摘要
212铀矿床产于某新生代陆相盆地边缘,其矿化的形成经历了早期热液、同生沉积、后生富集、晚期热液4个成矿阶段,并受特定的成矿条件所控制。矿床的不同地段,各种成矿作用发育程度不同,因而具有不同的成矿特点。
Uranium deposit No.212 occurs at the margin of a Cenozoic continental basin, the formation of its mineralization has experienced four metallogenetic stages: early hydrothermal, syngenetic sedimentation,epigenetic concentration and late hydrothermal and is controlled by specific metallogenetic conditions. Metallogenetic characteristics depend on different portions of the deposit and different development of metallogenesis.
出处
《铀矿地质》
CSCD
北大核心
1991年第1期24-30,共7页
Uranium Geology
关键词
铀矿
矿床
成矿作用
Metallogenesis
Syngenetic sedimentation
Epigenetic concentration
Hydrothermal superimposition
