Аннотации:
In present paper some aspects of stylolites morphology, classifications and genesis have been regarded on core samples of Famennian carbonate rocks from well on southern slope of South-Tatarian Dome. It was observed the presence of stylolites with sizes of 10-2 m, of suture, prisma and peak shapes. Fourier spectra can be used to measure and to classify stylolites as well as to estimate their influence on reservoir properties of carbonate rocks.