Uranium Deposits of Paleonecks of the Peripheral Zones of the Great Xingan Volcanic Plutonic Belt:Indicators of Large Ore Clusters
Combination of the uranium ore occurrences and deposits, revealed in the outer and flank zones of the Great Xingan volcanic plutonic belt (GXVPB), is one of the notable characteristics of the contiguous territories of South-East Russia (Trans-Baikal region), East Mongolia (Dornod), and North China (Yinshan-Liaohe). In the Trans-Baikal-Mongol-North China uranium-bearing province, common are the hydrothermal, hydrogenic, and polygenic uranium deposits of different geological and mineral-geochemical types and a wide age (from Archean to Neogene and Quaternary period) interval of the formation (Shatkov et al., 1999).
uranium deposits criteria
Vadim Khomich Hongquan Yan Yang Yanchen Natalia Boriskina
Far East Geological Institute, Far East Branch of Russian Academy of Sciences, Vladivostok, Russia Geological Survey Institute of Jilin University, Jilin, China
国际会议
The 6th International Maar Conference(IMC)(第六届国际玛珥会议)
长春
英文
45-46
2016-07-30(万方平台首次上网日期,不代表论文的发表时间)