铀矿地质2017，Vol.33Issue(6)：321-328,8.DOI:10.3969/j.issn.1000-0658.2017.06.001
中新生代盆地深部地质流体及铀成矿作用
Deep Geofluid and Uranium Metallogenesis in Meso-Cenozoic Basin
林双幸 1宫晓峰 1张铁岭1
作者信息
- 1. 核工业北京地质研究院,北京 100029
- 折叠
摘要
Abstract
With the discovery of depth origin evidence of mineralization solution (hot fluid) in the Sandstone uranium deposit of Kanru Gan,Mo Kum and Tortkuduk in Chusarysu basin of Kazakhstan,and the facts of later remobilization and transformation in Cenozoic and Mesozoic basins,the significance of deep sources hot fluids in the procedure of sandstone type uranium mineralization in Cenozoic and Mesozoic basin have been gradually recognized.This article roughly introduced the source and nature of geological fluids in Cenozoic and Mesozoic basin,and summarized three type fluid and their transformation method,as well the main feature of uranium mineralization by deep source hot fluid injection.The article also discussed the possibility of deep geofluid action to uranium mineral1zation in Meso-Cenozoic basin in North China.关键词
中新生代盆地/深源热流体/铀成矿作用/找矿新思路Key words
basin/deep geological fluid/uranium mineralization/creative exploration idea分类
天文与地球科学引用本文复制引用
林双幸,宫晓峰,张铁岭..中新生代盆地深部地质流体及铀成矿作用[J].铀矿地质,2017,33(6):321-328,8.
