摘要
中川岩体位于甘肃省礼县西北约13km处,属秦岭褶皱系的礼县—柞水冒地槽褶皱带西段中部,岩体是以印支期花岗岩为主体,与铀成矿关系较为密切。在中川花岗岩体内产有7902小型铀矿床及多个铀矿化点,其控矿因素多种多样,其富集规律也于各控制因素关系密切。
Zhongchuan rock mass is situated in northwest Lixian County of Gansu Province, tectonically, in the middle section of Lixian-Zhashui fault zone of Qinling fold system. It is the Indosinian granite that consist of main part of Zhongchuan body, and were closely related to uranium mineralization.
出处
《甘肃地质》
2014年第1期68-72,共5页
Gansu Geology
基金
中央地质勘查基金项目(编号:2011621037)
关键词
铀矿化
控制因素
富集规律
中川岩体
uranium mineralization
control factors
enrichment
Zhongchuan rock mass
