• 责任者：Zhang Bingshe (Xi’an Geolgy and Mineral Exploration and Development Institute ; Xi’an 710100 ; China) ; Xu Yong
• 刊名：Northwestern Geology
• 出版年：2013
• 卷期：46(2)
• 关键词：高岭土矿床 ; kaolin deposit ; 陕西 ; Shaanxi Province
• 页码：p.174-180
• 图表：4 illus., 3 tables, 12 refs.
• 分类号：1002
• issnNo：ISSN1009-6248
• isbnNo：CN61-1149/P

     Analysis of the kaolinite deposit and its ore-deposition environment shows that the areas of Fugu hard sedimentary kaolinite deposits were formed respectively in the lake controlled by freshwater behind the coast, the lake between distributary channels, delta plain lakes and moldering riparian lakes. A deposit formed in different sedimentary environments varies in orebody characteristics, ore types and industrial uses. The Deposits formed in the lake controlled by freshwater behind the coast and lake between distributary channels have a large scale and a wide distribution, however, because of the low kaolinite content, high impurity content, and poor quality of the kaolinite, their industrial uses were limited in Porcelain Manufacture.