Abstract
The detailed study and analysis of the change of numerous determinations of porosity and gas permibility, at different levels of depth in sections of wells of the Krasnosavodsko-Rudovskaia structural zone, testifes of own peculiarities of the porosity and permibility in different blocks. The porosity and permibility of the Krasnosavodsky block, at different levels of depth, change by various ways – wave - shapedly or sine curve – shapedly, step – shahedly or gradually and in the Rudovsky block they change only like sinusoid. The general feature for these blocks is the presence of collectors of satisfactory quality in sections of wells, even at depths of 516 ths. m, which is favourable for formation of hydrocarbon deposits at such depths.
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