DEVIATION OF A SYNERGETIC MODEL FOR THE P RECAMBRIAN IRON QUARTZITES (ON THE BASIS OF DATA ON IRON ORE FORMATIONS IN THE KOLA PENINSULA)

This paper is concerned with the Archean iron-ore formations, which po ssess a scale self-similitude, combined randomness and order at differ ent scale levels, coherent signs of formally different nature, and fra ctal nature, i.e. the signs typical of determined and chaotic systems. Special methods of the theory of dynamic systems provided a quantitat ive measure of the complex nature of ore genesis dynamics. It is suppo sed that before any genetic constructions the structures must be teste d for their belonging to one class or another.