The Kul'dursk deposits of brucite were opened up in 1965. The brucite consists of a rock composed mainly of natural magnesium hydroxide Mg(OH) 2 containing from 80 to 95%* magnesia (calculated as the calcined mass). The overall geological and geochemical characteristics of these brucites and the assessory rocks are described in the work of P. P. Smolina and co-authors [!, 2]. In order to explain the relationship between the natural types of brucites and their quality the present article examines the mineral-petrographical features of the commercial, brucite raw materials delivered from the Kul'dursk mines to enterprises in the refractories industry for the production of electro-technicalpericlase and magnesia refractories.For the investigation of the mineral composition and the nature of the distribution of impurities on the raw material stocks of the Bogdanovich Production Association, which manufactures refractory materials, we selected more than 30 gross samples, consisting of mixtures of brucite of various sorts and also assessory rocks # . Such a complicated substance composition for the mined raw material is due to the extremely complex geological structure of the deposits (Fig. I), which hinders selective mining of the ore in grades. Furthermore, the technological sorts of brucite, in terms of color and texture-structural features, are not clearly distinguished, which prevents their contouring during operational development without preliminary chemical analysis of the samples.The deposit is located within the limits of the Precambrian nucleus of the Khingan--Bureinsk anticline. The geological structure of the site is determined by its attachment to the magnesia-carbonate bed of the Murandavsk formation within the limits of the metamorphic aureoles of granitoids [i, 2]. The assessory rocks consist of magmatic and metamagnesia complex. Among the magmatic rocks the most widespread are the porphorized granites~ granodiorites, bostonites, applitogranoporphyries, and in addit&on there are dykes of dolerites and tuffs. The metamagnesia complex is composed of the following rocks: magnesia skarnoids and serpentinites, calcium silicate-carbonates, brucites, carbonated marbles, and anchimonomineral brucites.Three texture-structural types of brucite are detected at the site: pseudomorphic (fibrous-granular), collomorphic (fibrous striated), and automorphic (plate-granular). The commonest mineral-impurities in the brucite ores are dolomite, calcite, and serpentine.In the selected gross samples, after washing to get rid of the dispersed extraneous impurities, according to visual signs (color, texture-structural features) we identified four typical groups of brucite raw material and impurity (assessory) rocks, which were subjected to detailed mineral'petrographic, chemical, thermographic and x-ray analysis.~ Investigations were made to determine the quantitative mineral composition of the typical varieties of commercial raw material, the nature of the distribution of the mineral impurities, their morphological and other ...