• 责任者：Yue Weihao (College of Land Resource Engineering ; Kunming University of Science and Technology ; Kunming 650093 ; China) ; Gao Jianguo
• 刊名：Geology and Prospecting
• 出版年：2011
• 卷期：47(5)
• 关键词：钾盐矿床 ; potash deposit ; 找矿模式 ; prospecting model ; 云南 ; Yunnan Province
• 页码：p.809-822
• 图表：2 illus., 3 tables, 24 refs.
• 分类号：1002
• 出版序号：1800
• issnNo：ISSN0495-5331
• isbnNo：CN11-2043/P

The Mengyejing potash deposit lies in brown and variedness salting-in flult formation of the Cenozoic Mengyejing rock assemblage which is located at the back-foreland basin of the Lanping-Simao bidirectional arc zone, west of the Yangtze massif. Its metallogenesis exhibits evident evaporation-sedimentation cyclothem. The output of potash beds is controlled by strata, lithofacies and tectonics directly. The authors define it as a typical Cenozoic (lake facies) potash deposit, the Mengyejing-type potash deposit. The authors take Lanping-Yunlong, Zhenyuan-Jinggu and Jiangcheng-Mengla as three work areas for ore prediction, which have similar metallogenesis conditions with the Mengyejing potash deposit.