L. N. Sharpenok
Magmatic-ore systems of continental volcano-plutonic belts of mobile areas
The materials revealing the idea of the evolutionary-paragenetic nature of the relationship ore and magmatic formations reflected in the concept of magmatic ore system (MOS) are given. Mineralization is considered as the final product formation not of specific magmatic complexes but of various types of MOS in general. Evolutionary development of these systems in many cases leads to saturation of their ore-forming aqueous fluid phase, under certain conditions generating mineral ore formations. Character of petrogenesis structures of various types determines the composition of possible mineralization and specificity of formation of each of them determines its implementation.
Key words: continental volcano-plutonic belts of mobile systems, central-ring structures, magmatic-ore system, mineralization.