In Lesser Caucasus Atabek-Slavyan plagiogranite intrusive of Mesozoic differs from other the single-age and single-type intrusives by other its ore content and by development of heterogeneous genetic types of mineralization as well: copper-molybden-porphyry hydrothermal hematite and tourmaline. In article for the first time they are represented as complex of successively formed fields in single tectonic-ore-magmatic system.
Combination of these mineralizations is a rare phenomenon not only for the Lesser Caucassus. Along with this it demonstrates the rariety of geological events: duration of ore-formation process and its multi-stages by example of one intrusive object. There is analysis of possible sources of mother compositon of above mentioned types of mineralizations on mineralogical-geochemical data in article. There is no data on isotopy concerning these objects, but there is a possibility of analysis conduction dealing with ore matter sources on results of other research.