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一、前言气液包裹体(fluid inclusion)是把矿化流体一直保存到现在的唯一的天然产物。近几年来,对于测定气液包裹体的充填温度和盐度,并以此推测矿液的性质和矿床生成条件的研究工作极为盛行。例如,凯利和特诺勒(Kelly 和 Turneaure,1970)对于东安弟斯(Andes)山脉的锡、钨矿床整个矿化期矿液变化的研究,以及罗德(Roedder,1971)、拉伊和索金斯(Rye 和 Sawkins
I. INTRODUCTION Fluid inclusions are the only natural product that holds mineralized fluids until now. In recent years, research on the determination of the filling temperature and salinity of gas-liquid inclusions and the speculation of the properties of ore fluids and the formation conditions of deposits has become very popular. For example, Kelly and Turneaure (1970) investigated the mineralization during the entire mineralization of tin and tungsten deposits in the Andes range, as well as Roedder (1971), Rye and Cable Kings (Rye and Sawkins