Метод реконструкции геодинамических обстановок формирования комплексов докембрия с учетом эволюции химического состава мантии

The paper presents a reconstruction method for geodynamic formation conditions of rock complexes in the Precambrian, which takes into account the evolution of the mantle chemical composition. An important feature of this method is in usage of an evolutionary parameter (the relative nuclear mass), introduced by V. P. Keondzhan and A. S. Monin for the purpose of describing the evolution of the Earth's mantle chemical composition. The method is also provided for linear ordering of geological objects, based on a given partial order relation, which allows to substantially expand the range of solvable problems.