本文考察了澳大利亚北部地区东阿利盖特河铀矿区(EARUF)脆性-韧性构造的展布与发育状况,该构造控制着矿化的分布与有关的蚀变。从而提出与不整合有关的铀矿床的局部垂向体系的一般模式。引用了裂变径述资料,并和流体包裹体和稳定同位素资料一起,来说明与其有关的大的热液系统。 This paper examines the distribution and development of the brittle-ductile tectonics of the East Aligate uranium deposit (EARUF) in the northern part of Australia, which controls the mineralization distribution and associated alteration. Thus proposing a general pattern of local vertical systems of uranium deposits related to unconformity. Cited fission recapitulation data, along with fluid inclusions and stable isotope data, to account for the associated hydrothermal system.