Scientific publications

The authors discuss the results of RWM seismic studies along the profile Lake Syamozero-City of Kondopoga-Povenets Bay, located near the parametric borehole site, with regard for seismic data obtained by the ECWM and CDP-DSS methods, available geological and geophysical data and the drilling record for this area. This integrated approach provides a better understanding of the deep structure, composition, velocity section, possible geological nature and relief of the earth crust. The study of the Onega structure is important because it hosts large quantities of carbonaceous matter (CM) and productive mineralization that create geophysical anomaly fields indicative of their occurrence. Relationships between the rocks in the geological sequence of the trough are also significant both scientifically and from the point of view of geological prospecting and exploration. Therefore, correlations of the geological parameters of the unit with crustal matter, e.g. by drilling structural boreholes, can help solve some problems in theoretical geology.