Abstract
Peculiarities of trace element (TE) distribution in coals of the eastern Donets Basin (Donbas) are discussed. The correlation of TE distribution with specific features of the geological setting of the region can testify to the hydrothermal introduction of trace elements or their redistribution in fluid-active zones. The geochemical regionalization of eastern Donbas is based on TE distribution. Strontium–gold–base metal, tungsten, and selenium geochemical belts and a rare metal geochemical block are outlined.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: 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.