Abstract
The behavior of trace and rare earth elements (REE) in weathering crusts (WC) developed after metasedimentary rocks of the Kursk Group of the Kursk Magnetic Anomaly (KMA) is considered. Specific features of their distribution in the weathering profile are noted and intervals of their concentration are outlined. It is suggested that the database of these elements can be used as indicators of the multistage formation and respective age of the WC.
Published Version
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.
