Abstract
On the basis of the functional system of replacing carnallite with variegated syl-vinite, the laws of distribution of gases in the rocks of layer B of mixed composition are explained. Various variants of sylvinitization process of layer B carnallite during the movement of aggressive aqueous solutions are considered. It is shown that the decrease in the volume of reservoir B as a result of sylvinitization can be compared with the development of protective layers in the suite, which is used, among other things, for degassing rocks.
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