The idea of the petrogenetic grid of Bowen (1940) that was developed in connection with his decarbonation series of siliceous limestones and dolomites probably constitutes the earliest quantitative approach to constraining the P-T condition for equilibration of an observed mineral assemblage in a rock. A very important step towards the development of the petrogenetic grid is due to Korzhinskii (1959), who adapted Schreinemakers’ principles of organising a set of univariant reactions intersecting at an invariant point in a self consistent way (see, for example, Niggli, 1954; Ganguly, 2020 for an exposition of Schreinemakers’ principles) to...

中文翻译：

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4 变质岩的岩性网格和 PT 演化

Bowen (1940) 的岩石成因网格的想法与他的硅质石灰岩和白云岩的脱碳系列有关，可能构成了最早的定量方法，用于限制 PT 条件以平衡岩石中观察到的矿物组合。Korzhinskii (1959) 对成岩网格的发展迈出了非常重要的一步，他采用了 Schreinemakers 的原则，即组织一组以自洽方式在不变点相交的单变量反应（例如，参见 Niggli，1954 ；Ganguly，2020 年，用于阐述 Schreinemakers 的原则）...