Abstract:
Quantitative geochemical modeling possibilities of ore-bearing aqueous fluids separation process from a
magmatic melt are considered. Suggested procedures allow calculation of fluid/melt distribution coefficient
values for trace elements, their contents in a fluid, as well as its total resources in a genetically related
metasomaticaly altered rocks. Application of this approach to the geochemical modeling of real oregenerating
magmatic-hydrothermal system of the Korosten pluton granitoids (Ukrainian Shield), and associated
hydrothermal-metasomatic formations (Suschano-Perzhanskaya area) has confirmed its efficiency. The
purpose of present and future research is to obtain estimations of Ukraine and Kazakhstan regions mineral resources
potential independent from a simple summation of previously conducted regional works.
