• 责任者：Wang Chunlian (Key Laboratory of Metallogeny and Mineral Assessment ; MLR ; Institute of Mineral Resources ; CAGS ; Beijing 100037 ; China) ; Liu Chenglin
• 刊名：Acta Petrologica et Mineralogica
• 出版年：2013
• 卷期：32(3)
• 关键词：流体包裹体 ; fluid inclusions ; 包体测温法 ; temperature measurement of inclusions ; 湖北 ; Hubei Province
• 页码：p.383-392
• 图表：7 illus., 2 tables, 43 refs.
• 分类号：0600
• issnNo：ISSN1000-6524
• isbnNo：CN11-1966/P

     Owing to Yanshanian and Himalayan movement, a series of down faulted basins were formed in Late Cretaceous-Paleogene, when Paleocene halite of salt lake deposition was formed in Shashi Formation of Jiangling Depression. The understanding of paleoclimate has important significance for the study of the evolutionary phase of salt lake, the halite origin and the prediction of geological stages and strata of potash salts.