摘要
对矿物流体包裹体加热均一时发现,超过均一温度的热作用会改变包裹体内含物的物态及产生包裹体晕结构,称之为'反态现象'。实际工作中证实,这种热改造包裹体存在于各种矿物、岩石中。对它的研究不仅使其与原始包裹体加以区分。而且能提供叠加增温热液活动的信息。包裹体反态现象的提出和讨论,将深化包裹体热变化的研究,开拓包裹体研究的应用领域。
Obtaining the homogenization of mineral fluid inclusion by heating, the author has discovered the following facts. The heat treat exceeding homogenization temperature, would cause a change of the initial gas-liquid ratio and a phase state transition of inclusion, meanwhile, display a inclusion halo texture. The study of this heated reformed inclusions may help to obtain the informations on hydrothermal activities superimposed during the post-inclusion-forming state.The definition and discussion of the anti-state phenomena of inclusions will help the further study on the heat variation of inclusions and enlargement of it's applicable ranges.
出处
《矿物岩石》
CAS
CSCD
1989年第3期48-56,共9页
Mineralogy and Petrology
