Until now, the degree of study of intrusive massifs, with which associated with a variety of endogenous mineralization, remains insufficient to meet many of the demands of science and practice. In this regard, it is necessary to further improve the methods and techniques of study of these formations and, first of all, methods and techniques of field study of intrusions in the process of their geological survey.

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.