金红石中的包裹体水  

INCLUSION WATER IN RUTILE

作　　者：徐少康 栾俊霞 陈丹 

机构地区：[1]中化矿山总局地质研究院,河北涿州072754 [2]湖南化工地质勘察院,湖南长沙410004

出　　处：《化工矿产地质》2015年第3期168-170,共3页Geology of Chemical Minerals

摘　　要：金红石中的水以包裹体形式存在,对钛钢产品的质量有严重影响。蚀变和热液成因金红石包裹体水含量相对较高,变质型金红石包裹体水含量较低。除去金红石包裹体水的方法为爆裂法,最高爆裂温度为825-1000℃。The water exists in the rutile as inclusions has the serious effects on the quality of titanium steel.There are more inclusion water from alternative and hydrothermal rutile, and the content of inclusion water from metamorphic rutile is least. Decrepitation method can eliminate inclusion water in the rutile and the decrepitation temprature will be 825-1000℃ at most.

关 键 词：金红石 包裹体水 钛钢 危害 除去方法 

分 类 号：P618.47[天文地球—矿床学]