湾断裂及一系列北西向断裂带发育,构成有利的成矿构造结,其中发现多个大型、超大型的铀矿田和铀矿床,其铀矿化受多因素控制,以构造、围岩和岩浆-热液活动为主,在时间上、空间上具有独特的展布规律,通过对该矿床的岩石、构造、矿体和围岩蚀变特征的分析,探讨了围岩蚀变与铀矿成矿的关系,为同类地区的找矿提供了依据.
The granite body in Chuguangshan is controlled by Tanlu fault system Suichuang-Reshuizoufa fault system,Quneitangwan fault zone and a series of north-west fault zones are developed to form favorable structural knot.Many large-scale and super large-scale uranium field and uranium deposit have been found where uranium mineralization is controlled by many factors,mainly made up of rock fabric,wall-rock and magma-hydrotherm activity.The spreading rules are particular in time and space distributing.The relation ...
出处
《南华大学学报（自然科学版）》
2007年第3期33-36,共4页
Journal of University of South China：Science and Technology
关键词
铀矿床
矿体
围岩蚀变
uranium deposit
ore body
wall-rock alteration
