Fluid nature of carbonification and bulk argillization on the Gusevskoe deposit of porcelain stones (Southern Primor'e).

The article presents information on a study revealing the phenomenon of fluid carbonification of subvolcanic dacitic stock and host terrigenous rocks which results in bulk acid argillization on the Gusevskoe deposit of porcelain stones in Russia. It provides information that inversion of the oxidized state of carbonaceous fluids resulted in extensive synthesis of organic-acid compounds. It reflects that the unique character of development of the hole textures of destruction for spinels, micas, and feldspars was established from the study. The processes of bulk sublimation of silicate and ore materials under the influence of diffusing gases are presented.