The segment of the Mid-Atlantic Ridge, limited at the North with Doldr
ams fracture zone (6 degrees N) and with St. Paul fracture zone (1 deg
rees N) at the South, conventionary named by us as Equatorial, was stu
died in detail under international programme EQUARIDGE (7, 11, 12 crui
ses of r/v ''Akademik Nikolaj Strakhov''). Complex of geological-geoph
ysical survey was based on detail mapping of the topography of the Oce
an Floor with multibeam echo sounder. Compilation of the maps in scale
1 : 250 000 and 1 : 1 min have been with computer. Data obtained show
anomalous character of structure of the Equatorial segment: relativel
y narrow axial rifted zone and plateau like type of wide flancs probab
ly of nonspreading or diffuse-spreading origin.