Abstract
The paper considers processes of ore formation. This concerns complex dynamic natural objects, depending on polygenic geological phenomena, mutually interacting and forming a single mineral formation environment. Development of ore-forming systems is connected not only with the natural evolution of thermodynamic parameters, but also with physical-chemical properties and composition of ore-bearing deposits, state and character of manifestation of tectonic structures, such as field strength, degree of tectonic transformation of rocks, dynamometamorphism and others. Influence of postmagmatic fluids and other factors on the process of mineral formation is also considered. Mineral formation at gold deposits is the result of the interaction of various polygenic geological processes that ultimately determine the character of mineralisation at the deposits. Experimental studies cannot fully reconstruct the conditions of ore formation. Therefore, it is necessary to apply the method of recalculation of thermodynamic constants.
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