Ancient Precambrian shields are the largest geostructural elements of our planet, in the depths of which numerous mineral deposits are widely developed. Within the shields, Precambrian crystalline rocks are exposed on the day surface and are therefore most accessible for various kinds of geologic and geophysical studies.
How to cite:
Chekunov A.V., Kalyuzhnaya L.T., Tripolsky A.A., Kharitonov O.M., Sharov N.V., Borodulin M.A., Guterkh A., Matezhok R., Perkhuts E., Grad M. Comparative analysis of the depth structure of the Baltic and Ukrainian Shields based on GSZ data // Journal of Mining Institute. 1992. Vol. 135. p. 74-91.
Seismic wave fields recorded during regional geophysical surveys by the method of deep seismic sounding (DSS) on the Ukrainian Shield are the main source of information on the lithosphere structure of this large structure of the East European platform.
How to cite:
Kharitonov O.M., Sannikova N.P., Tripolsky A.A. Features of seismic stratification of the Earth’s crust of the Ukrainian Shield // Journal of Mining Institute. 1992. Vol. 135. p. 108-120.
Ultra-deep drilling opens a new stage in the knowledge of the structure of the Earth's interior, as evidenced by studies of the Kola GGS-3 on the Baltic Shield.
How to cite:
Kharitonov O.M., Omelchenko V.D., Grin N.E. Seismic studies of the lithosphere through the Krivoy Rog and Dnieper-Donets ultra-deep wells // Journal of Mining Institute. 1992. Vol. 135. p. 121-128.
