Quartz veins are natural objects with which industrial concentrations of ore mineralization are associated and which themselves can be bodies of minerals - raw materials for smelting various types of quartz glass.

The influence of host rocks on the regularities of the location of quartz veins within crystal-bearing fields, the genesis of the veins and the formation of crystal nests is quite widely covered in the Russian literature. In many crystal-bearing fields, the confinement of quartz veins to sequences of a certain composition, which are considered productive with respect to crystal content, has been noted. All researchers to one degree or another note the influence of rocks on the mineral paragenesis of crystal nests, and some consider the host rocks as a source of silica in the formation of not only crystal nests, but also the quartz veins themselves.

When studying hydrothermal deposits, the attention of researchers, first of all, is attracted by vein bodies diverse in composition and structural-textural features. Elucidation of the conditions and processes of their formation is in this case the main and rather difficult problem.

The deposit is located in the western exocontact of the microcline granite massif and is confined to a brachyanticline composed of various crystalline schists. Attention should be drawn to the following features of the geological structure of the deposit...