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《Journal of Salt Lake Research》 2011-04
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Clay Minerals of Paleocene in Lanping-Simao Basin and A Tentative Discussion of Salt-forming Environment

SHI Lin1,2,GAO Dong-lin1,ZHANG Cong-wei1,2,ZHANG Xi-ying1,TANG Qi-liang1(1.Qinghai Institute of Salt Lakes,Chinese Academy of Sciences,Xining,810008,China; 2.Graduate University of Chinese Academy of Sciences,Beijing,100039,China)  
Yunnan Lanping-simao basin is an important basin with K salt deposition in China.The clay minerals samples exist in Paleocene Mengyejing formation of muddy gravel phase(salt-forming epoch) in Lanping-simao basin including the samples of the same strata(Yuanyongjing Formation) in Chuxiong basin of central Yunnan are experimented by the method of XRD.The experiment results show that the dominant assemblage of clay minerals in Lanping-simao basin are illite and chlorite,and indicates that the dry paleoclimate and high paleosalinity in salt-forming epoch;but in Chuxiong basin,illite and chlorite,illite/smectite mixed-layer minerals are coexisting,it reflects the wetter paleoclimate than Lanping-simao basin.It indicates that the salt-forming epoch in Lanping-simao basin is later and the salification in Lanping-siman basin is stronger by calculating the relatively composition of the clay minerals.Based on previous researches,the tentative discussion of salt-forming environment in Lanping-Simao basin suggested that the overall degree of brine concentration in the southern part of the basin is higher than the northern,and the salt ore-forming environment in the southern is better than the northern too.
【Fund】: 中国科学院知识创新工程重要方向项目(KZCX2-YW-344)
【CateGory Index】: P642.13
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