... oolith limestone on a core scale from the rock microstructure and elastic wave velocities measured on samples. The method of velocity measurements allowed one to estimate the degree of rock heterogeneity on the sample scale and classify the rock as an isotropic one with embedding various inhomogeneities. Statistical characteristics of the parameters describing the void space structure are obtained: aspect ratio of oolitic and intergranular pores and coeffi ients of their connectivity. It is shown that ...

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