Abstract
The Osnytsk-Mikashevitsky volcano-plutonic belt may be considered as a representative of special intracraton type of volcano-plutonic belts of Early Precambrian in conditions of epiplatform rifting, which was the beginning of the basic restructuring of cratonic crust at the end of the early Proterozoic in central East-European platform. This is evidenced by duration of the belt formation, the inheritance of magmatism, the formation of structure and the variation of paleotectonic conditions from Early Proterozoic till Vend (Mesoproterozoic).
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.
