Thermobarometry has now become one of the central components of petrology and tectonics as it allows one to put quantitative constraints on the pressure-temperature path in the evolutionary history of rocks. The principles of equilibrium thermodynamics constitute the bedrock foundation for the formulation of thermobarometric expressions that are applicable to natural assemblages. Diffusion kinetics, on the other hand, determines the spatial domains over which equilibrium was achieved in a rock, as was recognised very early on by Harker (1932) in his comments about Goldschmidt’s application of Phase Rule to metamorphic rocks. Because of its wide ranging applications, the...

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2. 温度计的热力学和动力学：概述

热气压测量法现在已成为岩石学和构造学的核心组成部分之一，因为它允许人们对岩石演化历史中的压力-温度路径进行定量限制。平衡热力学原理构成了制定适用于自然组合的热气压表达式的基石。另一方面，扩散动力学决定了在岩石中达到平衡的空间域，正如 Harker (1932) 在他关于 Goldschmidt 将相规则应用于变质岩的评论中很早就认识到的那样。由于其广泛的应用，...