About the origin of the lithosphere and the hydrosphere of the Earth

Abstract

This article explains the formation of geosynclines, granite and basalt stratums, the World Ocean in a fundamentally new way. The nucleation and development of geosynclines is being connected with the formation of zones of deep breaks and with primitive water in them. Steam and hot water had been transforming ultrabasic rocks of the mantle, carrying out fast components - silica, carbonates, iron, etc. These mineral substances with the help of microorganisms fell out in shallow geosynclinal basins and after metamorphization entered into the composition of the granite stratum. The so-called basalt stratum of the continental Earth's crust isn't a real one. It represents the stratum of ultrabasic rocks of the upper mantle without mineral components, which have entered into the composition of the granite stratum. The formation of the World Ocean is caused by increasing of water quantity on the Earth during the Phanerozoic. It was not only the endogenous (juvenile) water, but the exogenous water, which was exudated by living organisms, as well. The areas of the initial Earth which hadn't gone through the geosynclinal path of development became the bottom of the Ocean. And its sides are the borders of mainlands elevated by isostasy forces.