Frustumational (primary lumpiness presence) inner fabric of natural rock level of space timinness - a new macroscopic synergetic feature

Development in synergetic sense of the ideas of V. I. Dragunov and D. V. Rundqvist on the rocks unit cells and Academician M. A. Sadovsky on the geophysical medium discreteness («natural lumpiness») has led to the establishment of a new rock macroscopic stereological phenomenon - primary lumpiness, or frustumation (from Latin frustum - lump) firstly in rock samples with simple mineral composition and genesis, and later in rocks with polymineral composition and polygenic. Preconditions of this rock phenomenon discovery are contained in the works of S. M. Beskin, A. G. Zhabin, I. S. Delitsyn, A.N. Nikitin, O. A. Sustavov, V. V. Indutny and M. Yur. Povarennykh, and much earlier in the works of D. S. Korzhinskiy on the local («mosaic») equilibrium during disequilibrium natural geological processes and several works of F. Yu. Levinson-Lessing. In order to reveal the petrophysical essence of the rock frustumation, we successfully conducted a complex of different scale investigations (from nano- to decimeter levels) of rocks with simple mineral composition and genesis with the help of traditional mineralogical-petrographical methods (polarization microscopy, UV-luminescence, X-ray- and microprobe analyses) as well as neutronographic investigation of rock fabric, laser-ultrasonic echoscopy, ultrasonic tomography, and scanning electron microscopy.