试论平果三水铝石成因、富集规律及工业价值  

DISCUSSION ON ORIGIN CENTRALIZE REGULARITY AND INDUSTRY VALUE OF THE AlO(OH)_3 ORE IN PINGGUO

作　　者：卢文华 韦永坚 黎乾汉 廖思福 

机构地区：[1]广西平果铝业公司矿山部,广西平果531400

出　　处：《广西地质》2001年第2期15-18,26,共5页Guangxi Geology

摘　　要：平果岩溶堆积型铝土矿系一水硬铝石铝土矿床 ,原矿中含有大量的准胶结物———红土。研究资料证实 ,红土中的三水铝石含量甚高 ,不少地段已达到工业利用的要求。其他矿物质来源于原生沉积铝土矿床 ,并与堆积矿同产于一个层位。The karst accumulative bauxite in Pingguo is bauxite deposit of AlO(OH) 3, The primary accumulative bauxite include many agglutinate--ruddle. Investigative datum confirm, the content of AlO(OH) 3 bauxite in ruddle is very high many ruddle have attained industry require. The metallogenic matter are derived from the primary sedimentary bauxite, and granted accumulative bauxite located in the same position.

关 键 词：红土化作用 三水铝石 富集规律 成矿作用 成因 工业价值 

分 类 号：P618.45[天文地球—矿床学]