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矿物中的流体包裹体作为一个封闭的地球化学体系,可以真实地记录矿物生成的物理化学状态。保存在流体包裹体中的流体主要为岩浆水、变质水、地层水、地热水、萃取水、CO_2和烃类等,而且他们是在热状态下被捕获于矿物的晶体缺陷和愈合裂隙中的。对于流体包裹体的研究最早可追溯到1858年。矿物生长过程中所圈闭的流体保存了当时地质环境的各种地质地球化学信息(如P,T,pH,X,盐度等)。包裹体中的物质成分是探索、了解相关地质过程的
Fluid inclusions in minerals, as a closed geochemical system, can truly record the physicochemical state of mineral formation. Fluids retained in fluid inclusions are predominantly magmatic water, metamorphic water, formation water, geothermal water, extract water, CO 2 and hydrocarbons, etc., and they are trapped in crystal defects and healing fractures in minerals under thermal conditions of. The earliest study of fluid inclusions dates back to 1858. The fluid trapped during mineral growth preserved various geo-geochemical information (such as P, T, pH, X, salinity, etc.) of the geological environment at that time. The material composition of the inclusions is to explore and understand the relevant geological processes