Open AccessDomes of the Srednepridneprovsky tectonoconcentre of Ukrainian shield
Author(s) -
Stanislav Yesypovych
Publication year - 2018
Publication title -
ukraïnsʹkij žurnal distancìjnogo zonduvannâ zemlì
Language(s) - English
Resource type - Journals
ISSN - 2313-2132
DOI - 10.36023/ujrs.2018.16.122
Subject(s) - ukrainian , geology , shield , facies , gneiss , shields , denudation , basement , sedimentary rock , natural (archaeology) , geophysics , geochemistry , seismology , geomorphology , petrology , paleontology , metamorphic rock , structural basin , civil engineering , engineering , tectonics , philosophy , linguistics
The granite-gneiss domes of the Middle Dnieper were discovered from the data of gravitational and magnetic fields, since Ukrainian shield was significantly denuded and covered by a layer of sedimentary formations of various thicknesses. As a result of the comparison of US geological and geophysical information with the data of the Canadian, Scandinavian and other shields of the planet, a stable assumption about the similarity of their development history arose. It was for understanding the structure of US that the key structural question was not solved - which complexes of natural associations, and why, lie on different denudation sections of it. In numerous described facies, and then in the formations, the questions of the geological development of the shield were not solved. In this work, an attempt is made to clarify some of these issues.