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Д·С·柯尔任斯基,В·С·索波列夫、Г．兰姆别尔格和Т·巴尔特早就开始研究在成分可变的矿物之间其组份分配的规律性,以及把这一规律性作为自然矿物组合形成热力学条件的标志。这一研究方向在Р·米勒尔、Р·克兰茨,А·А马拉库塞夫、М·М·别尔楚克、С·К·卡克西、В．德日、伍德等人的文章中得到了发展,并能正确地求出在矿物中存在的成分与其相应的Р—Т条件之间的规律性,即将其作为地质温度计和地质压力计用。
Kolkensky, В · Sopoljev, Г. Lambemberger and T. Barthes have long been investigating the regularity of their component distribution among the variable minerals and using this regularity as a hallmark of the thermodynamic conditions of natural mineral assemblages. This research is carried out in the fields of Р. Miller, Р克兰茨, А А Maracusev, МММ. Belchuk, СКК Kesi, В. The articles by Germany, Japan and Wood et al. Have been developed and the regularity between the composition of minerals present in their mineral and their corresponding conditions of Р-T has been correctly developed, using it as a geothermometer and geostress.