© T.Ju. Tveritiniva1, A.V. Vikulin2,3

1 Moscow State University, Moscow, Russia,[email protected]
2 Institute of Volcanology&Seismology FED RAS, 683006, Petropavlovsk-Kamchatsky, Piip, 9, Russia, [email protected]
3 Kamchatka State Pedagogical University, 683032, Petropavlovsk-Kamchatsky, Pogranichnaya Street, 4.

A structure of lithosphere plate boundaries as a zones of shear deformations is considered as geological evidence of «own» (not Euler) rotation of plates. An analysis of features of deformation field structural pictures of geological and tectonic maps confirms existence of vortex-type structures. There is established the existence of two direct proportional relationships between rates of lithosphere plate movement and extents of their convergent and divergent boundaries having different characterized times. It is justified the hypothesis about correlation of vortex processes in tectonosphere with wave processes caused by rotation planetary scale. The review of vortex motions and the extensive literature is given.