Abstract
The tectonic structure of the Orekhov-Pavlograd interblock zone of the Ukrainian shield is studied in this paper. This one has emerged since the 3600 million years ago, during the Katarchean/Archaean, ooidringed stage of the continental crust evolution. Its internal structure is described and anomalous features for future research are highlighted by comprehensive analysis of geological, geophysical, morphometric and remote sensed data.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
