370 



S. G. KOMAROV AND Z. I. KeIVSAR 



Table 4. A comparison of the most probable values for the permeability 

 ^pgj., determined from the specific resistance, with the average values of the 



permeability iLjei-OBTAINED FROM THE CORE (FROM EXISTING DATA) 



in resistance on the interstitial water saturation, as a result of which, for 

 approximately the same value of water saturation, there are different values 

 for the coefficient of increase in resistance. 



The latter is confirmed by the sharp change in the most probable values 



Fig. 8. Curves of the distribution of coefficients of increase in resistance Q. {N — per- 

 centage of values of Q corresponding to the interval of changes). 1 — Tuimazinskian 

 deposit, strata DjandDjj; 2 — Romashuiskian deposit, stratum Dj; 3 — Sokolovogorsk 

 deposit, stratum D^; 4 — Perm Priural'e; 5 — Shkapovskian deposit, strata Z)j andDy; 

 6 — Baku, productive stratum; 7 — Groznyi, sandstones of the Karagano-Chokrakskian 

 deposits; 8 — Nebit-Dag deposits; Turkmen. 



