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近二十年来,矿物包裹体的研究发展很快,理论上取得了新的进展,研究方法上不断革新,数据应用范围也日益扩大.目前,包裹体研究已可为地质研究提供成矿热液(或熔融体)的温度、压力、盐度、密度、初熔温度、气相和液相成分、稳定同位素组成、不混溶特征、成矿年龄、爆裂活度、pH和Eh值等十多种参数,并广泛应用于地质找矿、理论研究等方面. 包裹体理论的进展一、不混溶包裹体的研究自1958年索尔比等人确定了包裹体研究的三条基本假定以来,地质界一直认为包裹体仅是从均匀体系中圈闭的.但是,最近研究表明,它也可以从不均匀体系中圈闭出来.
In recent twenty years, the research on mineral inclusions has developed rapidly, new advances have been made in theory, research methods have been continuously updated, and the scope of application of data has also been increasingly widened.At present, inclusion studies have provided ore-forming hydrothermal fluids for geological studies (Or melt) temperature, pressure, salinity, density, initial melting temperature, gas and liquid composition, stable isotope composition, immiscibility, mineralization age, burst activity, pH and Eh value of more than 10 Parameters, and widely used in geological prospecting, theoretical research, etc .. The progress of the theory of inclusions First, the study of immiscible inclusions Since 1958, Solbi et al identified three basic assumptions of the study of the inclusion, the geological community It has been thought that inclusions trap only from a homogeneous system, but recent studies have shown that they can also be trapped from an inhomogeneous system.