Rock formation in the stratisphere (Experience of stage genetic research).

The results of the latest research by lithologists, including the author, who, jointly with hydrogeologists and geochemists, substantially specified the concepts on the mechanism of the processes of mineral genesis, fluid genesis, and different scale remobilization of sedimentary substances within the stratisphere (the over-metamorphic sedimentary cover of the Earth's crust), where a part of the sediments was transformed to rocks and ores that are completely different in their mineral composition and physical and chemical properties, due to reserves and long before metamorphism, are generalized. Conclusions are made about the openness and self organization of the stratisphere that together with over- and underlying natural systems influenced the orientation and the evolution of the sedimentary process. [ABSTRACT FROM AUTHOR]