Content Variations of Rubidium and Bromide in Sylvite Derived from Carnallite by Leaching of Magnesium Chloride  

作　　者：CHENG Huaide HAI Qingyu ZHANG Xiying FAN Qishun MA Haizhou 

机构地区：[1]Key Laboratory of Salt Lake Resources and Chemistry, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences [2]University of Chinese Academy of Sciences

出　　处：《Acta Geologica Sinica(English Edition)》2014年第S1期298-300,共3页地质学报（英文版）

基　　金：the West Light Foundation of CAS (2011-180);the National Program on Key Basic Research Project of China (973 Program) (2011CB403004) for financial support

摘　　要：The relationship between sylvinite and carnallite is important in the potash mine body contained carnallite,especially sylvinite overlies carnallite,the reverse of a normal depositional sequence.Trace elements are moreThe relationship between sylvinite and carnallite is important in the potash mine body contained carnallite,especially sylvinite overlies carnallite,the reverse of a normal depositional sequence.Trace elements are more

关 键 词：CARNALLITE primary sylvite secondary sylvite BROMIDE rubidium. 

分 类 号：P619.211[天文地球—矿床学]