我国东南四省五个岩盐矿床石盐中流体包裹体的初步研究  

The Preliminary Study of Fluid Inclusions in Salt from Five Halite Deposits of Four Provinces in Southeast China

作　　者：杨吉根[1] 

机构地区：[1]华东地质学院地质系

出　　处：《盐湖研究》1994年第3期1-9,共9页Journal of Salt Lake Research

摘　　要：扼要地介绍了我国东南四省五个岩盐矿床的地质情况，初步研究了这五个岩盐矿床石盐中流体包裹体在类型、成因、成分、数量、大小、形态以及排列方式等方面的特征，并在最后指出了研究石盐中流体包裹体的重要性．This paper briefly introduced geological situation of Dingyuan, Qingjiang. Yingchen. Hengyang,Lixian five halite deposites from Anfei, Jiangxi, Hubei. Hunan four Provinces in Southeast China.and preliminarily studied fluid inclusions in salt from these halite deposites.The result of study showed that fluid inclusions in salt are areextraor-dinary abundsnces. Their common and abvious characteristics as showed by followings:(1) complete type.(2)more complicated genesis.(3) main in liquid phase,(4)simple componet,(5) multiple.(6)disparity in size of single.(7) preponderant assemblage, (8) varied in array pattern of assemblage. The study of fluid inclusions in salt from halite deposites is very imPOrtant. because it is favorable to understund total process as well as physicochrenical condition in form for halite dePOSites and analyze also influence of fluid inclusions on hydro-mining of halttes as well as building Of waste repository.

关 键 词：岩盐矿床 石盐 液包体 

分 类 号：P619.211[天文地球—矿床学]