An Analysis of Fluid Inclusion Homogenization Temperature of Halite from oft-com:office:smarttags" />Bieletan Salt Playa Lake in Qinghai and Its Geological Significanceoft-com:office:office" />

• 责任者：Zhao Yuanyi (Institute of Mineral Resources ; Chinese Academy of Geological Sciences ; Beijing 100037 ; China) ; Li Botao
• 刊名：Mineral Deposits
• 出版年：2010
• 卷期：29(4)
• 关键词：流体包裹体 ; fluid inclusions ; 干盐湖 ; playas ; 钾盐矿床 ; potash deposit ; 察尔汗盐湖 ; Qarhan Salt Lake
• 页码：p.684-696
• 图表：8 illus., 5 tables, 22 refs.
• 分类号：1002
• issnNo：ISSN0258-7106
• isbnNo：CN11-1965/P

This paper has studied the temperature for the formation of mineral salts in Bieletan section in the hope that it might provide a basis for understanding the formation conditions of potash salt. The distribution characteristics of homogenization temperatures of halite in Bieletan area exhibit three or two temperature sections, which are respectively low-temperature section, medium-temperature section and high-temperature section. oft-com:office:office" />