Title : Characterization of lonsdaleite as an indicator of crystal growth according to the laws of vortex dynamics of a spherical vortex
Abstract:
A variety of three forms of lonsdaleite was identified and studied during the crystallochemical formation of crystals in the bowels of the depth plasma fluid. From the study of the crystal-chemical and geometric properties of the minerals of kimberlite pipes and volcanic formations, and based on the spatial geometric crystallography and physics of "slow" fluids, it was found that these initial stages of formation cause the growth of crystals both along the faces and through sectorial regions according to the laws of "direct” spherical vortex, and “turned inside out direct” spherical vortex. Namely, the crystals, through lonsdaleite, that carry the genetic and morphological information about past pulsation processes in the depth plasma fluid interacting with the Earth's crust during movement and cooling. An analytical mathematical conformal analysis of the distribution and change of the density (viscosity) of its own "semi-frozen fluids" in the crystals themselves was carried out for the cases of two, three and four "chambers" of some crystals, characterizing the formation, structure and development of lonsdaleite according to the characteristic proposed by V. Milyuvene.
