摘要
本文对新疆阿尔泰可可托海的三号伟晶岩形成的物理化学条件、特别是流体-熔融包裹体进行了研究，证明岩浆的确可以分出热液，对于三号伟晶岩脉来说，这种热液组分主要是NaCl－CO2－H2O流体。
This paper deals with the physico-chemical conditions under which pegmatite dike No. 3at Koktokay, Altay, Xinjiang was formed in terms of fluid-melt inclusions. The results indicatethat hydrothermal solutions can be really fractionated from magmas. As for pegmatite dike No. 3,this kind of hydrotherpal solutions is dominated by NaCl+CO2+H2O fluid.
出处
《矿物学报》
CAS
CSCD
北大核心
1996年第1期1-7,T002,共8页
Acta Mineralogica Sinica
