Lomakin I. The Relief of seamounts and uplifts and bottom tectonic of Atlantic and Indian oceans.

The linear structures of the ocean floor are oriented in a limited number of directions according to the spatial position of a global tektonolineaments network. The unity of lineament systems of continents and oceans shows. The Transverse Structures are cross the continents and oceans without changing of direction. The geomorphological, structural-tectonic and petrological studies suggest the heterogeneity of the ocean floor. Today's varied and sometimes considerable depth of abrasion terraces of different areas and morphostructures of the Ocean argues the significant scale of vertical tectonic movements and their decisive role in the formation of oceanic lithosphere. All the basic processes of formation of the ocean floor crust are exhaustively explained in terms of the theory of the fault-block structure of the Earth tectonosphere. Keywords: lineaments, terraces, leveling the surface, underwater research, fault-block tectonics.