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作 者:CUI Ruizhi SANG Shihua LIU Qian ZHANG Kaijie
机构地区:[1]College of Materials and Chemistry & Chemical Engineering, Chengdu University of Technology [2]Mineral Resources Chemistry Key Laboratory of Sichuan Higher Education Institutions
出 处:《Acta Geologica Sinica(English Edition)》2014年第S1期304-304,共1页地质学报(英文版)
基 金:supported by open the National Natural Science Foundation of China (Grant No. 41373062, 40973047);the Specialized Research Fund (20125122110015);the Doctoral Program of Higher Education of China,fund of Key Laboratory of Salt Lake Resources and Chemistry (KLSLRC-KF-13-DX-1);the youth science and technology innovation team of Sichuan Province, China (2013TD0005)
摘 要:1 Introduction China has very abundant liquid mineral resources.Especially,the brine resources in the west of Sichuan Basin are pushed into the first place in China,whose K and B contents are unusually high.These rare liquid mineral resources have very good exploitation prospect(Lin,2001;2006).Generally speaking,phase equilibrium1 Introduction China has very abundant liquid mineral resources.Especially,the brine resources in the west of Sichuan Basin are pushed into the first place in China,whose K and B contents are unusually high.These rare liquid mineral resources have very good exploitation prospect(Lin,2001;2006).Generally speaking,phase equilibrium
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