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人们对稀有金属矿化同酸性岩浆作用的关系问题已研究多年,尽管进行了大量研究工作,但仍然还有不少争论不清的问题。看来,要解决这些问题,除了传统的方法外,尚需适当地引入新途径和新方法。本文试图根据用矿物中熔体包裹体和流体包裹体的研究方法所获得的结果,来研究稀有金属矿化与岩浆作用的关系问题。近年来这一方法越来越广泛地用以解决各种与探求所研究的对象的成因有密切联系的问题。本文主要是详述能够阐明《岩浆熔体-热水溶液》体系某些特点的内生作用的基本参数(温度和压力)的
The relationship between rare metal mineralization and acid magmatism has been studied for many years. Despite a great deal of research work, many controversial issues remain. It seems that in order to solve these problems, in addition to the traditional methods, new ways and new methods need to be appropriately introduced. This paper attempts to study the relationship between rare metal mineralization and magmatism based on the results obtained from the study of melt inclusions and fluid inclusions in minerals. In recent years, this method has been used more and more extensively to solve various problems that are closely linked to the search for the causes of the subjects under study. This paper describes in detail the basic parameters (temperature and pressure) of endogenesis that characterize certain characteristics of the “magmatic melt-hot water solution” system