江西清江盆地岩盐矿床三种盐矿物中流体包裹体的初步研究  

PRELIMINARY STUDY OF FLUID INCLUSIONS OF THREE SALINOUS MINERALS FROM HALITE DEPOSIT OF QINGJIANG BASIN IN JIANGXI

作　　者：杨吉根[1] 

机构地区：[1]华东地质学院

出　　处：《化工矿产地质》1995年第1期47-54,共8页Geology of Chemical Minerals

摘　　要：清江盆地岩盐矿床是我国东南地区中新生代的一个重要盐矿。该盐矿的矿石矿物主要为石盐，其次为钙芒硝和硬石膏，在这三种盐矿物中均含有较丰富的流体包裹体，但其流体包裹体的类型，成分、数量、大小和分布等特征都存在差异。就一般而言，研究盐矿物中的流体包裹体对发展岩盐矿床地质理论和指导开采以及处置核废物都具有重要意义。Abstract The halite deposit of Qingjisng barn in Jiangxi represents one of important Meso-Cenozoic rock salt deposits in Southeast China, with halite as major ore mineral and glauberite and anhydrite as minor. Any of these three minerals contains aboundant fluid inclusions but they are clearly different in type, size, quantity,composition and distribution of the inclusions. Generally speaking, researches on these differences will contribute to a greater degree to expanding theory of salt geology, directing development of salt deposits and, even in the future, disposing of nuclear waste in thesmined deposits.

关 键 词：盐矿床 岩盐矿床 盐矿物 液包体 钙芒硝 

分 类 号：P619.211[天文地球—矿床学]