Abstract
Results of a comprehensive study of anhydrous (anhydrite, barite, celestite, and thaumasite) and hydrous (gypsum, epsomite, metabasaluminite, and brochantite) sulfates from kimberlite rocks are presented. An assumption is put forward for a possibility to use the typomorphic features of the predominant sulfates from kimberlites to improve the technological processes of extraction of the valuable mineral from a productive ore.
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