Rock Formation in the Stratisphere (Experience of Stage Genetic Research)

摘要

The results of the latest research by lithologists, including the author, who, jointly with hydroge-ologists 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 trans- formed to rocks and ores that are completely different in their mineral composition and physical and chem-ical 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.