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我们以前曾经说过,对于金属矿床中分带现象的热动力的研究,要求掌握一定的物理参数。其中最重要的就是成矿压力,特别是涉及表示矿物形成的自由焓变化的方程式的温度。 本文旨在阐述为确定葡萄牙博拉拉地区含钨石英脉的生成温度剖面而采用的测定气液包体均一温度的方法。
As we have said before, the study of thermodynamic zonation in metallogenic deposits requires certain physical parameters. The most important of these is the metallogenic pressure, especially the temperature of the equation representing the free enthalpy change of mineral formation. The purpose of this paper is to describe a method for determining the homogenization temperature of gas-liquid inclusions for the determination of the temperature profile of tungsten-bearing quartz veins in the Porla area of Portugal.