摘要
通过对7903矿床地质背景、矿化特征、矿床控矿因素分析,认为矿床受构造和层位双重控制,铀源主要来自花岗岩,矿床成因属表生淋积型铀矿化。
In the paper are the geological setting, mineralization and ore controlled factors of 7903 uranium deposit in Gansu Province analyzed, the author supposed that the deposit was controlled by structure and the stratigraphic horizon, the uranium source came from granite, the genesis of deposit should belong to supergene leaching type mineralization
出处
《甘肃地质》
2010年第1期53-57,共5页
Gansu Geology
关键词
铀矿
特征
控矿因素
甘肃
uranium deposit
characteristics
ore-controlled factors
