Widespread in the Dzungarian Alatau Hercynian granitoid intrusions many geologists divide into two complexes: Central Dzungarian and younger Lepsin, which are attributed different metalliferousness. However, the attribution of specific massifs to one or another complex in many cases causes discussion and remains unresolved due to the lack of clear age boundaries for most of the large massifs, ambiguity of definitions of absolute age and diversity of material composition...

In recent years, on the southern slopes of the Dzungarian Alatau discovered and studied peculiar vein alkaline-basaltoid rocks, which correspond to the totality of geological and petrographic-mineralogical features of camptonites. A characteristic feature of these rocks is the abundance of various clastic inclusions, mostly of deep origin. The study of these inclusions is of undoubted interest in connection with the problem of genesis of lamprophyres and the structure of deep horizons of the Earth's crust and upper mantle.